NUCLEAR QUADRUPGLE RESGNAN‘CE STUDY OF CHARGE-TRANSFER COMPLEXES Thesis for flu Degree of DE. D. MICHEGAN STATE UNEVERSITY James Austin Ryan 1967 TH ‘u L a” 'J LIBRA 12 Y Michigan State University This is to certify that the thesis entitled Nuclear Quadrupole Resonance Study of Charge-Transfer Complexes presented by James Austin Ryan has been accepted towards fulfillment of the requirements for fliL—degree mghs'm—iflx Wfizw ;' ( finial-wt; Date December 16, 1966 0-169 ABSTRACT NUCLEAR QUADRUPOLE RESONANCE STUDY OF CHARGE-TRANSFER COMPLEXES by James Austin Ryan A nuclear quadrupole resonance Spectrometer of the Dean type has been constructed both for frequency and field modulation and for display of the signal either on an oscillosc0pe screen or, by use of a lock-in amplifier. on a recorder. New chlorine quadrupole resonances have been found in the following charge-transfer complexes, SbCls-POC13, Fec13-Poc13, TiCl4-2POC13 and (TiCl4-POC13)2. These reso- nances were observed both at liquid nitrogen temperature and at room temperature, although in all cases the resonances due to the chlorine nuclei of POC13 in the complex molecule disappear below room temperature. A study of the temperature dependence of the resonance due to the "axial" chlorines of the SbCls part of SbCls'POC13 has been made. This study indi— cates a possible phase transition between 770K and 1650K. An estimate of the contribution of the solid-state effect to the observed resonance frequencies has been made assuming that the partially charged atomic sites in the lattice may be replaced by point charges and that this lattice James Austin Ryan of point charges makes the dominant contribution to the measured field gradients. A comparison of the calculated contributions of the lattice charges with the measured contribu- tions indicated that the Sternheimer antishielding factor for chlorine is much smaller than the value previously used by other workers. The shift in the absorption frequency of the chlorine atoms of POC13 in the complex, compared to their frequency in solid POCls itself, was used to estimate the relative amounts of charge shifted from donor to acceptor on complex formation for the complexes studied. The absorption frequencies due to chlorine atoms of SbCls and SnCl4 in SbCls-POC13 and SnCl4°2POC13 were used both to indicate the existence of nonequivalent bonding orbitals on the central metal atom and to estimate the total charge shifted to the central atom upon complex formation. The problems associated with the interpretation of NOR data for donor-acceptor complexes have been discussed in detail. NUCLEAR QUADRUPOLE RESONANCE STUDY OF CHARGE-TRANSFER COMPLEXES BY James Austin Ryan A THESIS Submitted to Michigan State University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Department of Chemistry 1967 ACKNOWLEDGMENTS The author is deeply indebted to Professor M. T. Rogers for his guidance and encouragement during the course of this work. He would also like to give special thanks to Dr. V. Nagarajan for his valuable advice and assistance in the con- struction of the NQR Spectrometer and Professor R. Schwendeman for several stimulating discussions. The experimental assistance of Mr. Michael Buckley, Mr. Russel Geyer and Mr. James Grumblatt is gratefully acknowledged. Finally the author would like to thank the Atomic Energy Commission and the Dow Chemical Company for financial support during a part of this work. ii TABLE OF CONTENTS Page .INTRODUCTION . . . . . . . . . . . . . . . . 1 I. THEORY AND BACKGROUND. . . . . . . . . . . . . . 4 Physical Theory. . . . . . . . . . . . . . . . . 4 A. Absorption Frequencies . . . . . . . . . 4 1) Basic Equations . . . . . . . 4 2) Absorbtion Frequencies and U . Selection Rules . . . . . . . . . 12 B. Zeeman Splitting of Quadrupole Spectra . 18 C. The Effect of an Electric Field on an NQR Absorption Line. . . . . . . . . . 21 D. The Effect of Temperature on the NQR Absorption Frequency . . . . . . . . 26 E. The Effect of Internal Electric Fields on the NQR Frequencies . . . . . . . . . 52 Chemical Interpretation of NOR Data. . . . . . . 40 A. Atomic Field Gradients . . . . . . . . 40 B. The Townes and Dailey Theory of Mole- cular Field Gradients. . . . . . . . . 44 C. Evaluation of the Parameters of the Townes and Dailey Equation . . . . . . . 57 Previous NQR Studies of Charge Transfer Com—" plexes. . . . . . . . . . . . . . . . . . . 63 II. EXPERIMENTAL . . . . . . . . . . . . . . . . . . . 70 A. The Nuclear Quadrupole Resonance Spec- trometer . . . . . . . . . . . . . . . . 7O 1) Introduction. . . . . . . . . . . . 7O 2) Superregenerative Oscillators . . . 75 5) Modulation and the Lock—in Ampli- ' fier. . . . . . . . . . . . . . . . 82 4) Frequency Measurement . . . . . . . 89 5) Spectrometer Operation and Problems in Detecting Resonances . . . . . 95 6) Temperature Dependence of the 27. 512 MHz Resonance in SbCls POClg. . . . 101 B. Chemical Synthesis . . . . . . . . . . . 101 1) Trans-dichlorobisethylenediamine Cobalt(III) Chloride-HCl'ngo . . . 101 iii TABLE OF CONTENTS - Continued Page 2) The Cu(I) Complexes of Some Thio- semicarbazones. . . . . . . . . . . 105 5) Mercuric Chloride Complexes . . . . 104 4) The Complexes of ICl with Pyridine and Its Derivatives . . . . . . . . 106 5) Binary Complexes of POC13 . . . . . 106 6) Ternary Complexes of POCla. . . . . 112 III. CALCULATION OF THE CONTRIBUTION TO THE MEASURED FIELD GRADIENT FROM CHARGES SITUATED IN THE LATTICE. . . . . . . . . . . . . . . . . . . . . 114 A. Introduction . . . . . . . . . . . . . . 114 B. Theory . . . . . . . . . . . . . . . . 118 C. Some Details of the Modification and Use of LATSUM. . . . . . . . . . . . . . . . 125 D. A Test of LATSUM . . . . . . . . . 125 E. The Crystal Lattice Field Gradient Model and Programs ROTATE and DIAG 1) The First Model . . . . . . . . . . 126 2) An Improved Model . . . . . . . . . 128 5) ROTATE. . . . . . . . . . . . . . . 151 4) PROGRAM DIAG. . . . . . . . . . . . 154 IV. RESULTS. . . . . . . . . . . . . . . . . . . . . 158 A. Assignment of Absorption Frequencies to Specific Atoms in the Complexes. . . . . 158 1) SbC15°POC13 . . . . . . . . . . . . 158 2) SDC14'2POC13. . . . . . . . . . . . 143 5) (Tic14 POC13)2. . . . . . . . . . . 144 4) Pure SbC15.. . . . . . . . . . . 144 B. New Resonance Frequencies and Their Temperature Dependence . . . . . . . . . 146 C. Compounds in Which No Resonances were Found. . . . . . . . . . . . . . . . . . 152 D. LATSUM, ROTATE, and DIAG Results . . . . 156 1) Tabulated Results of LATSUM and ROTATE. . . . . . . . . . . . . . . 156 2) Comparison of the Lattice Sum Re- sults Using Both the First Model and the Revised Model . . . . . . . 180 5) DIAG Results. . . . . . . . . . . . 180 iv TABLE OF CONTENTS - Continued Page V. DISCUSSION. . . . . . . . . . . . . . . . . . . . 187 A. Temperature Dependence of the Absorption Frequencies and Phase Transitions . . . . 187 B. Calculation of the Point-Charge Field Gradient. . . . . . . . . . . . . . . . . 195 C. Frequency Shifts in the Complexed POC13 Chlorine Atoms. . . . . . . . . . . . . . 200 D. Shifts in the NQR Spectra of SnC14 and SbCls Upon Complex Formation. . . . . . . 204 1) General Comments . . . . . . . . . . 204 2) SnCl4-2POC13 . . . . . . . . . . . . 206 5) Sbc15-Poc13. . . . . . . . . . . . . 211 SUMMARY. . . . . . . . . . . . . . . . . . . . . . . . 215 REFERENCES . . . . . . . . . . . . . . . . . . . . . . 216 APPENDIX . . . . . . . . . . . . . . . . . . . . . . . 225 TABLE 10. 11. 12. 15. 14. LIST OF TABLES Secular Equations for Nuclei with Half— Integral Spin. . . . . . . . . . . . . . . . . Formulas for the Nuclear Quadrupole Resonance Frequencies. . . . . . . . . . . . . . . . . . Quadrupole Coupling Constants of Halogen Con- taining Molecules Which Have Been Measured Both in the Solid and in the Gaseous State . NQR Data Indicating Hydrogen Bonding . . . . . 2 Values of anO = gig for Various Atomic States Frequency Shifts Upon Complex Formation Be- tween Brg and Some Substituted Benzenes. . . . NQR Resonance Frequencies in Charge Transfer Complexes Compared to the Resonance Frequenc- ies in the Pure Compounds. . . . . . . . . . . Physical Dimensions of the Coils Used With the High Range Oscillator. . . . . . . . . . . . . Comparison of q and n as Calculated Both by LATSUM and by Other Authors. . . . . . . . . Charges Used in LATSUM . . . . . . . . . . . Resonance Frequencies for the Compounds Studied in This Work . . . . . . . . . . . . Temperature Dependence of the Most Intense Line of SbCls'POC13 . . . . . . . . . . . . Coupling Constants and Field Gradients for the Compounds Studied in This Work . . . . . . . . Temperature Coefficients for the Chlorine Resonances of Complexed SbCls and SnCl4. . . . vi Page 16 17 58 59 42 64 67 99 126 151 148 149 150 152 LIST OF TABLES - Continued 15. Compounds in which NQR Absorptions were Missed. . . . . . . . . . . . . . . . . . . . 16-572 LATSUM and ROTATE Results for the Complexes Studied in This Work. . . . . . . . . . . . 58. Comparison of LATSUM Results Using the New Charges to LATSUM Results Using the Old Charges . . . . . . . . . . . . . . 59. Line SplittingslAql and "Experimental" Values of y . . . . . . . . . . . . . . . . oo 40. DIAG Results. . . . . . . . . . . . . . . 41. Temperature Factors for SnCl4°2POC13. . . 42. Bond Angles (in Degrees) and Bond Lengths (in ngstroms) of POCl3 in Various Complexes From X-ray Investigations. . . . . . . . . . . 45. Electronic Charge Lost by the POC13 Chlorine Atoms Estimated from NQR Data . . . . . . 44. Charge Transfer in Complexed SnCl4. . . . 45. Charge Transfer in Complexed SbCls. . . . vii Page 154 158-179 181 182 . 184 192 . 201 205 210 215 FIGURE 1. 2. 10. 11. 12. 15. 14. 15. 16. LIST OF FIGURES Pictorial representation of the various vectors and volume elements. . . . . . . Splitting of the quadrupolar levels by a mag- netic field. Assumed electric field direction Line width change with temperature for a) Hexachlorobenzene, b) 1, 2, 5- Trichloro- benzene. . A plot of the Sternheimer factor (7 ) versus ionic charge for helium-like ions. . . . . . . Ionicity versus electronegativity difference according to the approximations of Pauling (80). High Range Gordy (60). and Townes and Dailey (44) (15-55 MHz) Oscillator. . . . . . . Low Range (2-20(MHz) Oscillator) . . . . Modulation unit for the NQR Spectrometer Block diagram of the NQR spectrometer. . . . . The partial Spectrum of SbCls'POCls showing the 50.560 also shown line . . . Definition ROTATE . . A molecule A molecule A molecule and the 50.616 MHz absorption lines; are the quench Sidebands from each of the angles a and 8 as used by Of SbCls'POCls. . . . . . . . . . . Of SDC14'2POC13 . . . . . . . Of the dimer [TiCl4'2POC13]2. . . . Temperature variation of the most intense SbCls resonance of SbC15°POC13 . . . . . . . viii Page 19 24 28 56 62 74 75 85 90 91 155 159 140 141 151 INTRODUCTION Although the first pure quadrupole resonance was ob- served in 1950 (1), as yet no extensive application of this technique has been made to chemical problems. This is not due to a lack of potential applications but rather to experi- mental difficulties and the fact that the theory which con— nects experimental results to molecular structure is not, as yet, well deve10ped. Since the absorption frequencies measured by nuclear quadrupole resonance (NQR) spectroscopy may be interpreted in terms of migration of charge away from or toward, the resonant nucleus, this method is ideally suited to the study of charge-transfer complexes. At the beginning of this work there had been several NQR investigations (2-9) of charge-transfer complexes reported in the literature, but the results of these investi- gations seemed somewhat chaotic. In some cases they indicate no charge transfer while in other cases possible Shifts are obscured by solid-state effects on the resonance frequency. Finally, in the cases where an unambiguous charge-transfer effect is seen in the NQR absorption frequencies, no attempt has been made to study the size of this effect in a series of charge-transfer complexes. The solid-state effects, which result in a Splitting of NQR lines, have been known since the beginning of NQR Spectroscopy but they have never been studied in detail. The usual method for taking them into account is to take an average of the measured fre— quencies. Unfortunately for the study of charge-transfer complexes, this method is unsatisfactory because the split- tings may be of the same order of magnitude as the charge- transfer effects. In this work an NQR Spectrometer was constructed and used to study charge-transfer complexes. The complexes studied were chosen because chemical and X-ray data indicated that strong charge transfer takes place and because they represent a chemically related series. The adducts studied are formed by a transfer of electrons from the Lewis base POC13 to a Lewis acid. They include [TiCl4'POC13]2, SbC15° POC13 and FeCla‘POCla which, together with the previously investigated SnCl4°2POC13 (9), form a series whose charge transfer Should be related to the strength of the Lewis acid involved. Furthermore, since complete X-ray data are avail- able for SbC15°POC13, [TiCl4’POC13]2 and SnCl4'2POC13, an investigation of the solid—state effects was possible. A calculation of line splitting as a function of the Sternheimer parameter was made assuming that the field gradient produced by charged ions situated in the crystal lattice dominated the charge-transfer effects. This calcu- lation, which assumes a model that replaces the charged ions by point changes whose magnitudes are dependent on the ionicity of the bonds in which the ions are involved, pushes to the limit some segments of the NQR theory. Thus results from this work may be used to evaluate this theory. The molecular field gradients, which were obtained from the experimental absorption frequencies after allowance was made for solid-state effects, were then used to evaluate the extent of charge transfer. I. THEORY AND BACKGROUND Physical Theory A. Absorption Frequencies 1) Basic Equations The overall Hamiltonian HEL describing the interaction between a charged nucleus and the surrounding electronic charge may be written as pe(re)pn(rn)dvedvn ’ (1) H =+f EL V r \ / Nuclear \ // K" surface f // Figure 1. Pictorial representation of the various vectors and volume elements. where pe is charge density of the electrons external to the nucleus in the volume element dVe at position re with reSpect to the center of the nucleus under discussion, on is the charge. density of the volume element an within the nucleus at a position Vn with respect to the center of the nucleus. Also, Vn is a vector from dVn to dVe and Gen is the angle between r and r as shown in Figure 1. From e n the law of cosines 1 '2' '— = (r 2 + r 2 - 2r r cos 9 ) r e n en (2) r 2 2r -% = l- (1 + (-2) - -—3 cos 9 ) r r e e e e rn which can be expanded in a power series in-;— to yield e r I" 2 _1.= 1 _11 _I1 +.... r r (1 + r P1 + (r ) P2- ), (3) e e e where PE is the Legendre polynomial of cos Gen; i.e., P1 = cos een - 4. 2 _ (4) Pg 2 (5cos Gen 1) etc. The first term of this power series corresponds to an electric monopole, the second to an electric dipole, the third to an electric quadrupole and, in general, a term in 2. We shall Pg corresponds to'a multipole moment of order 2 be concerned with the term in P2. In particular we are interested in the energy levels which arise due to this term. Substituting Equations 5 and 4 into 2 we obtain the equation _ 1 (5) H — f f V 2p -§ (5 cosaeen -1)pe(re)/re3 andVe 9 V5; Vri n n for the nuclear electric quadrupole interaction. This equation is valid only if re)»rn, since it is only under these conditions that the expansion (Equation 5) is valid. This restriction has the effect of excluding from our con- sideration electronic charge which actually penetrates the nucleus. This is not serious, however, since only s electrons have a non-zero probability of penetrating the nucleus and because of their Spherical symmetry they have no interaction with the nuclear quadrupole moment. Equation 5 may be expanded in Cartesian coordinates using the relation- ship r r cose = Z X X to yield n e en 1 ni ei H = r f (r )[é-Z x x x x - ;-r 2r 2] (6) Q 4 Dn n 2 .. ni nj ei ej 2 n e Ve Vn l X pe(re)/re3dvndve. However, if we define Qij and.(vE)ij by the relationships = _ 2 Qij é pn(Vn) (5xnixn-j éij rn )dvn n (7) X .X . + X -X . = f on(vn) [ 5( n1 ”3 n3 n1) - 5--r 21dV Vn 2 13 n n and _ ~ .1 (VE)ij - - éepe(re)8/BXi d/ij( re)dVe (8) = - é pe(re)/re5 [5XeiXej - éijre2]dVe e pe(re) xeixej + xejxei 2 - -J —;;S—- [5<; 2 > '- oij re ]dVe. e Then, 1 = = = - — Z .. .. = : HQ 6 ij013 (vmlj Q vs (9) where the double dot indicates a scalar product of two second rank tensors; this may be verified by direct expansion of Equation 9 using the first form of Equation 7 and the second form of Equation 8. Thus, we have seen that HQ can be completely described by two tensors S (the quadrupole tensor) and -V_-E (the electric field-gradient tensor) whose elements Qij and (vE)ij have been defined by Equations 7 and 8, reSpectively. Furthermore, the two tensors are sym- metric and it can be seen by inspection of Equations 7 and 8 that both a and 6E are traceless. Ramsey (10) has shown that the elements of the Q tensor Qij may be represented in the form Q = C[5( = c < I I |5(IZ)2 - 12 I I > = C[5I2 - I(I+1)] = c I (21-1), (12) using Equation 11. Hence, I I + I I eQ i j yj i _ ij 'ITEI:IT [5( 2 ) éijlg]. (15) Q It is of interest here to point out that while nuclei of Spin I > 1 have non-zero quadrupole moments, nuclei of Spin I = 0 and I =-% do not necessarily have to have a zero quadrupole moment (14). It often has been written that nuclei with I < 1 have zero quadrupole moments, this is in- correct. However, it is impossible to observe a nuclear electric multipole moment of 23 greater than that correspond- ing to 2 = 21. This is easy to prove. From Equations 5 and 1 we can see that insofar as the nuclear coordinates are con- 2 cerned the interaction for the 2 th moment is proportional to f r p (r )P dV . (14) Vn n n n E n but if wn is the nuclear part of the total wave function W _ - 2 * total - wewn,Equat1on 14 becomes 5 rn ¢nP£¢nan. n However, if the angular momentum of the nucleus is I then wn must be an eigenfunction corresponding to an angular momentum of I. Since 5i has no angular dependence but PE has an eigenvalue of 2 under operation by the angular momentum operator, rfiwn and Pgwn correspond to eigenfunctions with angular momentum eigenvalues of I and between I + fl and II - 2 l, respectively. In order that Equation 14 not vanish rfiw; and Pgwn must correspond to the same eigen- values; hence, I must lie between I + Z and II - fl . This can only be true if E‘s 21 hence for nuclei Of'Spin I multipole interactions of order 22 where Z > 21 cannot take place. Returning to the quadrupole interaction let us examine the electric field gradient tensor 57?. The elements (VE)ij previously given are identical to Vij' where Vij =§%E%§f , and V'is the electrostatic potential at the nucleus 3) (the units of Vij are cm‘ . In the usual notation.X1=x', X2=y', and X3=z' where the primes indicate that we are not yet in the principal axis system. Since (7E is traceless and symmetric Y'Y' + Vz‘z' = O (15) and we need specify only five elements to completely Specify the tensor. 10 These elements are: (VE)0 = % V2.2. 1 . (VE)i1 7JE‘Vx'z' 4.1Vy.z.) .21. (VE)12 - 2J6 (Vx‘x' -vy'y' i'zvx'y') Any symmetric tensor may be diagonalized, this diagonalization corresponding to a transformation to the principal-axis system. The diagonalized tensor has components _ 1, 2.1 (VE)Q - 2 sz — 2 eq (vs)i1 = o (16) 1 1 (VE)42 - 2J6 (Vxx-Vyy)- 2J6 n eq. This correSponds to the definitions _.1 q — e sz and (17) (v -v )/v n xx yy zz . Using the convention I VXX (g_l Vyy lg_|vzz|, n may vary from 0 to 1. For n = 0, V = V = - 2-V and for n = 1, xx yy 2 zz V = 0 and V = -V . The first condition corresponds to xx yy zz cylindrical symmetry. For chlorine atoms involved in single bonds it is a very good approximation to assume cylindrical symmetry, therefore the assumption is usually made that n = 0. An expression must now be derived which will relate the observed resonance frequencies to the quantities q and n. We proceed by writing an expression for the quadrupole energy level designated by the quantum number m, where m can take 11 the values m = +I, I-1, .... -I, these numbers corresponding to the allowed spin orientations in the electric field gradient. Thus, it is necessary to calculate the matrix elements (mlHolm'> for the two cases of axial (fi=0) and non-axial (n#0) field gradients. To calculate the matrix elements we need only know the general behavior of wave functions ¢n(m) with the angular momentum Squared operator I2 and the angular A . A A A . momentum operator I, With components Ix, Iy and I2, 1.e., (mllem'>==m6mm' and (mllxiilylm'>= [(I m)(I¢m+1)] ém¢1,m' (18) where 6 is the familiar Kroneker delta. Using these relation— ships we can write (Equation 19) the only non-zero matrix elements (15). Since = _.1 = eQsz 2_ 2 eQ(Vxx:YYY) HQ 6 §.Qij( E)ij 41(21-1)[512 I 1 + 41(2I-1) j 2 2] I - I and [ X y ' _ _ _ =e2 2— (mlHQIm>—-< mlHQl m> 4I%%I:I) [5m I(I+1)] and (19) ==<-m|HQ|-mi2>====<-mi2|HQl-m> ; then 2399... .n 2' -i E = [I(I+1)-m(m+1)] [(I+1)I-(m11)(mi2)] ; 41(21—1) 2 the quantity e2qQ is commonly called the quadrupole coupling constant and is identical with qu' which is another common notation Since q'E eq. For n = 0 we have only diagonal non- zero matrix elements and use of Equations 18 immediately yields 12 Em = = A[5m2 - I(I+1)] (20) where we have used the common notation A = e2qQ/4I(2I-1). We see immediately that all levels except m = 0 are doubly degenerate. Thus, for half-integral Spins there are I +-§ energy levels and for integral Spins there are I + 1 levels. 2) Absorbtion Frequencies and Selection Rules In order to derive the selection rules it is necessary to consider a mechanism by which transitions between energy levels are produced. Although it is possible in theory to induce transitions by application of an electric field gradient, in practice this would require a field gradient which is too large to be produced in the laboratory. In order to induce an observable number of transitions, we must, therefore, turn to an oscillating magnetic field which can interact with magnetic dipoles; that is, electromagnetic radiation. The time dependent Hamiltonian representing this interaction may be written as H(t) = -yh(HXIX + Hny + HZIZ) (21) where 7 is the magnetogyric ratio, h is Planck‘s constant, Ix, Iy and I2 are the components of the angular momentum operator and Hxl'Hy and H2 are the components of the linearly polarized oscillating magnetic field. The matrix elements 2will then be proportional to the transition prob- abilities and may be calculated with the aid of Equation 19. 15 We then find that the transitionslAmJ = 0 and 1 are allowed; these then are the selection rules for the case of n = 0. Furthermore, it can be shown.following the treatment of Pake (15) for the case of magnetic resonance.that maximum transi- tion probability occurs when the Bohr condition w = - (22) is satisfied. We may now write, using Equations 20, an expression for w: a. = {115 (2|m|+1). ’ (25) There are (I + %)doubley degenerate energy levels for half— integral spins and I + 1 doubly degenerate levels for integral nuclear Spins. If I and m are known, which is usually the case, then equ/h (in units of MHz) may be calculated directly from the measured value of absorption frequency. If the m value is not known, and this situation may only arise for spins I > 5/2, the values of ml and ma may be uniquely determined by measuring the ratio -$:-= %%E:+$—% . For the case of n # 0 the problem of writing down ex- pressions relating ean, n and w becomes much more complex. Now we must also consider matrix elements of the type calcu- lated in the second of Equations 19. This results in the mix- ing of the pure magnetic dipole states with states differing in m by.i 2. Because of this the selection rules 'Am|= 0.1 no longer hold and for values of n) 0.1 the probability for 14 observation of transitions correSponding to lAm|= 2 becomes quite large. Reddoch (15) has observed the 93Nb(I = 9/2) resonance in NbCls. The observed spectrum contains lines due to transitions for which IAm|= 2 and even IAmI= 5. The calculated relative intensities for n = 1/5 in the transi- tions lAmI = 1, [Aml = 2 and lAml = 5 are, respectively, 129, 54 and 7.8. In some cases the degeneracy of the doubly degenerate levels is removed. For the case of I = 5/2 we now have to consider the matrix elements Hm,mi2 =< mlHQImiZ> in addition to the matrix elements Hmm ; the Hamiltonian matrix now becomes 0 Hi” i’ -' E 0 Hi , _ .3 H = H__é_’§_ O H‘fi-é‘ - E 0 O H‘B'Ié‘ O H__3__a_ - E where Hi Epi-E = 5A, gi-§.i-§ = -5A and 34-4'1-3 =If5 A n. This matrix may be put into the diagonal form by simply re- arranging rows and columns. When this is done two submatrices are obtained along the diagonal, the first of which is Hes” Hit-4 3-43 H44” 15 This submatrix yields a secular equation E2 -5A2 (54-n2) = 0, using the previously tabulated values of the matrix elements. This equation can be solved exactly to yield Eg.=:22gg(i+%;)§ and E_§ =-:EZQQ(1+%E)5. Solving the second matrix gives E9 = E-g and Efi = 31%? thus, the mixing of the magnetic dipole states does not remove the energy level degeneracy. Using the Bohr condition one then obtains .32 1_12339. 113*} w‘*2_’iz)-2(h”1+s)- (24) In a similar manner the other secular equations may be de- rived. Except in the case of I e 1 it is not possible to obtain an analytical solution for these equations. For the case I = 1 it is found that the degeneracy of the levels is lifted; in this case two frequencies are predicted =éeng _=§e‘2_qQ _ w+ 4( h )(1 + n/5) and w 4:( h )(1 n/5). It is thus possible to obtain ‘both n and ean from an ob- servation of w and w_. It is not possible to measure both + e2qQ and n for nuclei with I ?'% (e.g. 35€1,81Br) because only one resonance frequency is observed. As mentioned previously the assumption is made that n = 0 for chlorine resonances; from Equation 24, if n = 0.1 this assumption in- volves an error of about 150 kHz. This value for n is seldom exceeded even if a moderate amount of double bonding is present. The secular equations for the cases I = 5/2, 5/2. 7/2 and 9/2 are tabulated in Table 1; these are the most important values for the purposes of quadrupole resonance. 16 Table 1. Secular Equations for Nuclei with Half—Integral Spin I“ _====—. I Secular Equation Units of Energy 5/2 52 — 5(5 + n2) = 0 e = E/A 5/2 53 - 7(5 + n2)e — 2(1 — n2) = O a = E/2A 7/2 54 - 14(5 + n2)€2 - 64(1 - n2) 5 + 55(5 + n2)2 = 0 e = E/5A 9/2 as - 11(5 + n2) 53 - 44(1 - n2) 52 +-%§(5 + n2)2€ + 48(5 + n2) (1 - n2) = 0 e = E/6A Except for the cases I = 1 and I = 5/2 these equations are not analytically solvable. Various methods have been used in obtaining solutions for them. Cohen (18) has given the numerical solutions of secular equations for I = 5/2, 7/2 and 9/2 and has tabulated eigenvalues for values of n from 0 to 1.0 in steps of 0.1; Livingston and Zeldes (19) have tabulated the numerical solution for I = 5/2 in steps of 0.001; Reddoch (15) has numerically solved and tabulated results for I = 9/2 and n2 from 0 to 1 in steps of 0.01. Numerical solution seems to be the best approach. Bersohn (17) has expanded 8 in a power series in me about n = 0 which is valid for low values of n(n Z:0.25). When this value for n is substituted into the Hamiltonian a perturbation treat- ment allows us to extract expressions for absorption fre- quencies in terms of n and these are presented in Table 2. 'V c.‘ 17 Table 2. Formulas for the Nuclear Quadrupole Resonance Frequencies H I) g.» 8 ll 1 5/4 equ/h (1 + 3/5) 5/4 ean/h (1 - n/5) E II I = 3/2 on = Y/Zean/h (1 + nos)? . 2 ' I = 5/2 wl 5/20(§EQQ)(1 + 0.0926q2 - 0.654n4) ' 2 mg = 6/20(§399)(1 - 0-2057n2 + 0.162q4) 2 ~ I I I = 7/2 wl = 1/14(§EQ9)(1 + 50.865q2 - 101.29n4) 2 . _ 42 = 2/14(3399)(1 - 15.867q2 + 52-052n4) . 2 i i ' ws = 5/14(3399) (1 - 2.8014q2 - 0.527sn4) I = 9/2 wl = 1/24(§;99)(1 + 9'0335n2 - 45.691n4) mg = 2/24(§E99)(1 -_1.5581n2 + 11.724n4) w3 = 5/24(§;99)(1 - 0.1857n2 - 0.1255n4) w4 = 4/24(E§g9)(1 - 0.0809n2 - 0.0045n4) It should be emphasized that these equations are only valid for small n and should be used with caution. Recently Alexander and Ganiel (20) have expanded the quadrupolar Hamiltdnian around 1 — n and have calculated the eigenvalues and eigenfunctions of the fully asymmetric (n==1) Hamiltonian. This expansion has certain advantages because, since their Hamiltonian changes Sign upon a rotation of v, certain of the matrix elements may be set equal to zero unless both the wave functions involved in the matrix elements have the same phase ”’0 o— 5;- ‘1 V V. fl! VA .1. in (I! ‘1' 18 factor 7 under rotation of F. Comparison of their results with the exact numerical results shows that this expansion is valid in the region of i] from n = 1 to about n = 0.2, thus this method slightly overlaps Bersohn's expansion. The value of the power series expansion lies in the insight which it allows into the eigenfunctions and eigenvalues of the quadrupolar Hamiltonian but it seems clear that if accurate values of n and e2qQ are wanted from measured fre- quencies the numerical solutions of the secular equations should be used. B. Zeeman Splitting of Quadrupole Spectra If a single crystal of a material containing a quadru- polar nucleus is subjected to a weak magnetic field (of the order of 100 gauss) such that e2qQ>> VhH, where y is the magnetogyric ratio and H the magnetic field strength, it is observed that each line will be Split into two or more lines. This is due to the fact that the magnetic field lifts the degeneracy of the doubly degenerate levels (Figure 2). It is observed in this case that four lines are now possible and, in fact, have been observed. No attempt will be made here to give the full theory of Zeeman splitting but the simple case of n = O, I = 5/2 will be treated in outline. Das and Hahn (16) have treated all cases in great detail. In addition, Bersohn (17) treated Spins of any value and small n and Cohen (18) has given a full treatment for half-integral Spins and arbitrary n. The original study of Zeeman Splitting of 19 H # 0 _‘§ H=O A 2 m =.i-% 5 \ _+_§ _ .V - (LB (DB m = i‘% , \L * + Figure 2. Splitting of the quadrupolar levels by a magnetic field. a pure quadrupole line was done by Dean (28) and his methods of analysis are for the most part still in use. AS long as e2qQ>>th we may treat the magnetic field as a perturbation. We then wish to calculate the matrix elements of the Hamil- . , = + . . . tonian HQ H.Q HM,where HM lS given by the equation HM = -th(Izcose + IX Sinecos¢ + Iysin951n¢), G is the angle between the Z axis of the principal-axis system and the magnetic field direction, and ¢ is the azimuthal axis for H governed by the particular choice of X and Y for the principal-axis system. For the states of half-integral spin and m>§ there is essentially no mixing between states 20 and, for example, the states.i 5/2 are split apart according to the equation Em = Atsmg - I(I + 1)] 1F mhyHcose The matrix elements are not dependent on the Ix and Iy terms in HM and hence not on ¢; this is because the contribution due to these terms is small and may be neglected. However, for the case of m = i.'§ these terms may not be neglected Since this leads to a mixing of the states m =-§ and m = -§u That is, two new states arise whose eigenfunctions are desig- nated by w+ and w_, where w+ = C1¢% + ¢_é_and ¢_ = C3¢%_+ C4¢_§, Degenerate perturbation theory then leads to energies of Ei.= A[&-- I(I + 1)]¢'§-hyHcose where f = [1 + (I + i) tan29]§7 also, ¢+ = wi sina + ¢_§cOSd.and ¢_ = wdfi sind - Wfi C050 7 + f 1] tan d = [f _ 1 It is interesting to note that again we have no dependence on the azimuthal angle ¢ to the first order. From the above equations it may be shown that the frequencies of the four absorptions arising because of the level splitting are given by _ 6_A _ ___3-f wa-— h 2 yHcose 6A 5+f wB = 7T-- —§-yHcose 21 . _ 6A S-f wa’ - T?" + —§—-7Hcose . _ 6A 3+f wB - T?’ + -§-7Hcose . These four lines are symmetrical about the line which appears when there is no applied homogeneous static magnetic field. It Should be noted that this discussion applies only to resonance samples in the form of a single crystal. If the sample is a polycrystalline powder then we have a wide distri- bution of values of the angle 9 which results in a large number of lines at varying distances from the zero field line. Since the amplitude of each line is inversely proportional to the number of lines this has the effect of smearing out all lines. Therefore, Zeeman studies cannot be done on powders; however, this effect is useful in one modulation scheme. C. The Effect of an Electric Field on an NQR Absorption Line Bloembergen and co—workers {21-25) have observed broaden— ing of nuclear quadrupole absorption lines upon the applica- tion of an electric field to polycrystalline and Single crystal samples. Kushida and Saika (26) have also observed this effect in 81Br NQR Signals in NaBrOa. This effect is quite generally to be expected when the nucleus under investi- gation is located in a crystal site which lacks inversion symmetry. Dixon and Bloembergen (24,25) have investigated this effect in great detail. They present a phenomenological theory to explain the macroscopic physical interactions 22 reported in their first paper (24). They then present, in their second paper (25), microscopic theory in terms of ionic character and sp hybridization which attempts to pre- dict the electric Shift in terms of these more basic quanti- ties. The macroscopic theory may be understood in terms of a E * , third-rank tensor R* whose elements are Rfimp = §2m2__ = 5E ext eoqmp/BE£ , where Eext = l EleXt + 3E2ext E /\ + kEsext is the externally applied field and the Vmp's have been defined previously. Thus, the perturbation in the . . . . _ *. electric field gradient components Aqmp is eAqmp - % Rfimp )(- EEeXt (25). It Should be noted that REmp is a tensor defined at constant stress because this is the condition under which these experiments are performed. However, it is really the tensor i defined under conditions of constant strain which * we desire since strictly speaking. in Equation ZSngmp should be replaced by R These two quantities are related flmp' by the following equation: + d , flmp Bmp :rSmpqr Eqr where dfiqr is an element of the piezoelectric coefficient tensor and Smpqr is a fourth-rank tensor (27) which relates the changes in the electric field gradient components to the induced strain components. In most materials the dfiqr components can be considered small and fi* = i ; however, care must be taken with those materials which exhibit a large 23 Iqiezoelectric effect. It is also assumed that Eiext = Ei’ ‘Mhere Ei is the actual field which is felt by the electrons 5J1 the molecule. This is because the electron distribution .1n the molecule has an averaging effect on the applied field. Vtith these assumptions the perturbed Hamiltonian representing ‘Ehe quadrupole interaction may be represented as HQ' = HQ + HE = [eQ/61(21-1)]; [3/2(IjI + I Ij) - ik k k éik I(I + 1)][Vjk + i Ei Rijk] . (26) Frxnn the unperturbed part of HQ' we obtain the equation (see 22) wo(m+1-—+-m) = [3e2qQ/4I(21-1)h][2lm(+1] ; similarly, = [eQ/GI(ZI-1)][5m2-I(I + 1)] (27) E E E x[ szz --§ (AvXX + Avyy)] Fuxmn Equation 27 we may then obtain AwE(m+1 ——> m)= [eQ/(ZI-1)4Ih] [2|m|+ 11pm:i [R133 — g» i (28) (R111 + R122)]]. ”III IJsing the fact that is traceless, Equation 28 reduces to AwE(m + 1 —+m) = [SeQ/4I(21 - 1)h1[2lm|+ 11 [13312333 + EeR233 + EiRiss] I (29) \Mhere AuF is the electrically induced shift in resonance ov‘ .- it I" u.- .A‘ bu- P... 2}. 5.. ‘1- .Il fiv- Vs. 24 :frequency. If axial symmetry holds,R233 = R133 = 0; ‘therefore, Amp/mo = R333E3/eqzz, where index 5 corresponds tn) the z coordinate. If the sample is polycrystalline rather “than a single crystal,an average must be taken over all . . ea» R z direction Figure 5. Assumed electric field direction. I_ . ,uv‘ .np 1v:- “Q h In h.\. D (I) ‘ _~r ; b.“ 5‘ ~‘ ‘- I ‘u‘ ‘- .11 25 Because the 6-bonding orbitals are directed along the bond and the 1r-bonding orbitals are directed perpendicular to the bond the field has opposite effects on the 6 and Tr electronic distribution. For 6—bonding orbitals the change in qzz(A) iS quz(A) = -lqat|€6 and quz(B) = +lqatle6, § (30) orlquz/qat(= eEORB/(Z) A . where - < I I > (A )—l- eE R 2(1-s 2m 2]”‘1? (51) €6——¢gHEd/e c5 " OB[ 6 6 wg is the ground state eigenfunction of the molecule, here taken as the bonding LCAO orbital, and we is excited state eigenfunction, here taken as the antibonding LCAO orbital; RE is the internuclear distance. E0 is the scalar value of the applied electric field, S is the 6 overlap integral, A 6 is the average energy separation between the ground and the 6 excited state and eqat is the field gradient due to one un- balanced p electron in the valence shell. Several approxi— mations are involved, the most important being 862 = O and the assumption that there is only one low—lying excited state. The validity of the assumptions depends on the indi- vidual molecule but in any event the choice of a value for A6 is not clear-cut; Dixon has chosen, rather arbitrarily, twice the value of the bond dissociation energy for this value. For a double bond the change in the electric field gradient 1 5 ca lculated aS ’L .uv 97‘ vi ’v ‘i ‘A ‘i\ sql ;|\ ’1- 26 quz‘“ €7T/2 (qatl quz(B) : _€7T/2 (qat l ' with e.” = eEoRB/(A7r[(1 - SW2)2]3=*). It is important to notice that these effects are opposite to those of Equation 20; thus, in a bond which has some double-bond character, there will be some cancellation of the effects of the electric field. This has been observed by Dixon and Bloembergen. Using both variational and perturbation approaches, they have developed equations which relate the observed broadening to the Sp hybridization and ionic char- acter of the bond; at the present time, however, these equa- tions are too crude to yield meaningful results for the parameters. As will be discussed later e2qQ may also be ex- Pressed in terms of these quantities; thus the electric field effect gives another measurable to determine these parameters. It is clear that more work is needed on this effect. D~ The Effect of Temperature on the EQR Absorption Frequency It is generally found that as the temperature is lowered the frequency of an NQR line increases. Studies of tempera- tLire dependence have been used to determine the temperatures at; which crystalline phase transitions (28) occur and the temperature at which the barrier to internal rotation for 1. 2—dichloroethane is overcome (29). These transition temperatures are recognized because of distinct breaks in ..1 II- I'- v. a .-v r- ,- A I b (I) r 27 curves of frequency yersus temperature, the number of lines due to a particular nucleus may change due to a change in crystal structure during a phase transition. Frequently resonance lines which are observable at 770K disappear or greatly decrease in amplitude when the temperature is raised; this effect is not well understood although it is generally attributed to vibrational effects. The disappearance of quadrupole lines has sometimes been attributed to crystalline phase changes and undoubtedly in some cases this is true; however, in other cases the disappearance of the line may be more realistically attributed to vibrational effects. Several compounds Show an anomolous effect in that their resonance frequency increases as temperature increases. Haas and Marram (50) have recently attempted to explain this abnormal behavior in chlorine compounds in terms of two competing effects. First, there is the vibrational motion which tends to lower the frequency as the temperature is raised since this increases the amplitude of vibration with a consequent 'averaging out' of part of qzz' It has been found that tor— Sional motion dominates the vibrational effect. The second effect is due to the fact that as the temperature is increased the increased bending vibrational motion tends to break down the V bonds causing an increase in the population of the cl'llorine 2pTr orbitals, thus causing the absorption frequency t<> increase. Bayer (31) has treated the effect of torsional motion on the quadrupole resonance frequency. Many refinements have 9‘? 0.4. III ~..- ivy O ‘V .‘A 5..., n~~ vy. RA. H». L .’A .- I-.b 28 been introduced for this theory but only the simple theory is presented here, since the results are not used explicitly 111 this work. It is assumed here that the frequency of the txxrsional motion is much larger than the quadrupole resonance frequency and thus we need to consider only the average effect of torsional motion on the quadrupole resonance fre- quenncy. This is almost always true since vibrational motions are: usually in the infra-red or Raman region with frequencies of? the order of 1013 Hi, while quadrupole resonance fre- quenncies are in the order of 108 Hz‘ However, if the vibra— ticnnal frequencies are not much larger than the resonance frequencies a broadening of the resonance line, rather than a shift Occurs and is given by the equation Aw (eXp(—- g—T) , where Ad) is the line width change due to rotational motion and W is the finitential barrier to rotation. Tatsuzuki (52) has studied the changes in line width with temperature in 1,2,5-trichloro- benzene and hexachlorobenzene and his results are Shown in F j-<3ure 4 . (a) (b) Log Aw Figure 4. Line Width change with temperature for a) Hexachlorobenzene, b) 1,2,5-Trichloro- benzene. 29 Ta and Th are transition temperatures after which free rota— tion takes place. Values for W of 6.0 i.O.1 kcal/mole and 12.6;t-2 kcal/mole have been calculated from these data for the molecules hexachlorobenzene and 1,2,5-trichlorobenzene, respectively. Let us consider the effect of pure, very fast torsional motion on an axially symmetric electric field gradient q where the tensor, in the principal—axis system, may be written as -§- 0 o 0 -§- 0 n-Q II II .Q 22 O O 1 If a rotation of 9 about the Y principal axis occurs then cose O -sin9 -§- 0 O cose O sine E = o 1 o qzz 0 ~% 0 o 1 o sine O cose O O 1 -sine O cose ~§cosze + sinae O ~§sin9 cose 0 -§- 0 —§cose sine O —§sin29 + cosge For small values of 9, sin e g e and cose ; 1; then, 5192-3.» 0 —£-e ZZ - r A \ '00: If. .9. u r. 5" DA‘ ‘v 50 Since we are considering only very fast motion we are interested only in an average angle <9) and, since = 0 when 6 undergoes symmetric vibrations, we write \ 3 <92> - '5‘ o o a = qzz 0 4% O ( o o 1-51 Finally, taking into account simultaneous rotations about the X axis, denoting this angle by 9X and average angular motion about the Y axis as GY we obtain % - t o o 3 = qzz O 3 — t O _ 2 _ 2 o o 1 Skax > 3<9Y > ( (53) From Equation 55 we see that we must replace qu by qzzu‘) = qu (1 - a - 3 ). Similarly the rotational motion introduces an asymmetry para- : &( - - §<9Y2> ' small value of n we now calculate the resonance frequency as meter n given by n Neglecting this a function of temperature. If we treat the system as a rigid rotator a quantum mechanical treatment gives for the rotational (torsional) frequency v2 th/kT 47w 2 <92) A = kvz [5 + 1/(e - 1)], (55) E 2 Where k is Boltzmann's constant and A2 is the appropriate Inoment of inertia. Using this equation 51 1 w(T) = 1(0) [1 - a h/41r2 Axvzx {4; + 1/(thEX/k'r - 1)} .2, M412 i (.1. + 1/(th2Y/ktr - 1m (56) AY ZY and the temperature coefficient becomes _ h2 1 th.ex/kT thEY/kT 1 50(a—T)v— ' g 412 Ha [3(Jvzx7ki 1)‘2 + AY(th3£y/’+§ 3%T ’ (58) where d is the thermal expansion coefficient and B is the compressibility. Thus, to relate theory and experiment we need to measure the effect of pressure on NQR frequency. This has been done by Kushida, Benedek and Bloembergen (55) for C1 in KC103 and p-dichlorobenzene and for Cu in Cu20 and by Fuke (54) for SnI4, AS406, KBrOa and p-dibromobenzene. Kushida et al. (55) and McCall and Gutowsky (55) have im- proved the Simple Bayer theory but it has not been possible to obtain quantitative agreement with experiment, probably due to the fact that rotational frequencies are temperature dependent but also because other vibrational modes besides torsional motion become important. Fuke (54) has observed ‘this latter effect in AS408. . I'- ...\ .0! 3.. 0|: hank n- hp. V. 'd. ‘5- ‘$ «T‘ I I. e a. i ‘A a(1 52 E. The Effect of Internal Electric Fields on thegggg Frequencies The theory of Townes and Dailey which iS discussed in the Chemical Theory section, is an attempt to interpret NQR frequencies in terms of chemical parameters. This theory is strictly true only when the individual molecules are not allowed to interact with one another, which is true only when the substances under study are in the gaseous state. Since pure quadrupole resonance experiments must be carried out on a solid, a correction Should be made for the effect of the crystal lattice on the NQR frequencies. Although this adds considerable complexity to the treatment of NQR data, it has the advantage of allowing us to investigate solid-state interactions which could not otherwise be studied. Although there is no clear division among these effects an arbitrary division into three different interactions will be made in order to facilitate discussion. (1) Direct contributions due to the effect of charges situated on neighboring atoms in the crystal lattice. This effect is proportional to r"3 and hence should fall off rapidly with distance. However, calculations Show that some contributions are felt from atoms 603 and even 1008 away. This contribution is enhanced in some cases and decreased in other cases, by the Sternheimer effect, which is corrected for by multiplying the calculated ionic field gradient by 1 - 700, where 700 is called the Sternheimer factor and is gxositive (with a value between 0 and 1) for shielding and 55 negative for antishielding. The effect is due to the fact that external charges, besides having a direct contribution to the field gradient, also have an indirect effect due to a distortion of the closed Shell electrons around the quadru- polar nucleus. This distortion may decrease or increase the Shielding of the quadrupolar nucleus and hence is called antishielding or Shielding, respectively. It could also be said that the external charges induce an electric quadrupole moment in the electron distribution around the quadrupolar nucleus. This causes a redistribution of charge in the mole- cule which in turn affects the electric field gradient felt by the quadrupolar nucleus. This redistribution may be such that it enhances the field gradient (antishielding) or can- cels part of the field gradient (Shielding). In general small cations such as Li+ experience Shielding and large deformable anions such as Cl- and Br- experience antishielding. Stern— heimer and others (57-42) have calculated this enhancement factor for a number of neutral atoms and ions. Unfortunately this calculation is very difficult and often two calculations for the same atom will not agree. In particular, Sternheimer has previously calculated a value of -56.6 (41) for 7o) of the chloride ion; however,experiment (49-54) has indicated a value of -10 as being more reasonable. Burns and Wikner (50) have pointed out that, in a solid, higher symmetry and larger internuclear distances result in pertubations of the large negative anions, and since Sternheimer used wave r uer .‘uv \ in: .. CA,- I v‘vu‘h .A' Ow. . h‘, L3“ p; (Ii (I) l V 1. L!) D TI 4,. ’(‘1 ,1 in All W 54 functions which only apply strictly to atoms in the gaseous state, it follows that properties which are sensitive to this solid state effect cannot be calculated very accurately with these wave functions. Wikner and Burns (51) tried to correct this by using what they call contracted wave functions. They constrained the wave functions to give the correct value for the average diamagnetic susceptibility for the Cl- ion in a series of compounds. Using these wave functions they calculated a value of -27.4 for 700. Recently Sternheimer (55) has calculated a new value of yaafor the Cl- ion, taking into account second—order effects,and obtains an improved value of -45.89. He also states that the solid-state effects discussed by Burns and Wikner would decrease this value by as much as 2/5 although he did not make any quantitative estimate. Another reason for the poor agreement between the calculated and the empirical value for ya)(Cl-) can be found in the fact that Yoo is sensitive to the charge on the ion. This is logical Since the more polarizable an ion, the larger the antishielding. For example, in most chloro compounds the charge on the chlorine varies between zero for a chlorine in a completely covalent bond to -1 for a chlorine in a com- pletely ionic bond. Therefore, as an ion becomes more polariz- able (more ionic in the case of chlorine), it follows that the antishielding factor Should become larger and, furthermore, a smooth increase is expected. The Sternheimer factor for a neutral chlorine atom has been calculated by Sternheimer (57) as +0.42 shielding. This effect is expected to be quite v-F 9“” ov-fi ar‘ .11. \ L... h ‘5... p 6 b ‘1’ AA- " w‘. - § § 1‘1 Li ( r r '1 (I; “w. .VI 55 important. Figure 5, which is taken from a paper by Das and Bersohn (42), illustrates this point. The Sharp increase in going from He0 to H_ is especially interesting since it roughly parallels the change in going from C10 to Cl-. In this case the quadrupole moment induced in the closed shell electrons of H- is such as to be highly Shielding; however, it is quite likely that in a series like Cl+, Clo, Cl— a Similar curve is followed, especially Since we know that 700 (C10) = +.42 and ya3(Cl-) = -45.89. Recent calculations of field gradients in ionic lattices,with the assumption that the charged nucleus may be replaced by a point charge in PrCls (47) and CrCls (48), have yielded reasonable answers when compared to experimental results using an antishielding factor of -10. Since these two compounds are expected to be highly ionic a value closer to -27.04 would probably be more realistic since the experimental values are for less ionic compounds. Correspondingly a lower value for compounds studied in this work is appropriate as they are more covalent than the compounds used in the "experimental" determination of the antishielding factor. Unfortunately the calculation of the contribution of point charges to the field gradient at a quadrupolar nucleus is very sensitive to the Sternheimer factor because qzz(crystal) = (1 - 7a))¢zz' where 022 is the direct contribution to the field gradient from the external point charges. The large discrepancy between the calculated and the empirical factor is very disappointing and makes it 56 Figure 5. A plot of the Sternheimer factor (700) versus ionic charge for helium-like ions. 57 difficult to extract information from a point charge calcu- lation. (2) Modification of the electronic structure or molecu- lar unit as a result of interactions with neighboring mole- cules. The exact nature of these interactions is not well understood; however,Van der Waals interactions and dipole moment interactions probably occur. The latter interaction results in a small increase in ionic character of the bond and lowers the crystal energy. Table 5 presents the quadrupole coupling constants for a number of molecules in both the gas and the solid state (45). It will be noticed that for chlorine and bromine the coupling constant decreases in going from gas to solid. This implies a gain in negative charge on the halogen atom and, hence, an increase in ionic character. For iodine in ICl and ICN the absolute magnitude of the coupling constant increases implying a gain in positive charge and, hence, an increase in ionicity since iodine has a positive charge in these two compounds. (5) Additional bonds may occur between neighboring mole- cules in the solid. Examples of this are hydrogen bonding and formation of polymer-type structures in the solid. This latter behavior has been postulated to explain the NQR re- sults for solid 12, Bra and ICN. In 12 an examination of the crystal structure places two near neighbors each 5.543 from one of the iodine atoms in the iodine molecule. The sum of the iodine Van der Waals distances is 4.552; therefore, some «3) a nu. 1 t Qc n n s A .‘Qnd - ~ .~.~..J \ - ..\. 58 o.mwmml 0.0Ndml d>.NmNmI HumH ZQH o.>momu o.¢¢mml fi>.NmNNI HSNH HUH o.mmoml m.m¢fiml a>.mmmml Hbma Homo o.wm>al o.mmmfil H>.Nmmml Hhma Homo mfi.o 0.6msm- as.mmmm- Htmd NH 0.406 o.mam ms.mms ummk ummmo m.mmm o.>>m m>.wm> Hmmt ummmu om.o mm.mm> m>.wm> Hmmt mum ¢.¢>I m.mm| ¢>.m0fi| HUmm HUH mm.>ml mo.mwl ¢>.moal HUmm HUth «.mml ¢>.¢>I ¢>.moal HUmm HUmmo mm.moa| ¢>.m0fil Ho NHU mm c Uflaom mmw mumum UHEoum msmHodz masomaoz UONm vONm UOmw mumum msommmw mnu CH pom oflaom map CH nuom UmHSmmwS comm m>mm SUHAS mmasomaoz mcflsflmucoo :mmonm mo mu:Mumcoo msHHmsoo maomsuomso .m magma 59 kind of partial covalent bond must be formed between adjacent iodine molecules. This type of bonding has also been postu— lated for some Sb and Bi compounds (45,46). Examples of hydrogen bonding were studied by Allen (57), and Bray and Ring (58). Their data are given in Table 4. Table 4. NQR Data Indicating Hydrogen Bonding Compound Reference Frequencies (in MHZ) CC13CH(OH)2 57 58.190, 59.429, 59.515 CC13CH(OH)(OC2H5) 58 58.516, 58.705, 59.14 CC13COOH 57 39.967, 40.165, 40.240 The crystal structure of CC13CH(0H)2 has been determined by Kondo and Nitta (59). They find three C-Cl bond distances of 1.79, 1.78 and 1.72A; the two longer distances are at- tributed to hydrogen bonding of the hydroxyl hydrogens to chlorines in near neighbors. The quadrupole resonance fre- quencies for this compound shows a similar grouping, two lines quite close together and one line lying over 1.MHz lower in frequency. The explanation for this is that the two chlorine atoms engaged in hydrogen bonding give rise to the two high frequency lines and the other chlorine atom accounts for the lower frequency line. The lower frequency should be taken when studying the C-Cl bond in the compound and the .- pa ,- .100» ‘5..- . - ofle .1. u a In‘ .1 \ ..~ I . ~ .F-u “Ind A 1 ‘ h H...“ -- a" 9.,“ '1 . \u.‘~ . ‘s {I} 40 difference between an average of the higher frequencies and the lower frequency may be interpreted in terms of a charge Shift in the region between the carbon and chlorine atoms due to the formation of the hydrogen bond. This charge shift will undoubtedly affect the ionicity of the C-Cl bond and, if this is the only effect, NQR data may be used to estimate the extent of charge shift and hence the strength of the hydrogen bond. However, this charge shift may also be accom- panied by a change in the Sp hybridization of the Cl orbitals and this would complicate the interpretation. More data are needed for this type of compound before quantitative state- ments may be made. For CC13CH(OH)(OC2H5) one hydrogen bond is expected and the data roughly indicate this but the situation is less clear-cut; probably the hydrogen bond is not as strong. In trichloroacetic acid no hydrogen bonds are ex- pected and the data indicate that none are formed. Chemical Interpretation of NQR Data A. Atomic Field Gradients Let us first consider an atom. What will be the contribu- tions to the electric field gradient at the nucleus from the electrons of this atom? Suppose we had an electron in an atom described by the wave function wnfim when n is the princi- pal quantum number, £ is the azimuthal quantum number and m is the magnetic quantum number. The quantum number m used here should not be confused with the nuclear Spin quantum ..w" .. ~-- .71— I. l- U . . a u... 1 a :L 9‘ 1. ‘v-H ‘01» abv nub :.., s“ \nfl .\U \ y 's V\ 41 number m used previously (it is common notation to use the letter m for both of these quantities). The operator for ; 5cosae—1 q is 322 -—;3———-, where 9 is the angle between the z 22 axis and r. Then, in an obvious notation, 5cosae-1) anm = ‘9 fwn£m(”—"3'—r (Dngmdv . (59) If we use this equation we can estimate the relative import- ance of contributions from p(£ = 1), d(£ = 2) and f(2 = 5) electrons and also how q varies with the principal quantum number of the contributing electron. If we use hydrogen- like wave functions Equation 59 may be evaluated to give the result qnflm = 2£+5 7 (4O) furthermore, 1 2 2.3 = i 53a31(1 + 1)(2£ + 1) ’ (41) where Zi is the charge on the atom and a0 is the Bohr radius. a constant. Combining Equations 40 and 41 we get 4 Zi3 e qnzm = n33.3(z + 1) (21 + 1) (21 + 5) (42) Using Equation 42 for some fixed value of Zi and n, qnfim varies in the ratio 1/50:1/105:1/252 for p, d, and f elec- trons, respectively. We see then that q falls off quite rapidly with z. This effect is illustrated in Table 5, in which both the experimental and calculated (using Equation 42) Table 5. Values of qnflo = ggg-for Various Atomic Statesa Experimental Relative Electronic Value for Value of State Atomb qn£0 x 10‘15 anO c 5p I -45.0 1.00 5d Cs -0.51 0.14 5f Cs --- 0.048 6p CS -5.4 0.58 6d Cs —0.16 0.08 6f Cs --- 0.028 7p Cs -1.1 0.56 7d CS -0.09 0.05 2p F -21.0 1.00 5p Na -0.7 0.50 4p Na -0.2 0.12 aC. Townes and B. Dailey, J. Chem. Phys., 11, 782 (1949). bExperimental data are available only for these atoms. CObtained using Equation 42. Values are relative to 5p except for F and Na which are relative to 2p. 45 values for q for a given valence are tabulated. It can be seen that the relatively simple Equation 42 predicts in- tensities fairly well. In the next section we develop an equation for the ratio p -_— eEquO 1 eaoqat (45) where qmol is the molecular field gradient at the position of the quadrupolar nucleus and qat is the field gradient at an identical free atom nucleus. The values for qat are obtained from the splitting of atomic Spectra and also from atomic beam experiments. The atomic beam values are much more accurate. In obtaining qat the Sternheimer factor must be taken into account due to the polarization of the inner electrons by valence electrons; this effect must also be considered for q Most chemical interpretations of NQR mol' are given for p rather than ean and it has been previously assumed that taking the ratio cancels out the effect of polarization of the inner shells but for this assumption to be true 700 for free chlorine atoms must equal 700 for a chlorine in a covalent bond. Let us examine this assumption more closely. If the bonds of a molecule are covalent enough that the direct contribution to the field gradient from extern— al charges may be considered to be essentially zero, then the measured coupling constant e20q may be considered to arise entirely from the valence p electrons of the nucleus. These electrons will certainly distort the inner electrons inducing 44 enielectronicquadrupole moment characterized by a Sternheimer factor of 70S; hence,the measured coupling constant e2qQ e e2qm01(1 - 70$)Q. However, the free atom field gradient qat also arises because of the gradient due to valence p electrons (although it is not the same as qmol due to charge distortions arising from bond formation) and induces a quadru- pole moment in the inner Shell described by 70;. Thus, ezqétQ = eaqat(1 - 703)Q, but because the same mechanism causes the inner shell distortion it is believed that 705 = was; then p = qmol/qat’as desired. This is probably a good assumption. However, when there is appreciable ionic character in the bonds to chlorine (for example, in SnCl4, HgClg, SbCls and other similar compounds) the contribution to the field gradient due to external charges and valence electrons is expected to be more nearly equal and the measured coupling constant must be written as ean =e2<2[(qmol(1 - 705) + 4’22” - ymn, (44) where ' 705 + 7a): €20¢zz(1 - 700) must therefore be calculated and subtracted from the measur- ed equ before p is calculated. B. The Townes and DaileyfiTheory of Molecular Field Gradients The following treatment is taken,in part,from Das and Hahn (8). It Should be kept in mind that no completely gener— al treatment for the molecular field gradient has been given; 45 the theory of Townes and Dailey was developed for the particu- lar case of the singly bonded halogens although it may be generalized for other atoms if they are fairly electro- negative. In general, however, it is better to consider each nucleus separately and test each approximation of the Townes and Dailey theory to see if it applies in the particular case. All the NQR resonances reported in this work are chlorine resonances; therefore, the original development of Townes and Dailey seems appropriate. The arguments of Townes and Dailey should be regarded as heuristic rather than rigorous. Let us consider how qat of chlorine is modified when the chlorine is bonded to another chlorine in the C12 molecule. The bond is not expected to have any appreciable ionic character, double- bonding or pd hybridization; however, a small amount of sp hydridization may take place. The bonds use the chlorine pz orbitals and the direction of the z principal axis is along the chlorine-chlorine bond; cylindrical symmetry may be as- sumed. Then the electronic distribution in the valence shell of the bound chlorine atom may be described by the following four wave functions: ¢6= a? s + (1 «not pZ wx=px wy=py ¢£p'=(1_a)és- Qipz The measured value for qat corresponds to the integral of atomic wave functions 46 _ 5cosae-1 _. = -x- . qat _’qn£m (w nEO ( r3 ) wnfiO dV ’ m = 0 for p electrons E = 1 and we must also consider the atomic field gradients qn£1 :nd an-1 which are related to anO by = .. L . ' = = ‘45) qnzm qn£O[1 1(e+1)]' thus' 1f qn£0 qat’ qnz1 an-l = -§-qat. This means for a chlorine with one pz electron we get sz (atomic) = qat and—Vxx = Vyy = - i-qat, but if the electron were in the px orbital then VXX = qat’ Vyy = - fi-qat and sz = - é'qat' In order to describe the electronic state of the chlorine atom in this molecule we consider the wave func- ' ,, ; . = + + + . tions wé,w£p wx and wy then q an6 nfipq‘gp nqu nyqy where n = the number of the electrons and, for example, * 5 829-1 qcs = ((6 (—9%3—-—) ‘(6 9" *(5cos29-1 ‘err—-—9 * 5cosae-1 (-——s————) dfs st + (1-d)fpz r pde +-dé'(1-coéjs*(§9%§i§:;)pzdv + 12(1-a)§ fpz*(§£%§3§:;) sdv. The cross products are ignored because the atomic wave 2— functions are orthogonal and fs*(§£9§3§—i)sdv = 0 because the s electrons are spherically symmetric; hence, q6 - 2- (1-d)fpz*(§99§3§—i)pzdv = (1-c0qat. Below are listed the contributions to the molecular Vxx’ Vyy and sz from the various wave functions. 47 Number of Electrons in Orbital the orbit V V V xx gyy 22 (o 1 —i~~(1-a)qat -g-(1-o:)qalt (1-o)qat (X 2 ant -qat -qat (0 _ _ Y 2 qat ant qat ((1 ._ _ Ep 2 Oqat Oqat 20gat §‘(1-oz)qat §(1-wqat (-1+c1)qat We can see from the above that q E sz = (--1+'CL)qat and n = 0. If our bond had some fractional ionic character I, then the number of electrons in $6 would be (1+1) and if the bond had some fractional double bond character‘flpthen the number of electrons in wx and ¢y would be (2 - g),so q = [(-1+a)+ (1-O)I -l-Tr]qat but 1} still is zero. Let us now consider a chlorine atom in a planar molecule such as a chlorobenzene, then only the pX orbital takes part in double bond formation so that the orbital populations P become P(6)=1-I P (x) = 2 —'rr‘ P (y) = 2 P(£p)=2 and the field gradients become vxx = [§(1-a)(1-I) -7T]qat vyy = [141-a) (1-I) + 5777 qat q = sz = [(1-a)(I-1) + 17771.” = 512‘. 1 n 2 p ° 48 Thus, if n can be determined for these molecules an independ- ent determinationcflTTTis possible. We now attempt to derive the above equations in a more rigorous manner. For an ICl molecule we may write an LCAO wave function 2(c1 + i (I w =(1 + i2 + 213)%' (46) where S is the overlap integral fwlwcldv and i is relative contribution of (I to the total wave function. The ionic character of a bond is defined as I = %—i—%§-with ionic character in the bond being allowed for by the parameter i. However, if we consider the bond as being formed by the pz orbitals of I and Cl then it is known that a stronger bond will be formed if we allow some admixture of other states with the pure pz state. Energy and symmetry considerations suggest that the most likely states to mix with pz are s and dzg states; with this in mind we write the atomic wave func- tions as (c1 = (1-dsé)% pz(Cl) + d? s(Cl) + 6% dzg (c1) (47) WI = (l-a‘~5')§ pz(I) +(a')§ s(I) + (6')é-dzg(l). Four different contributions to qmol at the chlorine nucleus will now be considered. They are: 1) The two electrons in the molecular orbital Equation 46; 2) The two pairs of pX and py electrons on the chlorine atom: 5) The electrons which were in the 552 orbital in the free atom. These electrons 49 were previously accounted for with tap because in the mole- cule they are lone pair electrons; 4) The inner shell elec- trons. 1) The two electrons in the bonding orbital give rise to 2 q ='J¢*(5CO: 6-1) ¢dV __"2 .2 . _ (1+12+Zis)% [quC1 + l qII + 21q1c1] ’ where, in an obvious notation, qICl E ((1 (5co::9-1)wC1 dv' The term qII gives the contribution of the bonding electrons to the field gradient at the chlorine nucleus when the elec- trons are near the iodine nucleus. Because of the %3-term, qII is very small and is neglected. The term qICl arises because of contributions from the overlap region. The value of qICl is certainly less than quCl although not as small as qII' Furthermore, it is multiplied by 2i where i is less than unity. If the bond which contains the chlorine nucleus is quite ionic then i is small, but in the case of ICl Townes and Dailey estimate the ionic character as 0.25 and from this i =(l775. Reddoch (7) has stated that for i = 1 the error involved in neglecting qICl is no more than 10%; however, he does not say how this estimate was made. Although we will neglect qICl this may not be correct for co— valent compounds. If we use Equation 47 for (C1 we obtain 50 = _ _ ‘ é- . quCl (1 Cl é)qat(Cl) + qu22(Cl) + Edi-0 qsdzz(Cl), where we have neglected two cross terms which are zero be- cause of symmetry. 2) Each of the four electrons in the pX and py orbitals contributes -§-qat to field gradient as discussed previously, giving a total of - qat' 5) The two lone pair electrons contribute nothing to the atomic field gradient but in the molecule the pure s state gains some pz character. They then contribute an amount ~2d qat' 4) The inner shell electrons of chlorine should contribute nothing to the field gradient but because of polarization by the valence electrons small corrections should be made to qat; however, these may be made by using a value of qat which has not been corrected for polarization when we calculate the ratio p = Egggja . This correction has been discussed, it will not suffize for qdzg and qu22 but we are planning to neglect them so will not bother with a correction. Collecting all the contributions to the molecular field gradient qzz(Cl) we write _ 2 __ it. qzz(Cl) - 1:12:2i5 [qat(1 d 5)+éqd22 + Zdéb qSfiz?]' (48) In order to Simplify this equation into an easily usable form, we wish to neglect éqazg, dédéqsazg and the overlap 51 integral product 2iS in the denominator. The term éqd.2 may be safely neglected because both 6 and qd 2 are quite small, 6 being usually less than 5%, and Tabl: 5 shows ap- proximately an order of magnitude decrease in the qat result- ing from d electrons compared to that from p electrons. The product débéq sd 2 may not so easily be neglected. There is ‘ 2 no simple way to calculate qsd 2 and no experimental values 2 are available. Although its value is eXpected to be smaller 5% than q , E qat’ is expected to be smaller than d5, hence 92 the product dédg is less than d. For these reasons Townes and Dailey neglect dédtp Let us now consider the denomi- sd 2' nator of Equation 48,(1 + :2 + 2iS)-l. A typical value for S falls in the range 1/5, hence for a molecule like C12 or Bra where i = 1 the denominator becomes equal to [1 + 1 + 2(1)(%)] = 8/5: Therefore, according to Equation 48, for these molecules p =-§:%§-—- should equal 5/4 if we neglect sp hybridization. .However,athe measured p values for these two molecules are very close to unity, which is the expected value if we neglect overlap. Gordy (60) has discussed the inclusion of S in the Townes and Dailey formulation. He argues that the overlap term is included to take into account the contribution to the molecular field gradient which comes about because of some charge migration from around the quadru- polar nucleus to the overlap region and this charge must come from the outer regions of the quadrupolar atom. Since the major contribution- to the field gradient comes from the 52 electronic charge close to the nucleus the effect of the overlap migration is negligible. This argument does not seem valid as it only considers the direct effect of the charge migration and does not consider indirect contribu- tions to the molecular field gradient which must occur as a result of decreased distortion of the inner shells by the outer shells. Furthermore, the Townes and Dailey theory attributes the difference between the free atomic field gradient qat and the field gradient of an atom in a chemical molecule qmo entirely to the valence electrons which, of 1 course, are the electrons which migrate into the overlap region; Gordy conveniently overlooks this point. A more reasonable argument is advanced by Das and Hahn, who refer to some calculations by Schatz of coupling constants for 35C1 in the compounds HCl and CH3Cl (61), and by Das (62) of the coupling constant for 11B in some boron compounds. They find that due to a contraction of atomic orbitals on molecule formation qu may not be strictly equal to qat’ This effect may be partially corrected for by neglecting the overlap integral in the denominator of Equation 48. This explanation for the consistent interpretation of NQR data with the overlap integral set equal to zero, in terms of two cancelling effects, seems more reasonable than Gordy's argument. It also suggests that we must be careful to watch for cases in which we do not get a self-cancellation of effects. After neglecting the terms just discussed Equation 48 becomes 55 _ _:21-w6) _ qzz(C1) - I 1 + i c1.at + 2(1 wqat] (4.9) . . . _ 1 - 12 . which, substituting I — 1 i Equation 49.becomes qzz(Cl) = [(1-oc+c5-I) + I(a+<5)]qat- (50) We neglect the second order terms Id and Id (although in rare cases Iczmay need to be included) to obtain qzz(Cl) = (1-d + é-I)qat. (51) If we wish to correct for double bonding we define a quantity 'Wras the electron density in the px(or py) orbital of a free chlorine atom minus the electron density in a pz (or py) orbital of a bound atom and call this quantity the fractional double bond character. The population of each px (or py) orbital is (ZJHT and qp (C1) = - (é -7T)qp (C1); the pX and py electrons now contribute an amount q” =z-2(15U76at to qzz(Cl) instead of -2qat. Including this correction in Equation 51 gives qzz(c1) = (1-a&é=n=l)qat. (52) This is commonly referred to as the Townes and Dailey equation as these two authors derived it originally and it has been used successfully in interpreting NQR data from hundreds of compounds. In a similar manner Equation 55 may be derived: q(I)= [1-o&é+I:U]qat(I)o (55) 54 Cotton and Harris (65) have recently developed an equation similar to that of Townes and Dailey but from the molecular orbital, rather than from the valence bond, formalism. These authors claim that under appropriate limiting conditions their equation reduces to the Townes and Dailey equation but they do not explicitly state these conditions. It is interest— ing to note that their derivation is much more general than that of Townes and Dailey, not requiring an explicit intro- duction of hybridization. Their proof is no more rigorous than that of Townes and Dailey, although they do attempt to pro- vide a numerical corroboration of their most important assump- tion. The derivation of Cotton and Harris is given below. It is desired to calculate the quadrupole coupling conStant ezoaqa for a molecule which contains a quadrupolar nucleus designated by a. The wave function for the molecule may be expressed by a product wave function Y =7gik, each wk containing Nk electrons. Each molecular orbital wave function wk may be expressed in the LCAO-M0 approximation as: wk = r21 Cik(>1 (54) i=1 where n is the total number of atomic orbitals ¢i of the atoms in the molecule and all the ¢i are required to be orthogonal. The total field gradient in the molecule thmay be written as NUCL C q_ = Z qu k-+ NUCL where q is the contribution to qa from the charged nuclei of the surrounding molecule and neighboring molecules and qaf is defined by the equation 55 k 2 - k qak= M *(i‘aisfl) 1 av . (55) Using Equation 54, Equation 55 becomes _ k ,k k lj. NUCL; . qa-E§§NC1C. qa+qa (56) ‘ 3 where qij _ f¢: (5cosa re-1)¢i dV . Cotton and Harris then break down Equation 56 into three sums, one for each of the following types of qij: 1) qii, one-center integrals in which both Ii are on the quadrupolar nucleus. 2) Two-center integrals qij and qgé, where i refers to atomic orbitals centered on the quadrupolar nucleus, and 5) qgfwhere neither j nor fl refer to atomic orbitals on the quadrupolar nucleus. With this arbitrary grouping of terms they now write Equation 56 as _ k jj K k ij qa - 2:ka [ZiIICi qu (11+ ZICj I2 qa + chi Cj qa + z c. kc kqul + qa NUCL . (57) 3'13 j E Equation 57 must be simplified as it would be impossible to solve this equation in its present form by any presently known methods for most molecules of any chemical interest. In order to make simplifications the following three 56 approximations are introduced: 11 The sum over all core orbitals on atom unwill be taken as a constant P. Although this contribution should ordinarily be zero, the Sternheimer effect will cause some contribution to qa; thus, Elcikleqaii becomes 1 in in a 2 'l'l 2 EICi'kl q; l + :2 lci"k| q r 1" III M 0 ij" + q NUCL 2) The sum over two-center integrals go. a, ,where j" refers to a core orbital, will be approximated by a constant CORE a which corresponds to contributions from all charged q nuclei and their core electrons external to atom a. 5) The sum over all non-core two-center terms qzq, plus one- half of the sum 2 Cikcjkqtg, is assumed to exactly cancel i,j Core. Cotton and Harris attempt to justify this assumption a by computing the field gradient at one chlorine atom due to the net effective charges on all atoms of PtCl4-. They find, that in this case, the error made in neglecting this effect amounts to about 2.5% of the total field gradient. They do not, however, give anough details of this calculation to allow an estimate as to how good it was. 4) All three-center integrals are neglected. With these assumptions we may now write k'z i'i' k k i'j' [i.lci' qa +§I>i'ci, cj, qa ]+ P . k qa =ZN k Using the Mulliken-type approximation (57) i‘jf _ i'i' qa -Siljl q(l I we write 57 _ i'i' _ k k 2 k k I 3., 1], C1. i' 1 k j'>i' 3 1'j (59) where fi' is the molecular orbital expression for the occu- pation of ¢i° When Equation 59 is multiplied by eerswe get 2 2 = 2 i'i' e 055 e Qaqa E. "‘Ei'[e qa Qa+ >3 fi' 1 ° (60) il The term in the square brackets is then replaced by eaoogat’ then with Nk replaced by 2-Nk (since chlorine has one hoIé in the p shell) we finally get e20 q pa=‘—z——Q‘L = Z l e Qaqat l 3 z (Z-Nk)[‘Ci¥l2 + ' Z c.k c.k s. ..1. k . (61) This equation has many potential advantages over that of Townes and Dailey although much more extensive computation is needed when it is employed. However, it is not yet clear whether the assumptions involved are any better than those of Townes and Dailey. C. Evaluation of the Parameters of the Townes and Dailey Equation From Equation 52.p = (l-afié-I:"Y, and since we know ezqatQ and may measure e2qQ this equation may be used to interpret our experimental data in terms of bond parameters. However, we have only one measureable, p, and four parameters; therefore, we must estimate three of the parameters by other means in order to calculate the fourth from our experimental 58 data. It should be emphasized that all methods discussed in this section apply only to the interpretation of halogen NQR data. Townes and Dailey (65), and Gordy (66), have discussed approximations for obtaining these parameters. Gordy has madetnwaapproximations both of which neglect hybridization. In the first he sets 0,5 andjn—equal to zero and calculates the bond ionicity from the equation p = 1 - I. For compounds in which some double bonding is expected Gordy sets the ionicity I = fi-AX where AX is the difference in electronegativ- ity between the two atoms forming the bond. He then calculates 77 from the equation p = (1-IJWT: again neglecting hybridiza- tion. Values of 77-calculated using his second approximation are quite reasonable but his neglect of hybridization is not. For example the compound ICl has a coupling constant of 80 MHz and eaQqat(Cl)= 109 MHz; no double bonding is expected in this compound hence, neglecting hybridization, about 28% ionic character is calculated. This seems much too high and it is reasonable to invoke hybridization to explain this dis- crepancy. Gordy‘s assumption of I = fiAX is probably roughly correct, but it gives ionicities which are too high in the region of AX = 2. Whitehead and Jaffe C67) have used this same approximation but they use modified electronegativities. Townes and Dailey have also used two approximations, in the first dp hybridization has been neglected. This is reasonable for the halogens since the difference in energy between the p and d states is large and an upper limit of 5% probably may nay “va- .0‘ "r ~\ 5 (I, “J 59 be set on dp hybridization for the halogens. They also neglect double bonding and estimate 0 according to the following rule: if the atom to which the halogen is bonded is less electronegative than the halogen by 0.25 units or more,then d== 0.15, otherwise a.= 0; 6 is always less than 0.05. This rule was proposed by Townes and Dailey partly from a consideration of compounds of the group V and VI "elements" where 5 character of the bond may be estimated from the formula = cos y . a 'I:E$E$ (62) where ¢ is the angle between the bond in compounds where the group V and VI element is the central atom. Dailey (68) has re-examined this rule for a series of simple alkyl compounds. He finds that for halogens involved in C—Cl, C-Br or C—I bonds the factor 0.15 in the Townes and Dailey equation should be replaced by 0.156, 0.086, and 0.016, respectively. This takes into account both Sp and dp hybridization. Coulson (69) has calculated that maximum overlap occurs at about 50% sp hybridization but the curve of overlap versus sp hybridiza- tion is quite flat and 25% s hybridization would not cause a large decrease in overlap. The percentage of s hybridiza- tion is governed by two competing effects, the energy needed to promote s electrons into the p orbital so that hybridiza- tion may take place and the bond energy gained by reason of additional overlap. (Thus, 5 hybridization in the 6O neighborhood of 25% is favored. In addition, the s hybridi- zation of the group V and VI elements as calculated by Equation 62, varies between 10 and 25%. Finally, it is known that the amount of hybridization increases as the ionicity of a bond increases. All these facts indicate that the Townes and Dailey treatment of hybridization is quite reason- able. When double bonding is expected to be important, Townes and Dailey use the equation = aiRi + 532R2 R a1 + 532 , (65) first derived by Pauling. In this equation R is the ob- served bond distance in the compound under study, R1 is the sum of the single-bond radii for the two atoms involved in the bond, R2 is the sum of the double-bond radii, and a1 and a2 are the fractional importance of the single and double bond structures, reSpectively. Since R1 and R2 have been tabulated by Pauling (70), and by Townes and Schawlow (71), and since a; + a2 = 1, a2 E Trmay be calculated if R is known. To correct for some anomalies observed in internuclear distances in fluorine compounds Schomaker and Stevenson (72) have suggested that R; be modified to R1' by the equation R1' R; -0.09 AX, where AX is the electronegativeity dif- ference. However, in other compounds the correction itself introduces anomalies so it is probably better to disregard it. For well defined covalent bonds, such as a C- C or C— H 61 bonds, Equation 63 is fairly reliable, but for bonds like Sb-Gl or P-Cl it has more qualitative than quantitative significance. Using these rules to obtain a and;(, Townes and Dailey have calculated the bond ionicity I in a number of compounds and have constructed a graph of ionicity versus AX from which it is possible to estimate the ionicity of any bond with the aid of a table of electronegativity. Their graph is reproduced in Figure 6, along with those of Gordy and of Pauling,for comparison. Townes and Dailey argue that their graph is more accurate than Pauling's because Pauling based his values on an incorrect interpre- tation of dipole moment data. Although the Townes and Dailey equation (Equation 55) is probably quite good, and for the purposes of comparing a series of similar compounds quite reliable, their treatment loses much accuracy when the various rules are applied to evaluate the parameters in individual cases. Townes has estimated that these approximations are accurate to about 25%. Equation 61 derived by Cotton and Harris,offers certain ad— vantages since their parameters may be calculated much more accurately than those of Townes and Dailey and thus interpretations for individual compounds will be more re- liable. The best approach at present to the interpretation of the NQR data must be to interpret changes within a series of chemically related compounds as a function of the change in one specific parameter. 1.0-L O’Bq'b Ionic character 62 Figure 6. 1'. 0 2‘1 0 Electronegativity difference Ionicity versus electronegativity difference according to the approximations of Pauling (70), , Gordy (60), and Townes and Dailey (44). 63 Previous NngStudies of Charge Transfer Complexes Douglass (2) was the first to study a charge-transfer complex with NOR techniques. He studied complexes formed by chloranil with several donors. The only compound in which an NQR absorption could be found was the complex of chloranil and hexamethylbenzene. If charge transfer takes place as expected from the hexamethylbenzene to the chloranil, a charge shift from the chloranil ring to the attached chlorine atoms is‘ expected. This charge shift, by increasing the ionicity of the bonds,should decrease the BQIINQR absorption frequency. Douglass observed a slight increase in the absorption fre- quency which he explains by invoking solid-state effects. In substituted benzenes the crystal splittings are about 200 kHz and Douglass points out that the frequencies which result when 200 kHz is subtracted from his measured frequencies correspond to an increase in ionicity in the C-Cl bond of chloranil in the complex. On this basis he obtains an upper limit to charge transfer. There is, however, no good reason for expecting a crystal field effect of this magnitude or even this direction. In organic complexes two types of electron donors are commonly recognized. The first is a w-donor, which donates charge from wabonds, such as carbonyl bonds, multiple bonds, etc. or donates charge from the w- I cloud above an aromatic ring. The second is an n-donor which donates charge from lone-pair electrons. Charge-transfer complexes formed by transfer of W-charge are known to correspond VA Iv' 5n to. UT. RA 5v 5!- ~l.‘ II 64 to the weakest charge transfer (75). Moreover, charge transfer into the w-cloud of chloranil may not redistribute itself in a simple manner. HOOper (5) has studied the resonance frequencies of 35C1 in a 1:1 complex of CC14 and p-xylene and the 79Br NQR spectrum in CBr4.p-xylene and Bra-benzene. The halogen resonancesin.CCl4, CBr4 and Bra show only a negligible shift in frequency upon complex form- ation. Since the above complexes are uncomplicated by #- cloud effects on the acceptors these results indicate that the charge transfer is too small to measure by this method. Duchesne et al. (4) have studied a series of charge transfer complexes between bromine and some substituted benzenes and the results are given below. Table 6. Frequency Shifts Upon Complex Formation Between Brg and Some Substituted Benzenes. Compound Br Frequency Shift (MHz) C6H5°Br2 +0.107 C5H5F-Br2 —0.04 C5H5C1°Br2 -0.026 C6H5Br°Br2 '1.706 The frequency shift for the bromine in CeHsBr is —10.384 MHz, while the frequency shift of the C1 in C6H5Cl is only -0.004 MHz. These results generally support the work of HOOper and Douglass except in the case of the CeHsBr'Brg 65 complex. Duchesne et al. explain their results in the follow- ing manner. For the first three complexes the only mechanism for complex formation is a donation of charge from the #- cloud of the ring to the bromine molecule and this type of charge transfer increases the electron population in the anti- bonding 4pz orbitals of the Br atoms. This distribution should be spherical to a first approximation and thus have little or no effect on the Br NQR absorption frequencies. Nevertheless, if any appreciable charge transfer takes place it is puzzling that no frequency shift takes place for the chlorine frequency in chlorobenzene. In the complex CaHsBr'Brg, however, another type of charge transfer complex may be formed in which the bromine atom of bromobenzene may donate some charge from its lone—pair electrons to the bromine molecule. This type of complex is much stronger than a W-complex (75). Accordingly large shifts for both the bromine molecule and the bromine atomcflfbromobenzene are found. It is unfortunate that it was not possible to find an absorption in the complex C3H51°Br2 as CeHsl is also expected to be an n-donor. Grechishkin et al. (6) have studied the 1218b, 35Cl and 81Br resonances in a series of molecular complexes of SbCla and SbBr3 with substituted benzenes and ketones. They find only negligible shifts for the halogens (in those compounds where it was possible to find halogen resonances) and larger shifts for the antimony. These data agree well with the data previously discussed for w-complexes. Since the antimony is 66 the recipient of the w-charge it is logical that larger shifts 121Sb is about 10 times are observed; however, e2Qqat for that for 35C1 so the relative shift for antimony is negligible. From the above discussion it may be concluded that NQR studies have revealed only a negligible shift in the resonance fre- quencies for quadrupolar nuclei involved in w-type charge- transfer complexes. The probable reason for this is that such a small charge is transferred in the formation of the w-type complexes that other things obscure the effect of charge trans- fer on the NQR data; on the other hand, as exemplified by the CsHsBr°Br2 data, n—type charge-transfer complex formation has a noticeable effect on the NQR resonance. For this reason a series of n-type charge transfer complexes formed between quinoline, pyridine and some pyridine derivatives with ICl and IC13 were synthesized during the present work. Unfortunately, a search on several of the compounds over a frequency region which should have contained the 35Cl resonance frequencies for ICl and IC13 did not yield any absorptions. There is no apparent reason for this failure. Much stronger charge transfer complexes have been studied by Dehmelt (8) and by Biedenkapp and Weiss (9). These com- plexes are strong enough so that they may be considered to be formed from a Lewis acid-Lewis base reaction and in these the shifts in the chlorine resonances studied averaged greater than 1 MHz. It was thought (74) that this was outside the range of frequency shifts which may be attributed to crystal b" it V i (Y‘ of. \A/ an H H r o.\ n 67 field effects. Of particular interest are the shifts in the two complexes ASClg'POCls and SnCl4°2POC13; the chlorine resonance frequencies together with the previously measured frequencies for the pure components are given below in Table 7. Table 7. NQR Resonance Frequencies in Charge Transfer Com— plexes Compared to the Resonance Frequencies in the Pure Compounds Resonance Resonance Frequenc1es Frequencies Compound (MHz) Compound (MHz) POC13 28.995 SnCl4 24.294 28.958 24.226 AsCls 25.406 24.140 25.058 25.719 24.960 SnCl4-2P0C13 50.215 ASC13°POC13 29.208 50.117 29.168 21.146 29.154 19.807 24.481 19.055 25.125 24.799. An inSpection of Table 7 reveals that each complex has two distinct groups of frequencies. group may be associated with the chlorine resonances of P0C13 The higher frequency u ‘91-. * I . 4.4! ‘- u . I. -. ‘1: Hr in *5 3" ‘.I ‘6‘ 1.. R5“, 5VAL~ . 4. ...a_ n . "deu ‘Vcl. (I, ’ A ’. : (n MP- \- 68 and the lower frequency group with those of the Lewis acid. We find that the chlorine frequencies in SnCl4-2POC13 have large shifts relative to the uncomplexed molecules. These may be qualitatively explained in terms of a simple model in which the charge transfer from the oxygen atom of POC13 to the tin atom results, by induction, in an increase of electron density on the chlorine atoms of SnCl4 leading to an increased ionicity in the Sn-Cl bond and a decrease in ionicity in the P-Cl bond. Thus, the NQR frequency of the chlorine atoms of SnCl4 should decrease while that of the chlorine atoms of POC13 should increase as is, in fact, observed. For the AsC13°POC13 complex, only negligible changes from chlorine NQR resonance frequencies of the pure compound are observed. This may be explained on the basis that no complex, or at most only a very weak complex, is formed as indicated also by data from Raman spectroscopy (74) and from thermodynamic studies (75). In this study we have prepared a fairly large series of P0C13 complexes, although it has been possible to find resonances in only four of them. It was thought that the shifts in the 35Cl.resonance frequencies in the complex rela- tive to those in the uncomplexed components would give a measure of the acid strengths of the Lewis acids involved in these complexes. In addition, since quite accurate X-ray structures were available for several of these complexes, it was thought that calculations of the field gradient induced 69 by the charged nuclei in the crystal lattice, combined with the observed splittings of the NQR lines, would yield some information on the solid state interactions in these complexes. lunar Lah'bé int: #IL 7.. Der; Q 33);! II. EXPERIMENTAL A. The Nuclear Quadrupole Resonance Spectrometer 1) Introduction The problem of finding NQR absorptions is simple in concept. All that is needed is a spectrometer which pro- duces electromagnetic radiation in the proper frequency range, and whose frequency may be varied until an absorption is detected. Since all known quadrupole resonances fall into the frequency region between 0 and 1000 MHz, we need a Spectrometer which Operates in the radiofrequency region. In this investigation we shall be concerned with chlorine quadrupole resonances, which are expected to fall into the frequency region 0-55 MHz; most of the NMR absorptions of commonly observed nuclei also occur in this frequency region. Thus, it is not surprising that many of the experimental methods are the same. It is not practical to use the balanced-bridge method since the frequency must be scanned, requiring that the bridge be continuously rebalanced. It had previously been thought that the nuclear induction method was unsuitable for the purpose of detecting NQR absorptions because the twofold degenercy of NQR energy levels did not permit any net nuclear induction to appear. Recently, however, it has been found that the application of magnetic 70 9AA", nix/H“ Q 0" ‘01 L) F. ‘P‘. so; ' y «83‘ J a a 71 modulation of about 50 gauss amplitude removes the degeneracy well enough so that it is possible to detect NQR resonances by this method. Hartmann et al. (76), using a Varian Wide-Line NMR Spectrometer, have recently detected chlorine NQR absorptions in bis-ethylene diamminodichlorocobalt(III) chloride-HCl-Xflgo. They detected three resonances at approximately 5, 10 and 15 MHz due to igéi-é‘ ; ig—i-ig-and :t%-%:1:-§- transitions, respectively, by simply tuning the variable frequency Varian VF-16 oscillator by hand and observing the output on an oscillo- scope while the sample was in the probe and the field was modu- lated with an amplitude of about 50 gauss. However, the most common method for observing NQR absorption is by means of either marginal or supergenerative oscillator—detectors. These consist of a radiofrequency oscillator which is modified in such a way that it detects when the frequency is swept through a resonance. Marginal oscillators are in common use in wide-line NMR but superregenerative spectrometers are less commonly used because of troublesome Sidebands, even though they were originally introduced by Roberts (77) for use in NMR. In NQR work, however, the superregenerative oscillator is used almost exclusively, as it is much more sensitive than the marginal oscillator. This is an important consideration since, in general, NQR lines are much weaker than NMR lines. From now on we shall confine our discussion to super- regenerative oscillator-detectors as they have been used exclusively in the present work. 72 It is of interest to examine the factors which determine the signal-to-noise ratio AS/An in the output of our spectrOm- eter. Pound (79) has calculated this ratio for the case of nuclear quadrupole resonance and found that _ v.35 oi Af hBNQCIE‘)é 7 v)3 (I + m) (I - m + 1) n 2(1 + 1) 16 kT(kTBF)?T1E *1: for single crystals; this ratio should be reduced by a factor of 2/5 if the sample is in the form of a powder. VC is the effective volume of the resonant circuit, Q is the well-known quality factor of the resonant circuit, A is a constant very close to unity, f is the filling factor, V the magnetogyric ratio, No the number of resonant nuclei per cc, v the resonant frequency, T1 the relaxation time and (kTBF) an effective temperature T, bandwidth B, noise figure F for the spectrometer; T2*is a line width parameter roughly analogous to the Spin-spin relaxation time in NMR. It may be shown (16) that the optimum signal-to-noise ratio is obtained when 72H12T1T2*(I + m)(I - m + 1) = 1, where H; is related to the output voltage of the Spectrometer. Since T1 is gen- erally quite small (typical values being in the range of 1 millisecond) large values for the rf voltage are needed to satisfy this equation. This is one of the reasons why super- regenerative oscillators are preferred, since typical rf voltages of 20-150 volts may be developed across the coil of the tank circuit. Marginal oscillators typically only reach 75 about 0.5 volts, although Special circuits (82) are avail- able which can attain voltages in the range of about 20 volts. 2) Superregenerative Oscillators In Figures 7 and 8 are given the wiring diagrams for two oscillators which were constructed during the course of this work. The first has its circuit parameters chosen so that it works well in the frequency region of 15-55 MHz while the second works well in the region of 2-20 MHz. The lowest fre- quency NQR line observed was that of PrC13 at 4.5 MHz and the highest was that of CC14, which has its highest frequency line about 41HMHz, but the oscillators worked well as low as 2 MHz and as high as 55 MHz. In order to make clear some of the difficulties encountered in frequency measurement we will now briefly sketch the theory of the superregenerative receiver. The distinct feature of this type of oscillator is that the oscillation is periodically dampened or quenched. Two different modes of operation may be distinguished, coherent and incoherent. In the coherent mode the next oscillation cycle is initiated before the decay of the previous cycle to noise level, while in the incoherent mode the next cycle starts from the noise level. The inco- herent mode is more sensitive and most radio and radar appli- cations of the superregenerative receiver use this mode but in our applications we require transmitting and receiving properties so use the coherent mode. Operation in the coherent 74 ..uoumHHHumo iumz mmumav mmcmm smflm .s musmflm nocmso .U Hmsumuxm .JI «Hun M mama «no meW . . mudfio - 0*“ , mom i , , x mama mm Ia..u . mmzm .00. «000. mooo. am new mammfi HW_% Sow 2 0 . Mmm a.“ . sows xoom Soon mm mm: s¢.o HOO. ._T+ Ma 61 Hoo.o I I ___ H.o xma > mNm+ 0» oom+ +m 75 .Auoumaaflomo ANmS.ONINV mmcmm Boa .m musmflm m u Mm...” fl. M NfiNW [V 1H #0 HHOU - N%. mam.H. _ 8 88L 289289289 («8. 1 mm. - «moma mmzl 52. .H Ho __ mNTHWJ§3)\hHJ2§€LHLSZ<. O ozm 2mm 2mm #90 . fioo. Hmcmwm H o o ms cos :1 cos use coflumascoz >mmmloom+ +m . uqfl F .49 : 37.9. Gaffe: ind. . I'd? S qgenc ' a J: t3 ‘. ‘H Lu 3&2 76 mode gives rise to discrete frequencies rather than a single one. These frequencies consist of a center frequency, which correSponds to the actual frequency, of the oscillator, and two series of sidebands. If v0 designates the center fre- quency and v is the quench frequency, then the frequencies Q of the first series of sidebands correspond to the formulas v0 + v v0 + 2v v0 + 3v while the other series 0' Q' Q ° ' ' ’ correspond to the formulas v0 - v v0 — 2v v0 - 5v . . . . Q' Q' Q Thus, a quadrupole resonance absorption consists of a whole spectrum of lines, one of which is v0 and the rest are side- bands. Although in theory the amplitude of the sidebands should decrease as they are further removed from the central frequency, in practice the first upper and lower sidebands often have the same amplitude as the central band. This situ- ation is not too bad as we may pick the central frequency of the triplets as the center frequency. However, it often happens that the first and second upper sidebands are compara- ble in size to the center line while the lower sidebands are quite low in intensity or vice versa and in this situation it is impossible to pick out the center band. Both this problem and that of the closely spaced doublets and triplets of NQR lines will be discussed more thoroughly in the section on frequency measurements. The quenching action is brought about by periodically driving the voltage of the grid of the oscillator tube to a negative enough value so that current flow is stopped, there then ing c v I- vhf w u;n\ ”a-“ f \I'Juu‘n-x usua exte: 77 thereby dampening the oscillations. The oscillations are then restarted by withdrawing this voltage and again allow- ing current to flow in the oscillator tube. There are two methods for applying this quench voltage. In the first, commonly referred to as external quenching, a periodic voltage. usually a sine wave of appropriate frequency generated by an external oscillator, is applied to the grid of the oscillator tube. It was found by running test experiments under varying conditions that the best voltage for the external frequency was in the region 4-9 volts. The higher the voltage used the higher the quench frequency that may be used but as the quench voltage is raised undesirable modulation of the oscil— lator output is introduced. In general, it is desirable to quench at as high a frequency as possible consistent with the condition that a small amount of noise be alflDwed in the oscillator output. This noise generally increases as the frequency of the oscillator increases, and to keep the noise level down the quench frequency must be continuously raised as the oscillator frequency is increased. Increasing the quench frequency also increases the coherency of the oscil- lations as is evident from the preceding discussion. Thus, we try to keep the quench frequency as high as possible while still allowing enough noise for the proper operation of the oscillator. Raising the voltage of the external quench in- troduces more noise (correSponding to more incoherency) thus allowing us to raise the quench frequency, but it also in¥f fin NU - C1Y1 78 introduces amplitude modulation. At low oscillator fre- quencies it was sometimes necessary to lower the quench frequency so much that a sharply decreased sensitivity was noted. In summary then, the voltage and frequency of the external quench are adjusted in conjunction to obtain the highest quench frequency (although not too high) consistent with the proper noise and the least amount of amplitude modulation. In the second method, called self-quenching, the oscillation is dampened by the following action. During oscillation current flows in the oscillator tube, this results in a small gridhleak current which flows through the variable resistor R1 to ground and back to the cathode, thus complet- ing the circuit. During its passage some of the grid-leak current is diverted to charge capacitor C; which in turn causes a negative potential on the grid. As more current flows the capacitor becomes more highly charged and the grid becomes more negative until current flow through the tube is cut off. The capacitor then discharges to ground through R1, decreasing the negative potential on the grid until current may again flow in the tube, then the whole process is re- peated. The quench frequency is mostly controlled by the product of R1 and C1. In the circuit of Figure 7, R1 = 2 Meg- .ohm and C1 = 50 pf, permitting quench frequencies in the range 20-40 kHz. This control is logical since the larger is R1, the more slowly is C1 discharged to ground and hence the lower the quench frequency. Again R1 must be continuously adjusted 79 as the frequency of the oscillator is changed in order to maintain the prOper noise level. The advantage of self- quench is that it is slightly more sensitive than external quench. However, external quench has the advantage that it does not need to be adjusted so frequently as the oscillator frequency is changed and changing frequency does not affect the oscillator frequency; these are both significant ad- vantages. The oscillator can only detect rf power absorp- tion (which would indicate a nuclear absorption frequency) during the build-up of oscillation amplitude following a period in which the oscillation has been quenched. The method of detecting a resonance is to detect a slight lowering of the rf voltage at the plate of the oscillator tube. This lowering comes about in the following manner. For a self- quenched circuit, an absorption of power lowers the base volt- age upon which a new oscillation cycle must start, thus it takes a longer time for the grid to reach the cut-off voltage, corresponding to a decrease in quench frequency. Since a decrease in quench frequency means fewer bursts of rf voltage at the plate in a given time, the average rf voltage at the plate decreases; this decrease is the basis for detection of the absorption. For an externally quenched frequency circuit the quench frequency is fixed but the average amplitude of the rf bursts is lowered by an absorption, which the plate sees as a drop in average rf voltage. The high-range oscil- lator may be operated as either a self-quenched or externally- quenched oscillator. In order to operate it with external 80 quench, R1 is switched from ground to a BNC connector at which the output from the quench oscillator is injected and the value of 31 is then decreased until self-quenching stOps. Capacitors C2 and C3 are adjusted by experiment to obtain the most sensitive Operation of the spectrometer but as a general rule if one is more open the other should be more closed. For this reason they are connected in tandem in the low-range oscillator such that as one opens the other closes. The frequency of the oscillator within a given range is varied by tuning the tank capacitor C4. The range of the oscillator may be changed by changing the tank coil L1. Typical coils allow a range of about 10 MHz. The sample to be studied is inserted directly into the tank coil and since most searches and measurements are made at liquid nitrogen temperatures some extension of this coil is needed outside the oscillator. At first this was done by means of a standard shielded cable RG-SB/U but this caused problems because it introduced increased capacitance into the tank circuit. Although the problem was partially solved by using Special low-capacitance cable RG-62/U this was not completely satis- factory because shielded cable was not rigid enough, the oscillator being very sensitive to vibration, and it was very inconvenient to change coils. All these problems were over— come in the following manner: A-é inch O.D. brass tube 6 inches long was rigidly mounted to the spectrometer chassis and fitted at the bottom with a male BNC connector. A-fi inch 81 solid brass rod was then run down the middle of the tube, being careful to keep the rod and the tube electrically iso- lated since the tube was grounded. The end of the rod was reduced and sharpened and used as the pin in the BNC con- nector, the other end of the rod being connected to the side of C4 which was above ground. The various coils were then mounted on female BNC connectors thus making coil changing quite simple and easy. In the process of building high frequency oscillators certain good practices should be followed. It is well-known that length of leads is critical but only in certain parts of the circuit. The most critical lead lengths are the lengths of wire between resistors, capacitors, etc. and the oscillator tube. Thus, for example, a resistor which is to be connected to the tube should have its connecting wire cut off as close to the resistor body as possible, allowing only a long enough lead to insure a good solid joint; the lead on the other side of the resistor body is not important. It is also good practice to get a chassis much larger than needed and to place the oscillator tube socket in the center allow- ing plenty of hand room so that the elements directly attached to the tube may be squeezed in quite closely. Lead lengths in the tank circuit do not seem to be critical but they should be of heavy gauge bare wire, preferably the tin coated variety. They should not be placed close to the walls of the chassis, if possible, as the wall and the wire tend to form a capacitor. .1 n n; 5 and t1 safe I ann‘ ‘ JauoL n: ,__. '—J () 82 All grounds in the oscillator should be to one firm ground and the tube socket center should a130 be grounded to this same ground. This helps to avoid ground loops and parasitic oscillations. Finally, particular care should be taken that all components are mounted solidly and rigidly. 5) Modulation and the Lock—in Amplifier In NMR work a resonance absorption may be detected di- rectly by a drop in rf power at the receiver but in NQR work this drop in power is too small to be directly detected. Accordingly, a method has been adapted from radio technology called modulation. As applied to the observation of nuclear resonance absorptions the concept of modulation is quite simple. In NQR there are two types of commonly used modu- lation, frequency modulation and magnetic, or Zeeman, modu- lation. When the frequency of the oscillator is passing through resonance both types of modulation cause the rf power absorption to appear at the frequency of the modulation, thus causing a signal to appear in the oscillator output at the modulation frequency, although this signal is not necessarily in phase with the audio generator producing the modulation signal. When no absorption is taking place the modulation has no effect on the oscillator output. Thus, the appearance of a component in the oscillator output at the modulation frequency means that the frequency of the oscillator coincides with an NQR absorption frequency in the sample under study. This sig- nal is much easier to detect than a drop in rf power. “d. . “1 “hr,- bu. \ a, .4» NIH . SE 85 In frequency modulation the frequency of the oscillator is constantly varied over a small frequency range which is determined by the amplitude of the modulation. The modulation amplitude should be determined by the width of the resonances. Wide resonances need large frequency excursions when sweeping through them; hence, large modulation amplitudes are needed; narrower lines require a smaller amplitude. Since excessive modulation amplitude tends to distort and broaden absorption lines the minimum amount of modulation should always be used. This is particularly true when using the lock—in amplifier recording technique. The frequency of modulation is another consideration. The most important consideration is that the modulation frequency must be small compared to the absorption line width. Since line widths have been observed from about 2-50 kHz, modulation frequencies generally should not exceed 300-400 Hz. It is also not advisable to use 60 cycles,or any harmonic or sub-harmonic,when using the recorder technique due to the danger of picking up line noise. Aside from this consideration many workers seem to prefer higher frequencies, typically 280 Hz, in order to avoid flicker noise but this is not a very convincing reason since flicker noise is only im- portant for frequencies below about iOHz. In this work several standard signals were recorded at widely varying modulation frequencies. The results showed a surprising ‘Variation in signal-to-noise ratio with modulation frequency. (HPtimum modulation frequencies usually fell around 59 Hz so this he 01 .a:1: pres 84 this modulation frequency was adopted. No explanation can be offered for the variation in signal amplitude with modu— lation frequency. Although there are many schemes for frequency modulation of superregenerative oscillators the one adopted in the present work is believed to be the best. It consists of placing a 1N950 diode D1, which acts as a capacitor, in parallel with the tank capacitor. The diode then has the property that its capacitance varies with the voltage applied to it. Thus, if a periodic voltage is applied to D; the fre- quency of the oscillator is varied periodically. For example, the 1N950 varies in capacitance from 0-88 pf with a variation of 0-150 volts. The slope of a graph of the capacitance of the diode versus applied voltage changes in different voltage regions so the diode is biased with a d.c. voltage to bring the voltage into the region with the desired slope. Figure 9 shows the auxiliary unit used for frequency modulation in this work. It can accept either 60 Hz line voltage, which is stepped down to 6 volts rms with a filament transformer, or 1-10 rms volts of audio voltage supplied by an audio oscillator, in this case a Hewlett-Packard Function Generator Model 202A. In either case the audio frequency is supplied to an inter- stage transformer with a 2:1 ratio which steps up the voltage and also acts as an impedence matching device for the audio oscillator. The auxiliary unit also supplies a d.c. bias using a standard Eveready 45-volt battery. 85 .Hmuwfiouuummm moz may now was: GOHumHspoz .m musmflm nuuflzm use GOflumHspoz .emmo Mo~¢ .H MW 30> ma ITHUZPO lfllllllO zoom >mag .nYu ; XH Koaumauommcmuu mmmumumucH mud udQCH umEHOMmcmuu ucmsmHHm $33" uzJ 16 Thus I pe*io ' i sine 86 In magnetic modulation the absorption is made to appear and disappear periodically by applying a periodic magnetic field to the sample. As previously explained, the application of a magnetic field of sufficient size to a polycrystalline sample will cause the resonance to broaden out and disappear. Thus, when a square wave or half—wave rectified sine-wave voltage is applied to a Helmholtz coil or a solenoid in which the sample is placed, the resonance disappears during the on- period and appears during the off-period. If an unrectified sine wave is applied, the situation is more complex but essentially the signal appears and disappears twice during a modulation cycle, since both positive and negative voltage producetflmzsame magnitude magnetic field (although Oppositely directed), and the broadening of NQR absorption lines depends only on the magnitude of the applied field. Accordingly, the induced frequency in the oscillator output appears at twice the modulation frequency. Magnetic modulation in this work was applied by means of a solenoid wound in four layers around a cylindrical Dewar vessel. The sample is placed inside the Dewar vessel in the sample coil and both are immersed in liquid nitrogen. The wire was of small enough gauge to permit winding forty turns per inch over the length of three inches and the diameter of the Dewar was three inches. The sinusoidal current was supplied from the Hewlett-Packard Function Generator which was fed into a Fisher lOO-watt power amplifier. This amplifier .J in t O , E S F ¢ Pk Y. ; . 3a .11. Nd n . .. . a HHv ‘1 pl V s PU ‘5 V w'L V r s , 1 l sen ‘L “V 87 supplies currents in the range 0.1 to several amperes rms; three amperes roughly corresponds to a field of 400 gauss rms at the center of the solenoid. The signal-to-noise ratio for many NQR signals is so low that it may not be easily observed on the oscilloscope. In this case some device must be found which improves the signal-to-noise ratio. Abragam (78) has shown that the narrower the band width around the modulation frequency which we observe, the better the signal-to-noise ratio. Thus, if our modulation frequency is 59 Hz and we observe all signals in the output of our oscillator in the frequency range 59.i 0.1 Hz our signal-to-noise ratio will improve compared to signals observed in the range 59 :,1 Hz. The narrower this bandwidth the more improved will be our signal-to-noise ratio but there is a practical lower limit to the bandwidth. We 'wish,'then, to use a narrow—band amplifier to amplify only signals at the modulation frequency in the output of the oscil- lator. The oscillator output will also contain some noise at the modulation frequency at which the narrow-band amplifier is centered, but the phase of this noise will not be fixed but random. The signal induced by the modulation will be of fixed phase although not necessarily the same phase as the modula- tion. If we pass the output of the narrow-band amplifier into a phase-sensitive detector, then the output of the detector A is proportional to Aincose, where 9 is the phase angle out between the input signal from the narrow-band amplifier and CCI‘. SE?) is no *1 I). 88 the modulation signal; the noise will then be greatly reduced. The input to the phase-sensitive detector is put into phase with the modulation by passing it through a phase- shifter circuit, the amount of phase shift being set by maximizing a strong known signal. The output of the phase— sensitive detector is then rectified and fed to a recorder. A signal may be detected by noting marked changes in the level of the d.c. output to the recorder. An amplifier which consists of a narrow-band amplifier followed by a phase- sensitive detector is called a lock-in amplifier. For further discussion of the lock-in amplifier see references 78-81. Since the modulation amplitude is set at only a fraction of the line-width when using a lock—in amplifier the output of the amplifier is proportional to the slope of the absorption line and a first-derivative curve is obtained instead of an absorption curve. If desired, an output proportional to the change in slope of the absorption line may be obtained by detecting at twice the modulation frequency; a second deriva- tive of the absorption line is then obtained. This is desir- able if amplitude modulation is troublesome. Also, if an unrectified sine-wave magnetic modulation is used it is necessary to detect at twice the modulation frequency. A home- made lock-in amplifier constructed according to a circuit diagram by Bolte (81) was first used in this work but it was found that there were several mistakes in the wiring diagram and even when these were corrected the amplifier never worked 89 reliably. A Princton Applied Research Associates Lock-in amplifier Model JB-4 is now used and has worked quite satis— factorily. No NQR spectrometer would be complete without a lock-in amplifier since approximately half of the signals reported in this work could not be observed on an oscilloscope. Figure 10 shows a block diagram of the spectrometer. All the important parts have been discussed. A typical re- corded NQR spectrum is shown in Figure 11. 4) Frequency Measurement If the NQR absorption line whose frequency we wish to measure is a single sharp line strong enough to be easily observable on an oscilloscope, frequency measurement is rela- tively straightforward. The method is based on the fact that when the quench frequency is changed by an amount Av the Q first upper sideband moves up in frequency by an amount AvQ . the second upper side band increases in frequency by ZAVQ . etC-I the lower sidebands similarly move to lower frequency. The center frequency, in theory at least, does not move but this is strictly true only for externally quenched oscillators; in self-quenched circuits,changing R1 slightly does alter the central frequency and this movement of the central frequency can greatly confuse the measurement. However, once the high frequency oscillator was modified so that it could be ex- ternally quenched this uncertainty was removed. From the above discussion it is clear that the sidebands far removed from the center frequency move quite radically upon small 90 .HmumEouuoQO moz mnu mo EMHmMHU xoon .OH musmflm umouoomm Houoz Hm3mn Unsoum pmmmmu? xuoHo pfiocmHom GoaumHsvoE $\ Hmflmflamfid GWIMUQA Houomumn amoumoHHHomO has: coaumHsooz Houmumcmo _ Hmumfifi¢ umwmaame< Hmnmflm coauucsm_ l! 91. .mcHH 50mm Eoum mocmnmoflm nocmsv mnu mum CBOQm Oman “mmcaa coaumnomflm um: mam.om men cam omm.om men magsonm mHUOm.mHUQm mo Eduuommm Hmfluumm one .dfi musmflm n)- F" fin. at: u VOILE *asi: me is t‘ {L is ‘ u h Ff- ~54. the the 92 changes in the quench frequency. Without changing the quench voltage, which usually greatly alters the line shape, changes of about 5 kHz in the quench frequency may be made. Such a small change does not alter the positions of the closer side- bands on the oscilloscope screen so there is usually still some ambiguity'.regarding the center line. A further problem is that when an external signal is coupled to the oscillator it is received as a series of sidebands and a center band. The problem then becomes one of superimposing the central band of the external signal source upon the central line of the resonance spectrum. A useful technique is to pick out the three or four strongest lines from the external source and the sample absorption. Each sample line is then tuned onto the oscilloscope in turn and tested with each of the external source lines. Each external line is imperfectly superimposed on the absorption signal, the quench frequency is then varied and the two lines observed to see if they move relative to one another. This technique is usually successful with strong lines. However, even if the center line of the oscillator and that of the external source are correctly identified, it is very difficult to superimpose them exactly since there is a marked difference in line shape between absorption lines and those from the signal generator. This may lead to an error which has been estimated at.1 kHz from trial.nmasurements on NaClOs. If the NQR line is not a singlet the absorption spectrum becomes quite complex, due to over— lapp-ing of the sideband patterns. In this work the POC13 ”‘1” :vd‘i:e flownl H Vol.9 g. L t}., LUCA) O ments V ‘Mv “vi 5 38:. 95 lines in both TiCl4‘2POC13 and (TiCl4-POC13)2 overlapped. In the case of (TiCl4-POC13)2 it was possible to resolve the spectrum into three lines after a considerable time spent studying the spectrum but it has not yet been possible to re- solve the spectrum of TiCl4°2POC13. In the case of the more complex Spectra the best procedure is to pick out the strong- est lines and measure their frequency by superimposing what is judged to be the center line of an external oscillator on them. The quench frequency is then changed and the measure- ments repeated. From a study of the results, keeping in mind how sidebands behave upon changing the quench frequencies, an attempt is then made to distinguish the number and frequencies of the center lines. Needless to say, this procedure is not infallible. In the case of (TiCl4'P0Cla)2 additional COD? fidence in the results is gained from the agreement between the experimental results and the line multiplicity as predicted from the X-ray structure of this compound. In all cases ten frequency measurements were made for each line and an average used for the line frequency. From the precision of individual measurements of the same line, and from previous trial measurements on NaClOs and p-dichlorobenzene, it is believed that all frequency measurements made by the above techniques are accurate to.i 3 kHz. When absorption lines are too weak to be observed on the oscilloscope screen a different technique must be used. The follxjwing method was found to be the best of several methods "A. VJ 1+ CI) 94 tried. The line was first recorded repeatedly while chang- ing oscillator settings, modulation amplitude and lock-in amplifier settings, until the best recorded spectrum was obtained. This spectrum was then studied in an attempt to determine if it was a singlet or not. The most likely center lines were then picked out and the spectrum rerun at the slow speed of l/SOO rpm and stopped on each of the likely lines in turn. An effort was made to stop at the exact zero point of the first derivative, but this was not always pos- sible, because of a lag between the recorder and the lock-in amplifier. Furthermore, it was not possible to tell if the recorder was stopped at the correct spot. The correct center line from the external oscillator was then centered on the oscillo— sc0pe and this line was then centered on the frequency at which the oscillator was stopped by observing the output of the narrow band amplifier on another oscilloscope. The pro- cedure was then repeated at another quench frequency and by comparison of the shifts induced by the change in quench frequency the center line was decided upon. By comparison 'with measurements on known compounds.i 10 kHz is believed to be the accuracy of lines measured by this method. The precision of measurement is, however, somewhat better. Unfortunately. .i 5 kHz was the maximum change in quench frequency which could ‘be obtained. Since the uncertainty in measuring the quench frequency was :t 10 kHz this allowed some ambiguity in the choice of the center line. t« C 5. 95 It is believed that any line whose frequency was measured on the oscilloscope is accurate to.i 3 kHz while those measured on the chart are accurate to.i 10 kHz. However, especially in the latter case, there is a chance that a sideband was mistakenly chosen as the center line. This possibility is inherent in all frequency measurements involving superregenerative oscillators but is often ignored by authors when assessing their possible errors. 5) Spectrometer Operation and Problems in Detecting Resonances Searching for an NQR absorption is often frustrating and disappointing. Relatively minor things may cause the line to be missed. For example, some lines are quite sensitive to modulation while others are not. For no apparent reason some lines are quite intense while others with the same number of resonating nuclei per unit volume are quite weak. In some cases the latter phenomenon has been attributed to subtle differences in crystal structure although no one cares to go into this matter too deeply. For example, it is found that certain liquids which are rapidly cooled to liquid nitrogen temperature give no resonance signals but if they are cooled very slowly they do have resonance absorptions. This behavior is attributed to the fact that rapid cooling probably developed strains in the crystal lattice and these strains somehow erased the signal. Order-disorder phenomena also have an ef- :fim:t as shown by the following phenomenon observed by Dean (85): no signal was found for chlorine in p-chlorobromobenzene 2+ AMI" .- .R' ...C SET 2'31 Us gufi. A" V- th; 3?. 5.. 96 but when a small percentage of p-dibromobenzene was mixed with the p-chlorobromobenzene a chlorine signal appeared. The ab- sence of absorption was explained on the basis of a certain randomness in the crystal structure of p-chlorobromobenzene due to the fact that the halogen sites have equal probability of being a bromine or a chlorine atom. When the p-dibromo- benzene was added the crystal structure became more ordered since there was now a higher probability that a halogen site would contain a bromine atom. Khotsyanova (86) has explained some of his results in a similar manner. He has studied the spectrum of C6C15F which consists of 3 lines of 770K, while at 1950K no lines are observed. He ascribes this behavior to a crystalline phase transition to a totally disordered phase. It is also found that impurities have an effect on NQR lines. Some types of impurities have a more marked effect than others, but all impurities tend to broaden an NQR line and lower its intensity. Another factor which contributes to the difficulty of finding NQR lines is the wide range of frequencies at which they may occur. This difficulty is eSpecially troublesome in elements which have a large quadrupole moment. Compounds containing these nuclei have potentially a very large absorp- tion frequency, yet if they are involved in a highly ionic bond.the absorption frequency can be quite low. An example of this is 1271 (Q = -O.75) whose d: 5/2 ->:t 3/2 transition freque: Fartun predic but ca SUCK a Eltroc liquid 97 frequency ranges from 29.5 MHz in CdIg to 902 MHz in ICl. Fortunately the expected frequency range for 1271 may be predicted from studies on similar 85Cl containing compounds but calculated predictions have not been succeSSful for nuclei such as 55Mn (Q = 0.6) and 57Co (Q is expected to be of the same order of magnitude as Q for 55Mn) and it is difficult indeed to predict where NQR absorption will take place in com— pounds containing these elements. Finally, it should be mentioned that NQR absorptions are missed in many compounds for no apparent reason whatsoever. This happens more often than is desirable and is one of the principal drawbacks to the widespread use of nuclear quadru- pole resonance. The frequency sweeps in search of unknown resonances were made so as to minimize as many of the above mentioned draw- backs as possible. First, the sample was packed as tightly as possible into a glass vial to maximize the filling factor, or,if the sample could be melted without decomposition, it was melted into the sample tube. It was then annealed in an oven overnight at a temperature just below its melting point to minimize strains. If the sample was a liquid, or a solid near its melting point at room temperature, it was precooled overnight in a refrigerator then slowly cooled to 770K by gradually lowering it into a Dewar vessel containing liquid nitxnogen which had been pretreated by adding a small amount of Lhmrid nitrogen and allowing it to stand long enough to 98 establish a temperature gradient in the rest of the Dewar. Various methods were tried for adequately sealing sample tubes which contained substances highly reactive with air. At first rubber stoppers were inserted and sealed with plastic tape. This was not successful as the corrosive samples were found to attack both the rubber and the tape. Then Nylon stoppers were machined and inserted into the glass tubes containing the sample; these were sealed in with a tape especially resistant to chemicals and the top of the tube was coated with paraffin. At first this method was success- ful, even though the samples attacked the tape,but repeated immersions of the sample into liquid nitrogen soon flaked off all the paraffin. The final measurements were made on samples sealed into glass tubes. This seems to be the only satisfactory way to handle corrosive samples. In order to avoid temperature gradients, samples were kept in liquid nitrogen for half an hour prior to beginning the search. This was much longer than necessary but was a convenient time since it took this time to warm up the spectrometer and make some preliminary adjustments. The range of a particular coil was governed by the in- ductance of the coil, the larger the inductance the lower the frequency range of the coil. Thus, the larger the number of turns in a coil the lower its frequency range. In order to obtain a good Q for the tank circuit these should all be of the same size and the coil should be wound neatly with 99 closely spaced turns. All coils used in this work were 1.5 cm in diameter. However, if too many turns were wound on a coil, the coil became quite unwieldly. Conversely, in coils intended for a high frequency the number of turns became too few causing a serious drop in rf power in the coil. Both of these problems were solved when it was noted that a coil wound with fine gauge wire always had a larger inductance than a coil with the same number of turns of heavier gauge wire. Coils with a few turns were wound with heavy gauge wire while those intended for the low range of the oscillator were wound with small diameter wire; those for intermediate ranges had their wire gauge chosen to give a convenient number of turns. Below is given a table of coil size and gauge together with the frequency range of the coil. Table 8. Physical Dimensions of the Coils Used with the High Range Oscillator Number of Frequency Range Turns Wire Gauge in MHz 9 18 15-22 12 16 21-27 7 16 24-52 5 14 28-56 4 14 52-42 3 14 36-48 si; 582 [L‘ "1 100 The settings for the lock-in amplifier are maximized prior to the beginning of each run by use of a strong known signal. This signal should be as close to the expected sample frequency as possible. When all is in readiness, a low frequency modulation amplitude is chosen and the frequency range provided by the coil being used is swept. This is done by means of a Holtzer- Cabot motor of 120 inch-ounce torque and 1 rpm speed which is fed to an INSCO speed reducer that may be set to provide reductions of 1:1, 2:1, 5:1, 20:1, 50:1, 100:1, 200:1, 500:1, and 1000:1. The speeds of 1/500 and 1/200 were most often used. If the recorder trace showed no signals, the frequency range was swept again with a larger modulation amplitude. This was repeated with severalsdifferent modulation amplitudes. In some cases both frequency and magnetic modulation were used although frequency modulation was used most often. The noise level of the spectrometer was kept at a level which was de- termined through trial and error on known signals. All frequency measurements were made with a BC-221 Frequency Meter whose frequency was then counted with a Hewlett-Packard Model 524C Electronic Counter. The direct reading on the electronic counter was compared to the cor- rected frequency read from the charts on the BC-221 and in all cases agreement was excellent. sL ~.E 101 6) Temperature Dependence of the 27.512 MHz Resonance in SbCls-POClg It was decided to measure the temperature dependence of the strong 35Cl line of SbC15 in SbCls'POClg to see if a crystalline phase transition took place. For this purpose three slush baths were prepared to cover the temperature range from liquid nitrogen (770K) to room temperature (2970K). These were carbon disulfide, ethyl acetate and carbon tetrachloride. An ice-water mixture was tried but could not be used because the mixture damped out oscillations. Each bath was made by adding about 200 cm3 of reagent to a 500 cm3 Dewar vessel and then adding liquid nitrogen in small amounts. The mixture must be vigorously stirred otherwise the two liquids quickly separate. The mixture finally solidifies and is allowed to melt until a thick slush is ob— tained. This mixture easily holds its temperature.i 10K for about 50 minutes, after which it must be resolidified. The samples were allowed to equilibrate with the slush baths to eliminate temperature gradients and the resonance pattern centered on the oscilloscope screen. The frequency of the line was then measured by the method given previously. B. Chemical Syntheses The methodsibr the preparation of all samples and standard compounds are given below. 1) Trans—dichlorobisethylenediamine Cobalt(III) Chloride-HCl-xfigo frec mate 102 This compound was desired as a standard for the low frequency oscillator since it has 57Co resonances at approxi- mately 5, 10 and 15 MHz and a weak asCl resonance at about 16 MHz. It was prepared by the method of Bailar (87). At first it was not known that the HCl occluded in the lattice was essential to observation of the 57Co resonances so that no precautions were taken to retain the HCl which is very volatile and evaporates if the complex is air dried. When it was realized that HCl was essential the complex was dried in a desiccator over concentrated sulfuric acid with an open beaker of concentrated hydrochloric acid also inside the desiccator. The procedure is as follows: Six hundred grams of a 10% (by weight) ethylenediamine solution was added while stirring to a 2-liter flask containing 160 gms of CoC12°6H20 in 500 ml of water. A vigorous stream of air from the air jets in the hood was filtered through glass wool and blown into the solution overnight. Three hundred milliters of concentrated EKIL was added, the whole mixture poured into a large evaporating dish and then heated on a steam bath until a crust was formed over the surface. The bright green crystals of the complex were filtered off and quickly washed with alcohol then ether. The crystals at this point had partially turned to a dull green indicating some loss of HCl. They were then transferred to the desiccator and dried in an atmosphere of HCl gas. During the drying process they re- gained their bright green lustre. S) n; "\ '(J C) (\7 105 2) The Cu(I) Complexes of Some Thiosemicarbazones These 1:1 complexes were synthesized so that an attempt to find 63Cu(I) resonances in diamagnetic compounds could be made. Thiosemicarbazones of the following ketones and aldehydes were made and complexed with CuCl:acetone, cyclo— hexanone, benzaldehyde, o-chlorobenzaldehyde, o-methoxy- benzaldehyde and m-nitrobenzaldehyde. Each was made by react- ing the corresponding ketone or aldehyde with thiosemi- carbazide in a reaction quite similar to that used in forming hydrazones and oximes. The following procedure was adopted from the method of Sah and Daniels (89): 0.05 moles of thio— semicarbazide, 100 ml of water and 10 ml of glacial acetic acid were warmed on a steam bath until the thiosemicarbazide dissolved and the solution then added immediately to an alcoholic solution of the ketone or aldehyde. Usually a pre- cipitation of the product occurred immediately but sometimes it was necessary to cool in an ice bath. The copper com- plexes were made as follows (Gingras et al. (88)): 0.05 moles of the thiosemicarbazone were dissolved in methanol (about 200 ml) and heated to reflux in a three-necked flask equipped with a stirring motor. To this solution was added dropwise, while stirring, 0.05 moles of CuCl dissolved in about 100 ml. of ammonia solution (0.9 Specific gravity). The mixture was then stirred and refluxed for an additional thirty minutes, cooled to room temperature and the complex filtered off in the form of a dark Sludge ranging in color from light gray to 104 a dark olive green. The complexes were purified according to individual methods as recommended by Gingras. In the case of the o-methoxybenzaldehyde complex, which was not made by Gingras, the procedure for the p-methoxybenzaldehyde complex was followed. It Should be mentioned that these complexes do not seem to be soluble in any of the common solvents hence recrystallization, the most reliable purification method for solids, could not be used. The purification procedures consisted of washing with various solvents and solutions. It is not known how pure these compounds are. The complexes seem to be quite stable and have been stored in plastic topped bottles for over a year without noticeable decomposition. 5) Mercuric Chloride Complexes Mercuric chloride has a strong NQR absorption at about 22 MHz; hence, several complexes were made to see if the resonance line shifts upon complex formation. The preparation of HgC12°(CH3)2SO followed one of the methods of Selbin et al. (90). Approximately 20 ml of dimethylsulfoxide was heated on a steam bath and saturated with mercuric chloride. Upon cooling transparent crystals separated. An attempt was made to re- crystallize these crystals from acetone; however, an oil formed. Addition of ethyl ether followed by scratching the Side of the beaker with a glass stirring rod, however, pro- duced a white transparent precipitate of good crystalline form. The melting point as given by Selbin et al. was :U .‘4 \I,L \G. A! t, h adv 5L 105 125-60C and the first time the complex was prepared it had a melting point of 125-60C. The second time it was prepared a waxy rather than a crystalline material was obtained which, when recrystallized from ethyl ether, yielded a compound with a melting point of 77-80C. Although this compound was put in a vacuum desiccator connected to a vacuum pump for several weeks no complex with a melting point 125-60C was obtained. It is suggested that this compound may be HgC12-2(CH3)2SO but no attempt was made to determine its formula because neither complex yielded an NQR resonance. The four complexes (Pyridine)2°HgClg,(2-Picoline)2»HgC12, (S-Picoline)2-HgClg and (4-Picoline)2-HgC12 were made accord- ing to the following procedure: To a saturated ether solution of HgC12 the base was added and the white flocculent precipi— tate which appeared immediately was removed by filtration and washed 5-6 times with cold ether. It was then recrystallized from methanol, placed in a vacuum desiccator and the desiccator connected to an oil pump for several days. Preparation of the dimer of the 1:1 complex of triphenyl- phOSphine mercuric chloride (91). When a solution of tri— phenylphosphine in absolute alcohol (5.2 gms per 250 ml) was added to a solution of mercuric chloride in hot absolute alcohol (5.4 gms per 250 ml) the complex immediately precipi- tated in the form of glistening white Scales. These were collected and dried in a vacuum desiccator. 106 4) The Complexes of ICl with Pyridine and its Derivatives The complexes of pyridine, S-cyanopyridine, 2-bromo- pyridine and quinoline with iodine monochloride were prepared with a method adapted from Meyer (92).which depends on the fact that ICl and all the organic bases are quite soluble in CCl4 but most of the complexes are not. The method is as follows: The base and ICl were each dissolved in CC14 in ' approximate one-to-one molar ratios, the two solutions mixed together and the complex allowed to precipitate. The colors J.“u‘v:-n ' ll " " of the precipitates ranging from mustard yellow quinoline-1C1 to bright yellow 2-bromopyridine-IC1. This precipitate was, however, mixed with some brownish red particles, also the solution remained brownish red. Evidently the complex forma- tion does not go to completion, the reddish brown color being attributed to ICl. The original solution was decanted, fresh CCl4 added, and the whole mixture gently warmed on a steam bath. After a time this solution was also decanted, and the process repeated until no more red particles could be ob- served mixed with the complex and the CCl4 remained trans- parent in color. The complex was then air-dried. 5) Binary Complexes of POC13 Since the complexes are quite difficult to prepare, and to various extents react with moisture, no attempt will be made to give a general preparation, as has been done for the compounds previously discussed, but each preparation will be described individually. The compounds all have in common the 107 fact that they are hydrolyzed quite easily by the moisture in the air and every precaution must be taken to ensure as little contact as possible with the atmosphere. All Operations involving extensive handling of these compounds were carried out in a dry box under nitrogen atmOSphere. All reactions were carried out under an atmosphere of purified nitrogen which had been passed through a drying column. After the re- lrfih action was completed the reaction flask was quickly sealed and opened only in the dry box. The physical appearances of these compounds are quite diverse, some are low-melting waxy [ solids, while others are powders. It was found that the waxy solids were more stable and could be handled in the air for longer periods of time without decomposition. The complexes SbCls-POClg, TiCl4-2POC13, SnCl4-2P0C13 and (TiCl4-P0C13)2 were all made by the same general method. Two 250 ml Erlenmeyer flasks were first flushed out with nitrogen, then about 25 ml of the acid was quickly added to the first flask and the flask was weighed again. In the case of the TiCl4 complex, POC13 was then carefully weighed into the other flask on an OHAUS CENTIGRAM balance, such that the molar ratio of P0C13 to TiCl4 was either 2:1 or 1:1. The P0C13 was then quickly added to the TiCl4 and the flask again stoppered. Immediately an exothermic reaction took place and the solution became bright yellow; upon cooling the whole mass solidified. The mixture was then melted, stirred and allowed to resolidify to ensure good mixing of the 108 components. The solid was then completely melted and allowed to solidify except for the last few milliliters which were discarded. This process was repeated twice. The complexes were then stored in a vacuum desiccator over P205. In the case of SbCls and SnCl4,only one complex is formed with P0C13 so that a little excess reagent was added to ensure complete reaction. At first excess P0C13 was added as recommended by Gutmann (93) but this did not work as well as excess acid, Since excess acid was much easier to remove when the complex was pumped on with a vacuum pump. The SbCls complex was a pale lemon yellow color, which may possibly have been due to ,_w a slight impurity of SbCls, while the SnCl4 complex was color- less. BiC13°P0C13 and SbCla-POClg were also made by this method but since only a slight warming of the solution occurred, and the mixtures were cloudy liquids after cooling, there is some doubt that the complexes actually formed. Raman data Show that frequencies are only Shifted slightly in the mixture so the complexes are weak or nonexistent. The preparation of 2FeC13-5POC13 and FeCla-P0C13 followed a modification of the procedure of Gutmann and Baaz (94). FeCla which was slightly wet was dried in the following manner. A three-necked one-liter flask was fitted with a reflux con- denser whose top was closed off with a Drierite tube, a dropping funnel and a connection which allowed dry nitrogen gas to be constantly passed through the flask. This flask was flushed out for 50 minutes with dry nitrogen and about 20 109 gm «of wet FeCla and 100 ml of thionyl chloride was added. The mixture was refluxed on a steam bath for about three hours, until the thionyl chloride had reacted with all the water. The condenser was then put into distilling position and the excess thionyl chloride distilled off. A large excess of P0C13 was then added to the dark black anhydrous FeCla through the dropping funnel The resulting solution is a I‘m“ deep brownish red and was refluxed for an hour to ensure com- plete reaction. It was then transferred to a 250 ml Erlen- myer flask and the solution partially evaporated by use of an aspirator while warming the flask in a beaker of hot water. .,- When the mixture was reduced to a rather viscous appearance it was transferred to the freezing compartment of a refrig- erator and allowed to solidify. This process may take several weeks. The solid was allowed to warm at room temperature, at which point it remained a solid but with some drops of excess P0C13 still adhering; these were removed by evaporation in a stream of dry nitrogen. The complex, which is a dark red- dish brown spongy solid,was then transferred to a drying pistol and evacuated: the pistol wasyleft connected to a vacuum pump until a constant weight Was obtained. This latter process may also take several weeks. The complex is very easily hydrolyzed and Should be handled quite carefully. Another preparation, due to Dadape and Rao (95), was tried with much less success. In this method advantage is taken of the fact that while FeC13 is not soluble in CC14 the 110 complex is quite soluble in hot CC14 and POC13 is quite soluble in CCl4,hot or cold. A large excess of anhydrous FeCl;; is placed in a one-liter flask and 600 ml of dry CC14 is added along with 50 ml of POClg. The mixture is heated for an hour on the steam bath with constant stirring and the liquid decanted from the remaining FeC13 and cooled in an ice bath at which point the complex precipitated and was fil- tered off. Perhaps some arrangement could be made to carry out these operations in a dry atmosphere and a better yield could be obtained but the only time this method was tried mo st of the complex decomposed during the filtration step. In all other preparations of this complex the first method was preferred. FeCla'POC13 was made from the 2FeC13'5P0C13 as follows: 2FeC13-5P0C13 was placed into a drying pistol, the temperature raised to about 550C by refluxing acetone, and the pistol connected to a vacuum pump. After several hours the brown 2FeC13-5P0C13 changed to greenish yellow FeCla-POCIS by loss of P0C13. The complex BCla-POClg was made by the following pro- cedure: A 250 ml Erlenmeyer flask was first flushed out with dry nitrogen, then cooled in a slush bath of dry ice and isopropanol. BC13 gas was condensed in the cooled Erlenmeyer flask and an amount of POC13 added such that the BC13 was in large excess. The very volatile excess BC13 was evaporated with an aspirator leaving behind a white powder. During the removal of the excess BC13 it was discovered that the complex 111 sublimes at room temperature under reduced pressure. The complex was stored in a vacuum desiccator over P205. The two complexes AlClg-POCla and 2AlC13°3P0C13 are prob- ably the most difficult to prepare. Groenveld and Zuur (96) have studied the temperature versus composition diagram for the system AlClsaPOCla and they report three complexes, AlCla-POCls (m-p. 1860C), A1c13-290c13 (m.p. 1640C) and AlC13;POC13 (m.p. 410C) . They report making these compounds by sealing stoichiometric quantities of the reactants in heavy-wall glass tubes and melting the mixture. They also report making A1C13°P0C13 (m.p. 1860C) by dissolving AlCla in P0C13 and re- moving the excess POC13 with a vacuum pump. Gutmann and Baaz ( 94:) , on the other hand, on the basis of conductivity measure— Iments find that the only possible complexes between AlCla and Pool3 are AlCls'POCla (m.p. 1800C) and 2AlC13'5POC13 (m.p.. > 1600C) and do not mention a low-melting complex. It is interesting to note that Gutmann and Baaz obtain 2A1C13-5POC13 by a method identical to that described by Groenveld and 2“lur (96) for the preparation of AlCls'P0C13.' These reports are not encouraging to one who wishes to make these complexes with a minimum of fuss and bother. In all the preparations the A1013 used was first purified by vacuum sublimation. In the first attempt to make these complexes AlC13 was dissolved in POCla, the mixture placed in a vacuum desiccator and Pumped on with an oil pump. A dirty white powder was obtained Whose melting point was about 500C. This was pumped on for 112 several weeks without any change. Finally the powder was transferred to a drying pistol which was heated with reflux- ing acetone. The melting point of the complex then started to rise as POC13 was removed and continued to rise until all the POClg was lost. No complexes were obtained and several variations of this procedure also produced no results. In a second attempt to prepare these complexes, several thick-wall « g lass tubes were obtained with sealed bottoms and constricted necks for easy sealing. The tubes were about five inches long with about three inches of the tube below the constric- tion. Approximately one gm of AlC13 was weighed into each tube and stoichiometric amounts of POCla added to each tube Corresponding to the AlC13:POC13 ratios of 1:1, 1:2 and 2:5. The tubes were quickly dipped into liquid nitrogen to prevent reaction or vaporization of the reagents while the tube was be ing sealed off with a gas—oxygen torch. The constrictions Were wiped clean with a cotton swab and sealed. The tubes Were then allowed to come to room temperature. With suitable Precautions in case of an explosion each tube was heated with a. Fisher burner until the contents melted together. These Were the samples which were used in the NQR experiments. 6) Ternary Complexes of POCla In addition to the binary complexes of P0C13, a number of ternary complexes were also made. [A1(P0C13) a] [SbCle]s (97) was prepared in a 5-necked 1-liter flask which was continually flushed with dry nitrogen and was equipped with a stirring 115 rn<>t:or and dropping funnel. A 10‘1 M solution of SbCls in POClg was placed in the flask and a 10‘1M solution of AlCls. Jill POC13 added dropwise until a ratio of 5:1 was reached. firllee resulting precipitate was filtered in a dry box and vvaisshed with dry CCl4. It was then transferred to a vacuum éieessiccator to remove any CC14 and POC13 remaining. A similar Eazrcocedure was followed in preparing [Al(P0C13)5][FeCl4]3 (97). ssLllostituting FeC13 for SbCls : also the AlCls was added to t:r163 solution of FeC13 until a color change from red to pale gyxreeen occurred. K[TiC15°POC13] was made by the following berc>cedure: Using the same set-up as the previous preparation, 1Pj_<214 was added dropwise to a suspension of KCl in P0C13 llrltzil a molar ratio of 1:1 was attained. The solution was c=C>lrlcentrated in gaggg_until a good crop of yellow crystals was C51)1:ained. The flask was then transferred to a dry box where titles crystals were removed by filtration and washed with dry (3C3314. They were then dried in a vacuum desiccator over P205. s1~'>C215°TiCl.;,-5POC13 was prepared by the following procedure ( 98) : SbCls and TiCl4 were dissolved in a 1:1 molar ratio in city ethylene chloride and P0C13 added in excess. The mixture ‘VEiS concentrated under vacuum, filtered in a dry box and Vmashed with dry CC14. Finally, the resulting crystals were sublimed in 33939 at a temperature of 180-2000C. All solvents used in this work were dried with Drierite and then with magnesium sulphate. The solvent was then de- canted and distilled taking only the middle cut. They were stored over Drierite. III. CALCULATION OF THE CONTRIBUTION TO THE MEASURED FIELD GRADIENT FROM CHARGES SITUATED IN THE LATTICE I&.. Introduction As mentioned in the theoretical section, contributions t:<> the quadrupole coupling constant may result from charges eezcternal to the molecule being investigated. These charges atzre situated at fixed points in the lattice and the approxi- :nmaition is often made of replacing these charged atoms by js>c>int charges. In order to avoid confusion in subsequent C3;i.scussions the following definitions are made. The molecular ffj_eld gradient tensor EmOl at a nuclear Site is due only to e lectrons within the molecule and is the gradient which would kbee measured if the molecule was completely isolated. The C21:ystal lattice field gradient acrys arises due to solid SState effects and is a property of the crystal lattice. 3511 this thesis a model has been introduced which ascribes t:his effect to point charges Situated in the lattice; thus, tihe term crystal lattice field gradient will often refer to (zontributions from this source. This calculation is not a asimple one for several reasons. As previously mentioned a <:orrection must be made by use of the Sternheimer factor for the fact that the chloride ion is highly polarizable. The uncertainty in assigning a value for 7a) (Cl-) has been 114 115 discussed. Another problem is that, for the compounds we wish to discuss, it is not certain exactly what charge to assign to each point because the compounds which are investi- gated in this work are partially covalent. Thus, it is not realistic to assign the charge of the fully ionic species, but the partial charge on the ion is very difficult to determine. Sharma and Das (99) have shown in calculations on A1203, Fe203 and C‘r203 that a rather large contribution to the electric field gradient comes about from the dipole in- duced in the highly polarizable 02" ion. These contributions have been neglected in the present case partly because, Since all the ions involved are much less polarizable, this contri- 13111:ion is much smaller than that expected from 02‘, and partly 13€e<2ause this effect would be extremely difficult to calculate in our case. The above three approximations introduce enough mlicertainty into the actual lattice sum calculations that the results of the calculation Should be used with caution in quantitative predictions. The lattice sum results are, hOwever, quite valuable as a measure of the differences in environment of crystallographically different but chemically similar chlorine atoms. In particular this is of value when trying to determine the relative acid strength of a series of Lewis acids. It is important to make sure that the chlorine atoms one is using as test probes be in roughly equivalent Crystal atmOSpheres. An attempt is made here to get an idea Of the size of the external contributions to the field 116 gradient. When these contributions are determined, it must 1363 decided whether their effects overshadow chemical effects. IKIIthher reason for evaluating these sums is to explain the (31>:served multiplicity of the NQR lines. The splittings have toeeeen attributed to chemically Similar atoms in crystal- ILcaggraphically nonequivalent lattice Sites. However, few a:t:1:empts have been made so far to explain even qualitatively t:r1ned. The calculations essentially consist of summing a iftlrlcmion of e and r"3 over various sites in the crystal lattice. This summation procedure is continued until the sum converges. IIr1 theory this convergence should be rapid because of the r'3 'teezrnn in practice, however, this is not found to be the case lbsecause the lattice sums are conditionally convergent rather 'tlléan absolutely convergent. The usual practice is to pick a sE3°here of arbitrary radius (usually 20-602) around the atom a"'-“-which the lattice sum is desired and then to sum over all a4:0ms contained within this Sphere. For crystals in which the mEilL axis must be known. Jones, Barnes and Segal (105) applied I)eeVVette's method to the calculation of the field gradient in 21 Imumber of ionic halides. They assumed that the principal EI><:i.S'was along the sixfold axis. Unfortunately this is true only if the atom whose field gradient is being calculated lies (DI). the sixfold axis which is not true for several of the mole- czuilLes studied by them, introducing a considerable error in 1Zl'leese cases. In order to find the principal-axis direction 3Lt: is necessary to calculate all nine components of the field €31TEidient tensor and then diagonalize the tensor; qzz will be 'trIEit component of the diagonalized tensor which is largest :111 absolute magnitude. DeWette and Schacher have extended DEEWrette's original method so that all nine components of the field gradient tensor may be calculated for any crystal sym- Infietryu This work is the first attempt to use this new method ‘fCDr the calculation of crystal field gradients. Dickmann (IL04) has computerized the method of DeWette and Schacher for tile purpose of calculating the electric field in a crystal due ‘to permanent dipoles in the lattice. This program LATSUM has been obtained from Dr. Schacher and suitably modified for 118 the present purpose. This modification consisted Of adding several subroutines, which first diagonalize the calculated tensor by rotating the axis system to the principal-axis system in order to obtain q and n. The tensor is then ro- tated to the principal-axis system of the molecular field gradient in order to evaluate the contribution of the crystal lattice to the measured field gradient. The main program was also modified so that the electric field gradient rather than the electric field is calculated and also so the program may be cycled for the several hundred lattice sums needed, rather than separately for each one. B - Theory For the sake of completeness, a brief discussion Of the tI‘Leory involved in the calculation Of the electric field gradient at a nucleus due to external charges Situated in a crystal lattice will be given. In order to calculate the full tensor Q two types Of sums I“List be evaluated . 5v.2~-r.2 AXial sums vi =5; Ell—#314 and 3 Off“ '1 =26. .v, r.5 (65 ax1a sums va j JpJ J/ J ) Where the va are the elements Of the tensor 5, the index j ideally runs over all the atoms in an infinite crystal, and ej is the charge at the j th atom. Both Of these sums were 119 derived under the point-charge assumption. Previous workers, taking their cue from Bersohn (105), have aimed at the direct evaluation Of these sums for all the lattice sites contained in a Sphere Of radius ranging from 20-1003 which is about the largest Sphere for which this direct summation procedure is practical. However, in some cases these limits do not include enough atoms to ensure convergence. This problem can be critical as the value of the sum is usually quite small compared to individual terms since these terms are both positive and negative and the final sum is a small dif— ference between two large terms. Although the terms fall Off quite rapidly as distance from the central nucleus in- creases, terms quite far away from the nucleus can make Sig- nificant contributions to the lattice sum. Thus, workers using this method should prove convergence of their sums but this is not easy to do and has been neglected in most cases. In our particular case a sphere 1003 in diameter would con- tain about 400,000 atoms. Since this is too many for the CDC-5600 computer to dO in a reasonable time we looked for a method which ensures faster convergence Of the lattice sums. DeWette used another approach, first evaluating the sum in each plane and then adding these sums for the complete set of planes. Each sum may then be made to converge absolutely in each plane which may be seen by considering the following Simplified version Of our lattice sums method: CD S = f(n), (66) n=1 120 where f(x) goes slowly to zero as x -%~OO and may be infinite at x = 0. This is exactly the behavior of the general terms in our sums (65) because Of the r"3 term. In order to ensure good convergence for (66) we introduce an auxiliary function F(x) which is finite at x = 0 and goes to zero rapidly as x -$>OO; now (66) may be rewritten as oo o: S = Z f(n) F(n) + Z f(n)[1-F(n)] . (67) n=1 n=1 The first sum of Equation 67 is absolutely convergent but the second is not. However, if f(x)[1-F(x)] is a smoothly vary- ing function of x then its Fourier transform is a rapidly con- verging function in Fourier Space. Utilizing the property that a sum of a function over a lattice in real space is equal to the sum of its Fourier transform over the reciprocal lattice in Fourier space, we can evaluate the second sum. A third condition on F(x) is that it must be such that f(x)[1-F(x)] be a smooth function at x = 0 even if f(0) = on. For the functions f(x) with which we will be concerned, it is always possible to find an auxiliary function F(x). Thus, we see from the above discussion that the sums Obtained in this work may always be made absolutely convergent by introducing an auxiliary function and dividing the original sum into two parts, one being summed over the ordinary lattice and the other being summed over the reciprocal lattice. However, if f(x) is not infinite at x = 0 and is fairly smooth it is not necessary to find an auxiliary function. Instead the Fourier 121 transform Of f(n) is taken directly and summed over the reciprocal lattice; only one sum then needs tO be evaluated. Schacher and DeWette have given the necessary formulas for the evaluation Of these sums and they are embodied in LATSUM. It turns out that if the sums are first evaluated in a plane the summation may be replaced by an integration. The sums are therefore not evaluated in a sphere, as in the usual practice, but in a cube. It is also more convenient to con- sider each atom in the unit cell separately. A lattice sum over all atoms at the equivalent position in each adjacent cell is taken, including enough adjacent cells to ensure convergence. The coordinates Of the position are chosen so that the atom at which the field gradient is desired is at the origin Of the unit cell. Each nonequivalent chlorine atom of the unit cell will have associated with it a total field gradient. For each total field gradient calculated, nine sums, one for each Of the components Of the tensors, are evaluated, multiplied by the charge Of the Site at which they were evaluated and added tO the sum of the previous components calculated, which have also been multiplied by their reSpective charges. In this way an electric field gradient tensor is Obtained with reSpect to a chosen coordinate system. The tensor is then diagonalized to transform it to the principal-axis system. The maximum contribution to the field gradient which may be Obtained in this lattice can thus be Obtained. 122 To illustrate this process consider a fully ionic mole- cule MClg with two molecules per unit cell. Suppose further that each of the chloride ions associated with a particular M2+ occupies a crystallographically nonequivalent position M2+ ions and 4 Cl- ions so that the unit cell consists of two at three nonequivalent positions. Because MClg is totally ionic the measured field gradient would be expected to arise entirely from external contributions Of the crystal lattice. Then, unless both nonequivalent Cl_ sites accidently experience identical Van der Waals forces and identical electric fields due to charges in the lattice, two quadrupole resonance absorp— tions would be eXpected. Furthermore, the difference between the two measured gradients should give some measure Of the solid-state interactions which occur, since in the gas phase both Of the chloride ions should be identical. In order tO Obtain the contribution tO the field gradient from the charges in the lattice,sums at each Of the nonequivalent positions must be evaluated. Designating two Of the chlorines as Cl(A) and the other two as Cl(B) the whole lattice is divided intO sub— lattices,each Sublattice with a different atom from the unit cell at its corner. Since the unit cell contains six atoms there will be Six sublattices; each Sublattice consists Of atoms Of the same charge. TO find the lattice sum at Cl(A) this atom is placed at (000) and the coordinates Of the other five atoms with respect to this origin found. The sums are evaluated to yield a tensor at each of the six points. These 125 tensors are each multiplied by the prOper charge and added together to yield the total field gradient at site A with respect to a chosen coordinate system. To Obtain the field gradient due tO external charges at Site B this whole process must be repeated with one Of the Cl(B) atoms at the origin. To Obtain the principal values Of the tensor and the rela- tion between the principal-axis system and the chosen system, the tensors were diagonalized to give the principal values and the resulting eigenvectors gave the angular relation be- tween the chosen axis system and the principal-axis system. C. Some Details Of the Modification and Use Of LATSUM LATSUM, as it was originally set up, calculated the con— tributions to an internal electric field in the crystal from the electric dipoles situated in the lattice. This was done by evaluating nine sums such as Equation 65; since the tensor system is symmetric and traceless, there are only five inde- pendent components to evaluate. The input data consist Of the three unit cell lengths a, b, and c and the three angles a, 8 and y for the crystal unit cell. Another card must be punched with the convergence limit and the maximum number Of cells N to be summed over. The program sums over successive cells until the value contributed by the next cell is less than the convergence limit or until the number of neighbor cells summed over is equal to N. Values Of N and the con- vergence limit should be chosen as some compromise between 124 speed and accuracy. If N is made large enough the sums may be made to converge to any desired accuracy but this may make the summation process too time-consuming. Values Of N=20 and a convergence limit Of 10‘7 were used at first. However, it was found that some sums which were very close to the plane containing the origin Of the cell did not converge so the convergence limit was changed to 10'”5 and N set equal to 80; with these limits all sums converged satisfactorily. The final output data which the original program needed were the coordinates Of the atom in the unit cell whose sublattice was to be summed over. Each sublattice then required a separate computer run which is unsatisfactory. For example, (TiCl4'POC13)2 has 80 atoms in the unit cell and there are seven crystallographically nonequivalent chlorine sites in the unit cell; this means that 560 sums must be performed. The first change in LATSUM,then,was to allow multiple sums to be done in one computer run. Furthermore, these sums are grouped so that all the sums for a particular lattice site are done consecutively, added, multiplied by their charge and printed out so that the contributions from different Sites may be evaluated. In terms Of the previous example of MClg this means that the two Cl(A) contributions are added together, multiplied by -1.0 and printed. Because of this modification additional information must be supplied to LATSUM, namely, the number of sublattices, the number Of nonequivalent atoms at which the field gradient is desired, the number of atoms in 125 the unit cell which belong to a particular nonequivalent site and the charge associated with this Site. The second change introduced was to add two subroutines which diagonalize the field gradient matrix when it is Ob— tained for a particular site. One of these, SMDIAG, which diagonalizesaasquare matrix by the method of Jacobi, was kindly supplied by Professor Richard Schwendeman. In addition to these major changes in LATSUM, numerous minor changes were also made. D. A Test of LATSUM Before LATSUM was used on the rather complex structures involved in this work, it was desired to test it out on some simpler systems first. The two systems chosen were the low temperature form of CrC13,which was done by Morosin and Narath (48% and CdIa which was done by Jones et al. (105). The former was picked Since it had 24 atoms in the unit cell and was the most complex previous calculation' and also be- cause a reading of the literature indicated that this calcu— lation was done correctly. CdIz was chosen because it had two nonequivalent sites in the unit cell. Although Jones et al. were not correct in their choice of the principal z axis along the sixfold axis in some Of their compounds, their choice was correct in this particular compound. This is veri- fied by the fact that, with the same choice Of the z axis, 126 our calculated tensor was very close to diagonal. The results of the LATSUM calculation are compared to those on CrCls (which were calculated by direct summation in a sphere) and those on CdIa (which were done by the earlier method Of DeWette) in Table 9. Table 9. Comparison of q and n as Calculated Both by LATSUM and by Other Authors — L LATSUM Other Calculations Compound q n q n CrCls -0.45000 0.5240 -0.42602 0.5219 _ a CdIg I (2b) -0.00580 0.1701 -0.00579 -- ca:2 I-(2a) —0.00584 0.1108 —0.00585 —- aThe notation 2a and 2b refers to crystallographically non- equivalent iodine sites. As can be seen the agreement is excellent. The slight differ— ence between values Of q and n for CrCls is probably due tO the superior convergence Of LATSUM. Since the CdIg calculations were made using the same method (that of DeWette) and the same crystal data, it is reassuring to see such good agreement. E. The Crystal Lattice Field Gradient Model and Programs ROTATE and DIAG a) The First Model Before a calculation Of the solid-state effects could be attempted some kind Of a model upon which to base the calcu— lations had to be developed. In this case it was decided to try to explain the line splittings as due to the effect of of‘ r‘ D—v-i 127 charged ions in the crystal lattice. This effect was expected to be large for two reasons. First, the ionicity of the bonds in the complexes averages about 50% with the result that the charge on each Of the sites is Significant. Second, because the atoms are unusually closely packed, the density of charged sites is greatly increased compared to previous crystals on which these calculations had been tried. vThuS, even though the full ionic charges were not used, significant contributions to the measured field gradients were expected. In considering only the contribution Of the charged sites, contributions due to induced dipoles, dipole-dipole interactions, Van der Waals interactions and partial chemical bonds formed between the chlorines in adjacent molecules are neglected. Nevertheless, for reasons given above, this model was expected to give a good first approximation. It was further assumed for the sake of mathematical simplicity that the charged ions could be re- placed by point charges. Using this model it is necessary first tO assign a charge tO each site. This is not easy since there are nO gOOd rules for Obtaining the ionicity Of bonds. The approximate relationships of Pauling (70) and Of Gordy (60), involving the electronegativity, have been used to estimate the ionicity. Pauling's relation has been criticized as being based upon an incorrect interpretation Of dipole moment data and Gordy's method is not really based on any experimental results. Townes and Dailey, working from quadru— pole resonance data, have developed a graph Of bond ionicity 128 versus the difference in electronegativity Of the two atoms involved in the bond (71). This graph was used to assign charges to each of the chloride and oxide ions, the charges on the other atoms were then chosen to maintain charge neutrality in the molecule. It was assumed that, in the com- plexes, there was a single bond between the oxygen atom of POC13 and both the phosphorus atom and the central atom Of the Lewis acid. This assumption may be justified, at least in the case Of SbClS'POCla, by Observing that the Sb-O distance in this complex is 2.188 (107) while the Sb-O distance in Sbgos is 2.27 (108). Using the charges selected as described above the calculation Of the point-charge field gradients was carried out. 2) An Improved Model After the calculation was completed it was thought that a better assignment Of charge could be made if the coupling constants actually found by NQR spectroscopy for POC13, SbCls, TiCl4 and SnCl4 were used. According tO the theory Of Townes and Dailey the measured quadrupole coupling constant ratio p is given by p==1-I-a. ‘Using the rule of Townes and Dailey, a,= 0.15 if the difference in the electronegativities Of the two atoms involved in the bond is greater than 0.25; otherwise, a,= 0. The ionicity (I) can then be calculated if the NQR resonance frequencies are known. Since NQR data are available only for the chlorine nuclei, the charges on the phOSphorus and oxygen atoms and on the 129 central atoms<fifthe Lewis acids are still undetermined. If the charge on oxygen is determined, and is separated into contributions from the central atom and phosphorus, the charges on these atoms may be determined because Of the charge neutrality Of the molecule. The only way to do this is to use the electronegativity differences. The following procedure, explained by means of an example, was used. For a hypothetical molecule Cl-M-O, if we assume there is some linear relationship between electronegativity and bond ionicities, we may write I(Cl) = AA¥(MC1), (68) where I(Cl) is the ionicity Of chlorine and AX(MC1) is the electronegativity difference between atom M and chlorine. Since AX(MC1) is known and I may be calculated from NQR data we can calculate A from Equation 68. It is reasonable to assume that the same relation will hold for the M-0 bond, hence I(O) = AAX(M0) . (69) Using these relations the ionicity of the oxygens was calcu— lated. In our compounds the oxygens were bonded to two atoms; therefore, using SbCls-POCla as an example, in an Obvious extension Of Equation 69, I(O) = AAX(Sb-O) + BAX(P-O), where A and B can be calculated from NQR data on SbCls and POCls. Table 10 lists the charge assigned to each atom. For the oxygen atom in [TiCl4'POC13]2,I(O) = AAX(Ti-O) + BAX(P-o). 150 In this case A was not calculated from the TiCl4 NQR data because it was felt that these data had too large an un- corrected crystal effect because Of the high ionicity Of the Ti-Cl bond and the consequent low value Of p. The value of A calculated from the NQR data would then be tOO large and, in fact, the calculated A was much larger than the A's calculated for SbCls, SnCl4 and POC137 an average Of the other A's was therefore used. In the most elegant approach this set of charges would only be the first approximation to the true charges. They would be used to refine the measured NQR data to extract the molecular field gradients. These molecular field gradients would then be used in the Townes and Dailey relations to Obtain a new set Of charges. This process would be repeated until self consistency was reached. However, it was felt that the model on which the calculations are based is not accurate enough to warrant this procedure. Table 10 gives the charges used in the LATSUM calculations. Since there are two kinds of chlorine atoms in the complexes, Cl(A) designates the chlorines attached to the phOSphorus and Cl(B) the chlorine attached to the central atom Of the Lewis acid. The LATSUM results using these charges are the ones used in further calculations. Townes (71) has estimated that the ionicity calculated using this method is within 20% Of the true value. 151 Table 10. Charges Used in LATSUM Compound Atom Charge Sbc15 Sb 1.625 Sbc1s c1 -o.525 Sbc15-Poc13 Sb 2.185 Sbc15-Poc13 Cl(A) -o.322 SbCls-POCla Cl(B) —o.525 SbCls'POC13 P 1.467 SbCls-POClg o -1.061 SnCl4-2POC13 Sn +2.806 SnCl4-2POC13 Cl(A) -0.322 SnCl4-2POC13 Cl(B) -o.411 SnCl4'2POC13 P +1.467 SnCl4-2POC13 o —1.082 [TiCl4-POC1312 Ti +5.952 [TiCl4°POC13]2 Cl(A) -o.522 [TiCl4-POC13J2 Cl(B) -o.741 [TiCl4°P0Cla]2 p +1.46? [TiC14'P0C13J2 0 -1.489 5) ROTATE LATSUM calculates a field gradient tensor due tO point charges in the lattice according to a particular choice for the directions Of the X, Y and Z axes. This tensor may be diagonalized by a rotation to its principal-axis system. On the other hand the molecular field gradient at a chlorine nucleus has its principal axes oriented such that the z axis is along the bond. Since we assume cylindrical symmetry for 152 the molecular field gradient the orientation of its X and Y axes is arbitrary. Hence, it is only necessary tO rotate the Z axis Of the calculated crystal lattice field gradient tensor SO that it is aligned along the bond; then, since the X and Y axes Of the molecular field gradient are arbitrary, the two coordinate systems will be aligned. We can then directly combine the 22 component of each tensor. A computer program, ROTATE has been written which performs this rotation. ROTATE works in the following manner; any tensor 8 with matrix elements Qij may be rotated to any arbitrary direction by the matrix transformation ST Q S = Q' where Q' is the matrix Of the rotated tensor, S is the matrix Of direction cosines and ST is the transpose of S. This rotation may take place in two (or more) successive rotations if this is more convenient. If the two direction cosine matrices are repre— sented by S; and 82 then S = 8152 and ST = SgTslT, hence Q' = SgTslTQslsg. In this case two successive rotations are performed one in the original XY plane by an angle a.and the other tipping the original Z axis by an angle 8. Program ROTATE is given the coordinates Of the two atoms involved in the bond and the unrotated tensor. ROTATE then calculates the bond direction relative tO the Z direction Of the original choice Of coordinates, calculates S and ST and performs the necessary matrix multiplication. It prints out the rotated matrix and also a, 8 and the bond distance as a check on the calculation. Figure 12 shows how o.and 8 are defined with Figure;12. 155 ACZ' Definition Of the angles d.and 8 as used by ROTATE. YO In F—l LC) ’13 Fr. 154 respect to the molecular bond axis Z and the axis system Of the unrotated tensor X', Y' and 2', which are equivalent to the crystalline a, b and c axes, respectively, for orthor— hombic symmetry. ROTATE is listed in the Appendix. 4) PROGRAM DIAG As a first approximation, one may take the 22 component of the rotated tensor and combine it directly with the measured field gradient to extract the molecular field grad- ient. Another more accurate method is available, however. The field gradient actually measured has principal axes slightly different from the molecular field gradient (although the molecular field gradient is expected tO dominate the measured value) because when the rotated crystal lattice gradient tensor is added to the molecular field gradient ten sor the resulting tensor is no longer diagonal. The Principal-axis orientation Of the measured gradient relative to the bond direction may then be Obtained by diagonalizing the resulting cumulative tensor. The largest element along the trace Of the diagonalized tensor will be the experimentally mea sured field gradient. An asymmetry parameter 7} due to the solid-state effects may also be calculated from the diegonalized tensor. Ideally the solid—state effects Should be the only contributors to this parameter so that the calcu— lated I} should correspond tO the measured 1]. At this point another complication, the Sternheimer factor, must be introduced which may increase or decrease, according 155 to its sign, the contribution of the crystal lattice effects. This has already been discussed but must now be taken into account. If it were known eXactly this would pose no prob- lem.as we would Simply multiply the calculated crystal leattice field gradient tensor by the appropriate factor. Lhafortunately, for several reasons already discussed (Section :I-Ji), the factor is not known. In addition to the previous discussion it should be noted that, although we always treat tries Sternheimer factor 700 as a scalar, because it depends or) the polarizability Of the chlorine atom it should probably be: a second rank tensor. At present it is not possible to take this into account. Or, more accurately, we assume the E 700 0 0 _ OO 0 ym 0 . 0 0 700 If we assume that the Sternheimer factor is known we can tensor is Of the form {ll Ca-:Lculate the molecular field gradient from the rotated crystal la‘itice field gradient tensor and the measured field gradient by the following procedure. Knowing the measured field gre~dient we guess a molecular field gradient which we assume is cylindrically symmetric. In the axis system in which: the Z axis is along the bond direction this trial molecular field grecfilient may be represented as a second-rank tensor Of the £0 llowing form a -2 O O E mOl(trial) = O -% 0 . 0 0 a 156 This is then added to the rotated crystal field gradient tensor and the resulting tensor diagonalized. The absolute value of the largest element on the trace Of the diagonalized tensor is then subtracted from the measured field gradient. This difference is compared tO the difference calculated for the previous iteration. If it is smaller than the previous difference we are going in the proper direction and the trial field gradient is incremented by an element Of the same sign and magnitude aS that used in the previous iteration. If the difference is larger than that of the previous iteration the Sign Of the increment is changed and if the largest value Of the diagonalized tensor oscillates tO one side and the other Of the measured value the magnitude Of the increment is cut in half. This process is continued until the diagonalized teIlsor converges to the measured tensor. The other two values on the trace Of the diagonalized tensor can be used to calcu- late the asymmetry parameter due to the crystal effects and the eigenvectors Of the diagonalized tensor may be used to determine the relative orientations Of the principal axes of the experimental field gradient. The trial field gradient is now the molecular field gradient. A computer program, DIAG, has been written tO perform these iterations and is. listed in the Appendix. The iteration procedure is repeated for a number Of values Of the Sternheimer factor. The method for assigning a Sternheimer factor to a chlorine atom will be illustrated by an example. Consider again MC127 in the gaseous 157 state both chlorine atoms are equivalent, therefore their molecular field gradients are identical. Since in the solid the two chlorines have different experimental field gradients this is clearly a solid-state effect. If we know the crystal structure of MC12 we can apply LATSUM, ROTATE and DIAG. This results in a set Of molecular field gradients as a function of the Sternheimer factor. We then pick the Stern- heimer factor which makes the two molecular field gradients identical. This procedure necessitates the assignment of the correct eXperimental field gradients to sites A and B; however, this may usually be done from an inSpection Of the results of ROTATE. Also, if there is reason to believe that at least a part of the splitting between two nonequivalent sites is due to a difference in the molecular field gradient, this procedure will no longer be valid. IV. RESULTS A. Assignment Of Absorption Frequencies to Specific Atoms in the Complexes With the aid of chemical considerations, relative intensi- ties and ROTATE it is possible to assign each NQR absorption tO a Specific chlorine atom in the molecule. Each compound will now be discussed separately. The crystal structure Of SbCls-POCla was determined by Lindqvist and Branden (106) and the atomic arrangement for the complex is shown in Figure 15; each numbered chlorine atom denotes a crystallographically nonequivalent site. In a similar manner Figures 14 and 15 Show the atomic arrangement for the complexes in SnCl4°2POC13, as found in the X-ray analysis Of the crystal structure by Branden (108), and for the complex [TiCl4'POC13]2 from the X—ray work of Branden and Lindqvist (109). 1) SbClsfPOCla At 770K six absorption lines are Observed for this com- pound, two lines grouped at about 50.5 MHZ, one at about 27.4 MHz, two grouped around 26 MHz and one at about 24.4 MHg. The intensities Of the four lowest lines are in the approxi- mate ratios Of 2:1:1:1. From chemical considerations we expect four different resonances, one from the three POC13 chlorines, one from the axial chlorine atom on the SbCls. 158 159 .mHOOm.mHonm mo masomgos a Amoao AmoHU .ma wusmflm .mHOOmm.¢Hocm mo mesomnos 2 .ea magmas 140 & 141 .NHMHUOm.¢HUHBH HOEHU OS“ MO OHSUOHOE fl .ma onsmflm 142 one from the chlorine atom trans to the POC13 oxygen and one from the two chlorine atoms gig to the POC13 oxygen atom. Reference to Figure 15 shows that there are six nonequivalent chlorine atoms in this complex. AS will be discussed, it is expected that charge transfer will be indicated by an in- crease in the resonance frequencies Of the POC13 chlorine atoms and a decrease in the resonance frequencies Of the chlorine atoms Of the Lewis acid. Thus, the two absorption frequencies at about 50.5 MHZ must be assigned to the POC13 chlorine atoms. Furthermore, the resonance due to a chlorine atom at site 5 should be twice as intense as that due to atoms at Site 4. It is Observed that the higher frequency line is much less intense than the lower frequency line and the higher frequency line is therefore assigned to site 4. This assignment is confirmed by the results of the crystal lattice field gradient calculations which calculate an un- crys Of +0.5 for site 4 and -0.05 for site 5 corrected q (it should be recalled that the molecular field gradients are all positive). The last four lines may be assigned to chlorine atoms bonded to antimony. The highest frequency line is unmistakably more intense than the other three lines each of which has approximately the same intensity. Therefore, this absorption is assigned to the two axial chlorine atoms (Site 6). Each Of the three equatorial chlorine atoms occupies a nonequivalent site SO we expect three separate resonances as observed. Two of these resonances are split 145 by less than 500 kHz while the other resonance lies 1.6 MHz lower in frequency. Hence, the lowest frequency is assigned to the Cl at Site 5, trans to the POC13 oxygen. The point- crys of -0.12 for charge calculations give an uncorrected q site 1 and +0.5 for site 2, hence, the lower frequency is assigned to site 1 and the higher to site 2. i 2) SnClg-ZPOCla At 770K five resonances are found for this compound, which is unfortunate because Figure 15 Shows seven nonequivalent chlorine sites, four for the POCls chlorine atoms and three at the SnCl4 chlorine Sites. Two absorptions may be associ- ated with the POC13 resonances instead of the four predicted. They were assigned to either sites 4 and 5, or 6 and 7, since these belong to different POC13 molecules and the most likely phase transition would be one in which the POC13 molecules are aligned in an equivalent manner. This point will be dis- cussed in more detail in the discussion. The LATSUM calculations were then used to assign the measured frequency to a particular site. It is interesting to note that sites 4 and 6, which should become equivalent if the POC13 mole- cules are rotated into equivalent positions, are always assigned the higher frequency line. The resonance at highest frequency Of the three which come from the SnCl4 chlorine atoms is assigned to Site 5 on the basis Of intensity. crys Of +0.57 while Site 2 has a calculated uncorrected q qcrys for site 1 is +0.42; hence, the line at higher frequency of the two remaining is assigned to site 2. 144 3) _ [TiCl4-POC13]3_ For this compound only the POC13 chlorine resonances could be Observed. Three lines are measured for this com- pound and three nonequivalent chlorine sites (Sites 5, 6 and 7) on the POC13 molecule are predicted. Hence, the NQR and X-ray results are in gOOd agreement for this compound. Since all three resonances are about equal in intensity (also predicted from the crystal structure), we must rely on the point-charge calculations to assign the frequencies. These. calculate uncorrected qcrys values Of -0.18, -0.09, and 0.00 for Sites 5, 6 and 7, respectively. For this reason the highest frequency absorption was assigned to Site 7 and the lowest to Site 5. 4) Pure SbCl5 In SbCls McCall and Gutowsky (110) have Observed three lines at 770K. These lines are themselves multiplets but McCall and Gutowsky report that they seem to center about 27.88, 28.5 and 50.4. It is likely that the two closer spaced lines are associated with either the axial or the equatorial chlorine atoms and that the high frequency line is associated with the other. This spectrum was re-examined in the present work; however, it was not possible to decide whether the high frequency line or the low frequency pair was to be associated with the axial position. The only basis for this decision was the intensity ratio because, since it is believed that the molecular field gradients at the axial and equatorial 145 positions should differ, ROTATE results can not be used. However, the lines were too complex to yield a reliable intensity ratio. Furthermore, X-ray data on SbCls (118) taken at -500C Show only two nonequivalent chlorine sites in the molecule corresponding to the axial and equatorial positions. In an effort to Obtain some new information to help solve this difficulty new NQR measurements were made on SbCls at -25OC; this temperature was chosen because it is quite close to the temperature at which the x-ray data were taken. The frequency region 51 MHz to 20 MHz was searched using the recording technique and two strong lines were found. These lines are quite intense and easily observable on the oscilloscope. There is no doubt that each is a single line. The two lineswere Observed at frequencies Of 25.114 MHz and 25.585 MHZ. Furthermore a comparison of the relative intensi- ties Of the recorded signals clearly shows that the lower frequency line is less intense and the intensity ratio closely approximates 5:2. Hence, the 25.585 MHa line is assigned to the equatorial chlorine atoms while the 25.114 MHz line is assigned to axial chlorine atoms. This assignment parallels the observations of Holmes et al. (111), who found for the tri- gonal bipyramidal molecule PCl4F two lines at 52.54 and 28.99. They also assigned the higher frequency line to the equatorial chlorines on the basis of intensities. It is obvious that a phase transition involving a change in the crystal structure between 770K and 2500K (-25OC) has taken 146 place, both from the change in line multiplicity and the abrupt drop in frequency (~v5 MHz). Working back from these results and using both the known behavior Of lines which have undergone phase transitions, and the fact that the line separation at 2500K (2.5 MHz) and at 770K (2.5 MHz) are equal, it seems quite likely that the lines centered at 50.4 MH; should be assigned to the axial position. B. New Resonance Frequencies and Their Temperature Dependence In this work new resonances were found in the compounds Fec13-90013, SbC15~POC13, TiCl4°2POC13, and (TiCl4oP0C13)2. In addition,the room temperature frequencies were measured for SnCl4-2POC13. The temperature dependence of the most intense SbCls line in SbCls-POClg was also studied. The input to DIAG requires knowledge of the measured field gradients. This quantity is Obtained when the measured quadrupole coupling constant is divided by 23%1941.I where Q(Cl) is the quadrupole moment of the 35Cl nucleus, e is the electronic charge and h is Planck's constant; this factor has the value -2.9552 x 106 when q is desired in units Of statcoulombs per cubic Angstrom (esu/Rs). The factor was calculated with h = 6.627 x 10-27, e = 4.80 x 10‘10 and 0 = -0.085. Since all the quadrupole coupling constants were negative this made all the measured field gradients positive. Although it is impossible to assign a Sign tO ean as measured by pure quadrupole resonance, the sign is taken to be negative for 147 all compounds Of chlorine in which the chlorine has a charge more positive than -1. This conclusion is drawn from data on gaseous chlorine compounds measured by microwave spec- troscopy where the sign Of the coupling constants can be determined eXperimentally. The data indicate that e2qQ be- comes more negative as the chlorine becomes more positive. There is every reason to believe that the sign Of the coupling constant does not change upon changing from the gaseous to the solid state. Table 11 lists the resonance frequencies of all the compounds measured in this work. Data were measured at both liquid nitrogen and room temperature for all resonances fimrwhich this was possible. All chlorine resonances which were ascribed tO the POC13 part Of the molecules dis- appeared at about 2000K. Table 12 lists the results of a temperature study on the most intense line Of SbCls in SbCls- POCla. This line is listed as Cl(6) in Table 11 and has been assigned to the axial chlorines in SbCls as discussed above (Section IV-A). Table 15 presents the coupling constants and the field gradients derived from the resonance frequencies. All frequencies are numbered for convenience of reference in the discussion. Figure 16 gives the data Of Table 12 in graphical form. Table 14 gives the temperature coefficients for all resonances which were observable at room temperature. These coefficients are based upon measurements at only two tempera- tures but only their signs and rough magnitudes are needed. 148 Table 11. Resonance Frequencies for the Compounds Studied in This Work Compound Temperature (OK) Frequency (in MHz‘) SbC15°P0C13a c1(1) 01(1) 01(2) 01(2) 01(5) 01(5) 01(4) 01(4) 01(5) 01(5) 01(6) 01(6) SDC14° 2POC13 01(1) 01(1) 01(2) 01(2) c1(5) 01(5) 01(4) 01(4) 01(5) 01(5) (11014-90013)2 01(5) 01(6) 01(7) FeC13 ' POClg TiCl4' 2POC13 b around 50.1 MHz could nOt Sb015C Equatorial Axial Axial SbCls Equatorial Axial 77 297 77 297 77 297 77 297 77 297 77 297 77 297 77 297 77 297 77 297 77 297 77 77 77 77 25.882 25.570 26.186 25.949 24.454 24.465 50.652 50.565 27.527 26.890 19.807 19.110 19.055 18.875 21.462 20.945 50.215 50.117 29.987 50.112 50.515 50.265 77 Several lines centered 77 77 77 250 250 be resolved. 50.4 28.5 27.88 25.585 25.114 * aThe number in parentheses refers to the numbered atoms in Figures 15, 14 and 15. bready Been discussed. The 77 K measurements on SnCl4-2POC13 are taken from Biedenkapp and Weiss (9). The 77 K measurements on SbCls are taken from McCall and Gutowsky (116). This frequency assignment has al- 149 Table 12. Temperature Dependence Of the Most Intense Line of SbCls-POCla (Line 6 of Table 11) ‘ .-_ _ Temperature (OK) Frequency (MHZ) 77 27.327 165 27.145 190 27.118 250 26.974 297 26.890 150 Table 15. Coupling Constants and Field Gradients for the Compounds Studied in This Work —* Compound Tempgrature eaQq/h (MHz) q(esu/Ra) K SbCls'POCla (1) 77 —51.644 17.476 (1) 297 -50.740 17.170 (2) 77 -52.572 17.722 (2) 297 -51.898 17.562 (5) 77 -48.868 16.556 (5) 297 -48.950 16.557 (4) 77 -61.264 20.751 (5) 77 -61.150 20.686 (6) 77 -54.654 18.494 (6) 297 -55.780 18.198 smut-290013a (1) 77 -59.614 15.405 (1) 297 -58.220 12.955 (2) 77 -58.070 12.882 (2) 297 -57.746 12.775 (5) 77 -42.292 14.511 (5) 297 -41.890 14.175 (4) 77 -60.426 20.447 (5) 77 -60.154 20.549 (TiCl 1:001:92 7(7T 77 -60.626 20.515 (6) 77 -60.224 20.400 (5) 77 -59.974 20.294 FeC13°POCla_ 77 -60.526 20.481 §2§lab Axial 77 -56.18 19.011 Axial 250 -46.228 15.645 Equatorial 77 -60.8 20.574 Equatorial 250 -50.766 17.179 a770K measurements on SnCl4°2POC13 bleiedenkapp and.Weiss (9). b770K measurements on SbCls by McCall and Gutowsky (110). 151 .OHUOm.mHOQm mo mUGOGOmOH macaw mmemusfl umoE mew mo GOHuMHHm> medumnmmEmB .ma mnsmwm AMOV ousumummea oom omm _ omm owe ope - n d d 1 1.93 V q S O I d 3 T. O . u so 5... I 8 b n w nTII. O J ) / .m. / .m. / .rN.s.N / II / / I / 152 Table 14. Temperature Coefficients for the Chlorine Resonances Of Complexed SbCls and SnCl4 - 2:: " i-m _i I Compound Atom Temperature Coefficient (in kHz per degree) SbC15°POC13 1 -2.5 SbC15°POC13 2 -1.1 SbCls-POCla 5 +0.14 SbC15°POC13 6 -2.0 SnCl4-2POC13 1 -5.2 SnCl4'2POC13 2 -0.74 SnCl4-2POC13 5 -2.4 Moreover, the Cl(6) resonance in SbC15°P0C13 which was studied in more detail shows that the graph Of resonance frequency versus temperature is quite linear. C. Compounds in which NO Resonances were Found A large number of compounds were examined in the NQR Spectrometer. Unfortunately, for a number of reasons, most of these failed to yield absorbances in the frequency ranges studied. It was suSpected in some cases, particularly the HgCla complexes and the POC13 complexes, that impurities caused the signals to be missed. It is desirable that these compounds be synthesized again and another attempt be made to find Signals. Another attempt should also be made on the n-donor complexes Of ICl and IC13 because impurities may 155 have also caused these signals to be missed. The resonances of ICl and IC13 themselves are not tOO strong and, since it was found that the intensity Of SbCls and SnCl4 resonances in their complexes was greatly reduced, it is possible that the Signals in the ICl and IC13 complexes are too weak to be found by present methods. However, if care were taken to Optimize all conditions it might be possible tO find signals for these complexes. It would also be interesting to look for the nitrogen quadrupole resonances in these complexes as they have been reported for the pure pyridine derivatives. Differences in the nitrogen quadrupole coupling constants in the pure and complexed molecule could be interpreted in terms of w-electron populations. It is not known why the copper, cobalt and manganese resonances could not be found although they may not be in the frequency range Of the Spectrometer. Table 15 gives the compound examined, the frequency range searched and the conditions Of the search for a number of compounds in which no Signals could be found. In order to Simplify and condense the conditions the following abbrevi- ations have been used: fm = frequency modulation, this is followed by two numbers in parentheses. The first refers to a relative attenuation of the voltage from the modulation unit with numbers ranging from one to six, where one refers to zero attenuation, two refers to a sixth of a turn Of the 10 K potentiometer which is acting as a voltage divider, three is two-sixths Of a turn, etc. The second number refers 154 Table 15. Compounds in Which NQR Absorptions Were Missed W Frequency Region. Compound Searched (in MHz) Conditions p-C6H4FC1 20-40 77°, fm(5, .05) (C5H5CH=N-NHz-NH2)CU 20-40 77:, fm(5, .02) 770, fm(5, .02) 77 fm(1, .02) ((CH30)C3H4CH=N-NHfi-NH2)CU 20-40 770: fm(1, .02) HgC12-2(C5H5N) 17-25 297:, fm(1, .05) 2970 fm(S, .05) 297: fm(1, .02) 77o; fm(1, .05) 77 fm(5, .05) HgC12°2(5-CH3C5H4N) 17-25 77°, fm(1, .05) [(C5H5)3P-HgC12]2 17-25 2973(2, .05) 2970(6, .05) 77 (5, .05) HgC12‘(CH3)2SO 17—25 778 fm(1, .02) 770 fm(1, .05) K3[Co(CN)5N0] 15—54 297° zm(.2) 297° zm(1.0) 29702 fm(1, .02) 297 fm(1, .05) K3[CO(CN)5I] 15-54 Same conditions as K3ICO(CN)5NO] K3[Mn(CN)5N0] 15—54 Same conditions as K3[CO(CN)5NO] CSHSN'ICl 50-45 77° fm C9H7N'ICl 50-45 77°, fm C9H7N-IC13 25-55 77° fm 2-BrC5H4N°ICl 50-45 77° fm 5~NCC5H4N-IC1 50-45 77°, fm SbCls-TiCl4-5POC13 18.5-41 77: fm(7, .05) 77 fm(1, .02) TiC14°K01-5P0C13 24.8-54 77°, fm(4, .05) repeated above at 77 K Continued Table 15 - Continued 155 Frequency Region Compound Searched (in MHZ) Conditions BC13'POC13 24.8-54 77°, fm(4, .05) 5 Different O 241013-90013 24.8-54 770' fm(4, .05) Complexes 77 , fm(1, .02) 81013-p0013 24.8—54 77:, fm(4, .05) 77 , fm(1, .02) Sb013-90013 24.8-54 77:, fm(4, .05) 77 , fm(1, .02) [A1(P0C13)8][SbC16]3 24.8-54 773, fm(4, .05) 77 , fm(1, .02) [A1(P0C13)8][FeCl4]3 24.8—54 77:. fm(4, .05) 77 , fm(1, .02) (TiCl4-P0C13)2 5.5-10.5 77:, fm(1, .02) 77 , fm(1, .01) 156 to the reference attenuation control on the lock-in amplifier. These two settings are the only information needed to repro- duce any of the modulation conditions Of this experiment. Zeeman modulation is denoted by zm followed by a number in parentheses which gives the current in amperes that was passed through the modulation solenoid. The other condition given is the temperature at which the searches were conducted. Most of the searches were conducted at liquid nitrogen temperature (770K) but others were also repeated at room temperature (2970K). It should be noted that, in addition to searching with recording techniques, visual searches were also carried out in all cases. D. LATSUM, ROTATE, AND DIAG Results 1) Tabulated Results Of LATSUM and ROTATE In the hexagonal SbCls crystal the z axis for LATSUM was chosen parallel to the sixfold axis and the x axis was chosen along the crystalline a axis. This means that the tensor for the axial chlorine atoms Should be almost diagonal. This is expected Since the axial chlorines almost lie on this crystal sixfold axis; for this same reason it is expected that n should be very close to zero. Both of these expecta- tions are realized. The three complexes are orthohombic in their crystal symmetry;zhence, the X4‘Y, Z axes of LATSUM were chosen along the crystalline a, b and c axes, respectively. LATSUM was applied to 22 nonequivalent chlorine 157 atoms; the results from both LATSUM and ROTATE are summarized in Tables 16-57. The numbering Of the chlorine atoms refers to that used in Tables 11 and 15 and in Figures 15, 14, and 15. Each table gives the results Of LATSUM and ROTATE for a Single chlorine site. "Tensor" refers to the crystal field gradient tensor calculated with respect to the original choice Of X, Y and Z atoms as given above. "Rotated Tensor" refers to this same tensor after it has been rotated so that its Z axis lies along the bond direction. In order to determine the principal values and the directions of the principal axes, the undiagonalized crystal field gradient tensor, as calculated with respect to the original choice Of coordinates, was trans- formed tO the principal-axis system by diagonalizing it. The eigenvector matrix for this transformation is given in the tables under the heading Of "Eigenvectors." If the axes Of the new coordinate system are denoted by X, Y and Z and those of the Old coordinate system are denoted by X', Y', and 2', then the elements Of the eigenvector matrix are the cosines Of the angles between the X and X' axes, X and Y' axes, etc. The angles along the diagonal Of this matrix are Of Special interest as these correspond to the angles between the X' and X axes, the Y' and Y axes and the Z' and Z axes, respectively. For convenience the arc cosines, rounded to the nearest degree of the elements of the eigenvector matrix:are collected in the section Of the table labeled "Direction Cosine Angles." Finally, the elements on the diagonal of the diagonalized 158 Table 16. LATSUM andaROTATE Results for the SbCls Axial Chlorines Tensor -0.45550 0.00011 0.00000 0.00011 -0.45516 0.00000 0.00000 0.00000 0.86646 Eigenvectors 1.00000 0.00000 0.00000 0.00000 1.00000 0.00000 0.00000 0.00000 1.00000 Angles for the Direction Cosine (in degrees) 0 90 90 90 0 90 90 90 0 qxx = -0.45516 = 0.86646 = -0.45550 = 0.00016 qyy U Rotated Tensor -0.45550 0.00009 0.00000 0.00009 —0.45516 0.00000 0.00000 0.00000 0.86646 159 Table 17. LATSUM and ROTATE Results for the SbCls Equatorial Chlorines Tensor -0.14857 -0.00061 0.00000 -0.00061 0.29075 0.00695 0.00000 0.00695 -0.14125 Eigenvectors 1.00000 -0.00174 0.00154 0.00177 0.99979 -0.02017 -0.00151 0.02018 0.99980 Angles for the Direction Cosines (in degrees) 0 90 90 90 1 91 90 89 1 qxx = -0.14145 = 0.29095 q = —0.14950 n = 0.02774 YY Rotated Tensor -0.14125 -0.00872 0.00000 -0.00872 0.29075 -0.00077 0.00000 -0.00077 -0.14867 160 Table 18. LATSUM and ROTATE Results for the SbC15°POC13 Cl(1) Chlorines Tensor 0.11550 0.00004 -0.21298 0.00004 -0.15028 -0.00001 -0.21298 -0.00001 0.05679 Eigenvectors 0.76721 -0.00155 0.64159 0.00008 1.00000 0.00200 -0.64159 -0.00148 0.76721 Angles for the Direction Cosines (in degrees) 40 90 50 90 0 90 150 90 40 qxx = -0.14127 q = 0.29155 q = -0.15028 n = 0.05090 YY Rotated Tensor 0.27098 0.00005 0.09210 0.00005 -0.15028 0.00005 0.09210 0.00005 -0.12069 161 Table 19. LATSUM and ROTATE Results for the SbCls'POCla Cl(2) Chlorines Tensor 0.21654 0.00000 -0.18190 0.00000 —0.15559 0.00000 -0.18190 0.00000 +0.08095 Eigenvectors 0.90561 0.00000 0.42855 0.00000 1.00000 0.00000 -0.42855 0.00000 0.90561 Angles for the Direction Cosines (in degrees) 25 90 65 90 0 90 115 90 25 qxx = -0.15559 q = 0.50277 q = -0.16718 n = 0.10454 YY Rotated Tensor -0.16568 0.00000 —0.02647 0.00000 -0.15559 0.00000 -0.02647 0.00000 0.50127 162 Table 20. LATSUM and ROTATE Results for the SbCls‘P0C13 Cl(5) Chlorines Tensor -0.00845 0.00000 0.21982 0.00000 -0.15804 0.00000 0.21982 0.00000 0.16647 Eigenvectors 0.82754 0.00000 0.56141 0.00000 1.00000 0.00000 —0.56141 0.00000 0.82754 Angles for the Direction Cosines (in degrees) 54 90 56 90 0 90 124 90 54 qu = -0.15756 q = 0.51560 = -0.15805 = 0.00155 qyy n Rotated Tensor 0.25266 0.00000 0.16067 0.00000 -0.15804 0.00000 0.16067 0.00000 -0.09462 Table 21. LATSUM and ROTATE Cl(4) Chlorines 165 Results for the SbC15°POC13 Tensor 0.26864 -0.00017 0.14878 Eigenvectors 0.94897 -0.00054 0.51557 Angles for the 18 90 90 0 72 90 -0.15904 -0.17904 qXX qyy Rotated Tensor —0.17654 -0.00006 0.05658 -0.00017 -0.15907 0.00000 -0.00012 1.00000 0.00141 0.14878 0.00000 -0.12960 -0.51557 -0.00158 0.94897 Direction Cosines (in degrees) 108 90 18 q = 0.51808 n = 0.12575 -0.00006 0.05658 -0.15904 -0.00016 -0.00016 0.51558 164 Table 22. LATSUM and ROTATE Results for the SbCls-POC13 Cl(5) Chlorines Tensor -0.04165 -0.19965 -0.07007 Eigenvectors 0.60594 0.59175 -0.55596 Angles for the 55 120 54 57 122 71 -0.15128 -0.17527 qxx qyy Rotated Tensor -0.15674 -0.05556 -0.04667 -0.19965 -0.07007 0.14861 0.15515 0.15515 -0.10699 -0.49779 0.62247 0.80524 0.06824 0.52712 0.77967 Direction Cosines (in degrees) 52 86 59 0.52655 0.07546 q W -0.05556 -0.04667 0.18488 0.21284 0.21284 -0.02816 165 Table 25. LATSUM and ROTATE Results for the SbC15°P0C13 Cl(6) Chlorines Tensor -0.05492 0.05879 0.00598 0.05879 -0.00829 -0.11598 0.00598 -0.11598 0.06521 Eigenvectors 0.52045 0.84905 -0.09102 -0.70910 0.57056 -0.60001 -0.47571 0.57682 0.79480 Angles for the Direction Cosines (in degrees) 59 52 95 155 68 127 118 68 57 qxx = -0.05554 q = 0.14857 q = -0.11522 n = 0.52420 YY Rotated Tensor 0.04555 -0.00545 -0.11845 -0.00545 -0.05241 -0.05989 -0.11845 -0.05989 0.00706 166 Table 24. LATSUM and ROTATE Results for the SnCl4°2POC13 Cl(1) Chlorines Tensor 0.15626 0.51417 0.00000 0.51417 0.04055 0.00000 0.00000 0.00000 -0.19658 Eigenvectors 0.76858 -0.65975 0.00000 0.65975 0.76858 0.00000 0.00000 0.00000 1.00000 Angles for the Direction Cosines (in degrees) 40 150 90 50 40 90 90 90 0 qxx = -0.19658 q = 0.41776 q = -0.22118 n = 0.05889 YY Rotated Tensor -0.19658 0.00000 0.00000 0.00000 -0.22028 0.02588 0.00000 0.02588 0.41687 167 Table 25. LATSUM and ROTATE Results for the SnCl4-2POC13 Cl(2) Chlorines Tensor -0.10000 -0.19751 0.00000 -0.19751 0.29115 0.00000 0.00000 0.00000 -0.19114 Eigenvectors 0.92294 -0.58495 0.00000 0.58495 0.92294 0.00000 0.00000 0.00000 1.00000 Angles for the Direction Cosines (in degrees) 25 115 90 67 25 90 90 90 0 qxx = -0.18258 = 0.57555 q = -0.19114 n = 0.02545 YY Rotated Tensor -0.19114 0.00000 0.00000 0.00000 -0.18175 -0.01897 0.00000 -0.01897 0.57288 168 Table 26. LATSUM and ROTATE Results for the SnCl4-2POC13 Cl(5) Chlorines Tensor -0.16016 -0.00225 0.11825 —0.00225 -0.20257 -0.02924 0.11825 -0.02924 0.56254 Eigenvectors 0.95905 -0.18980 0.21024 0.20424 0.97770 -0.04904 -0.19624 0.08997 0.97642 Angles for the Direction Cosines (in degrees) 16 101 78 78 12 95 101 85 12 qxx = -0.18485 q = 0.58946 q = -0.20465 n = 0.05084 YY Rotated Tensor —0.18666 0.00810 0.05455 0.00810 —0.20070 0.00547 0.05455 0.00547 0.58757 169 Table 27. LATSUM and ROTATE Results for the SnCl4-2POC13 Cl(4) Chlorines Tensor -0.18220 0.01279 0.00771 Eigenvectors 0.96885 -0.02597 -0.24657 Angles for the 14 89 91 1 104 90 -0.15220 -0.18448 qxx qyy Rotated Tensor -0.15416 -0.00769 -0.00068 0.01279 0.00771 0.55656 -0.00056 -0.00056 -0.15416 0.02464 0.24651 0.99970 -0.00574 -0.00055 0.96912 Direction Cosines (in degrees) 76 90 14 q = 0.55667 n = 0.09588 -0.00769 -0.00068 -0.18025 -0.05425 -0.05425 0.55441 170 Table 28. LATSUM and ROTATE Results for the SnCl4-2POC13 Cl(5) Chlorines Tensor -0.06271 0.06668 0.18255 0.06668 -0.08149 0.12282 0.18255 0.12282 0.14419 Eigenvectors 0.84217 —0.26575 0.47050 0.10115 0.95599 0.54269 -0.52964 -0.24104 0.81525 Angles for the Direction Cosines (in degrees) 55 105 62 84 21 70 122 104 56 qxx== -0.15201 q = 0.50150 q = -0.16949 n = 0.12451 YY Rotated Tensor -0.16528 0.01014 -0.01521 0.01014 -0.15520 0.05552 -0.01521 0.05552 0.29847 171 Table 29. LATSUM and ROTATE Results for the SnCl4-2TOC13 Cl(6) Chlorines ‘M TEn's'Or , 0.25254 -0.12295 0.00000 -0.12295 -0.11008 -0.00000 0.00000 0.00000 -0.14226 Eigenvectors 0.95592 0.29564 0.00000 -0.29564 0.95592 0.00000 0.00000 0.00000 1.00000 Angles for the Direction Cosines (in degrees) 17 75 90 107 17 90 90 90 0 qxx = -0.14226 q = 0.29010 = -0.14784 = 0.01925 qyy n Rotated Tensor -0.14226 0.00000 0.00000 0.00000 -0.14715 -0.01758 0.00000 -0.01758 0.28941 Ii 172 Table 50. LATSUM and ROTATE Results for the SnCl4°2POC13 Cl(7) Chlorines Tensor -0.17155 —0.01846 -0.02790 -0.01846 -0.05017 0.25611 —0.02790 0.25611 0.20150 Eigenvectors 0.99794 0.01725 -0.06182 0.01900 0.84070 0.54117 0.06150 -0.54125 0.85864 Angles for the Direction Cosines (in degrees) 4 89 94 89 55 57 86 125 55 qxx = -0.17559 q = 0.56882 q = -0.19545 n = 0.05976 YY Rotated Tensor 0.28085 0.00467 -0.20465 0.00467 -0.17559 0.00040 -0.20465 0.00040 -0.10724 175 Table 51. LATSUM and ROTATE Results for the (TiCl4-P0C13)2 Cl(1) Chlorines Tensor 0.10915 -0.14095 0.20545 —0.14095 0.26921 0.05101 0.20545 0.05101 -0.57854 Eigenvectors 0.74710 -0.55866 -0.56020 0.56114 0.82054 -0.10875 0.55651 -0.12088 0.92652 Angles for the Direction Cosines (in degrees) 42 124 111 56 55 96 69 97 22 qxx = 0.10125 q = -0.46184 q = 0.56059 n = 0.56154 YY Rotated Tensor -0.27098 0.07019 —0.26557 0.07019 0.55078 0.00584 -0.26557 0.00584 -0.07981 174 Table 52. LATSUM and ROTATE Results for the (TiCl4-P0C13)2 Cl(2) Chlorines Tensor 0.56558 -0.25411 0.09752 -0.25411 -0.25465 -0.01975 0.09752 -0.01975 -0.51092 Eigenvectors -0.96149 0.22749 0.15422 -0.25444 0.52466 0.81240 0.10590 -0.82055 0.56254 Angles for the Direction Cosines (in degrees) 16 77 81 105 58 56 84 145 56 qxx = -0.51277 q = 0.65805 qyy = -0.52528 n = 0.01961 Rotated Tensor -0.52141 -0.01677 0.01959 -0.01677 -0.10120 -0.59827 0.01959 -0.59827 0.42262 175 Table 35. LATSUM and ROTATE Results for the (TiCl4-POC13)2 Cl(5) Chlorines Tensor -0.24047 0.22476 0.12810 0.22476 0.59100 0.57115 0.12810 0.57115 -0.15055 Eigenvectors 0.88856 0.27751 -0.56551 -0.40189 0.85487 -0.52815 0.22124 0.45858 0.87115 Angles for the Direction Cosines (in degrees) 27 74 111 114 51 109 77 64 29 qxx = -0.51024 q = 0.65428 q = —0.54404 n = 0.05166 YY Rotated Tensor -0.52560 -0.06758 0.07827 -0.06758 -0.05657 —0.45761 0.07827 -0.45761 0.56197 176 Table 54. LATSUM and ROTATE Results for the (TiCl4-P0C13)2 Cl(4) Chlorines Tensor -0.25476 0.04995 -0.28551 0.04995 -0.28522 -0.21410 -0.28551 -0.21410 0.55798 Eigenvectors 0.74071 -0.60407 -0.29401 0.56175 0.79695 -0.22217 0.56851 -0.00060 0.92962 Angles for the Direction Cosines (in degrees) 42 127 107 56 57 105 68 90 22 qxx = -0.52091 g = 0.67874 q = —0.55784 n = 0.05441 YY Rotated Tensor —0.11555 0.15127 —0.57604 0.15127 -0.25000 -0.29802 -0.57604 -0.29802 0.54544 177 Table 55. LATSUM and ROTATE Results for the (TiCl4-POC13)2 Cl(5) Chlorines Tensor -0.00561 0.22498 0.04590 0.22498 0.11156 0.09510 0.04591 0.09510 -0.10794 Eigenvectors 0.68479 0.58681 -0.45211 -0.65190 0.77550 0.04901 0.56500 0.25949 0.90049 Angles for the Direction Cosines (in degrees) 47 54 116 129 59 87 69 76 26 qxx = -0.12480 q = 0.51168 qyy = -0.18689 n = 0.19921 Rotated Tensor -0.09195 -0.11476 0.02851 -0.11475 0.26581 —0.07192 0.02851 -0.07192 -0.17585 178 Table 56. LATSUM and ROTATE Results for the (TiCl4-P0C13)2 Cl(6) Chlorines Tensor -0.05496 -0.18458 -0.05695 -0.18458 0.15611 0.06092 -0.05695 0.06092 -0.12115 Eigenvectors 0.85574 -0.51158 0.09706 0.52065 0.84155 -0.14519 -0.00758 0.17448 0.98465 Angles for the Direction Cosines (in degrees) 51 121 84 59 55 98 90 80 10 qxx = -0.15577 g = 0.28086 q = —0.14708 n = 0.04759 YY Rotated Tensor —0.10799 -0.09482 -0.05485 -0.09485 0.20052 0.15726 -0.05485 0.15726 -0.09255 179 Table 57. LATSUM and ROTATE Results for the (TiCl4-P0C13)2 Cl(7) Chlorines Tensor -0.04414 -0.05579 0.18877 Eigenvectors 0.81450 -0.26075 -0.51859 Angles for the 55 72 105 18 121 89 -0.14558 -0.15289 qxx qyy Rotated Tensor 0.08197 0.12112 0.18642 -0.05579 0.18877 -0.15275 -0.06654 -0.06654 0.17687 0.51225 0.48952 0.94992 -0.17224 0.01267 0.85495 Direction Cosines (in degrees) 61 100 51 q = 0.29827 n = 0.02518 0.12112 0.18642 -0.08255 0.10275 0.10275 0.00058 180 matrix qxx’ qyy' and qzz E q are collected, along With the crystal field asymmetry parameter n. 2) Comparison of the Lattice Sum Results Using Both the First Model and the Revised Model In order to facilitate the comparison of calculations using the charges assigned by the method of Townes and Dailey (old charges), and those using charges calculated from the NQR data (new charges), values of q E and n calculated using qzz both the old charges and the new charges are collected in Table 58. As can be seen, the results are quite sensitive to the charges assigned to the sites which is a not unexpected result. 5) DIAG Results In Table 59 the results of DIAG, as applied to chlorine atoms which should have identical molecular field gradients but occupy nonequivalent sites in the crystal lattice, are given. Thus, the difference between the two measured field gradients should be due entirely to solid state effects. The size of these effects, following our model, will be determined mol + crys by the Sternheimer factor. If we write q2 = qzz 22 then lqu z(meas)l = zlqzz(a)-qzz(b)l = Ichrys|= lqcrys(a) _ qggys(b)l, where qz is the measured field gradient, qul and crys 22 have been defined previously, and qzz(a) means the field gradient at site a. Application of DIAG to the calculated and measured field gradients then allows us to estimate a Sternheimer factor. This is done by applying DIAG to the measured field gradient, using a number of different Stern— heimer factors, and a series of molecular field gradients as 181 mammo.o nmmmm.o womao.o summm.o Asvao mmnwo.o mmomm.o mmmmo.o mmomm.o Amvao ammma.o mwaam.0 w>¢mo.o nmmmm.o Amvao aeemo.o enmnm.o memea.o ammam.o Aevao mmamo.o mmemm.o ammao.o mmmam.o Amvao Homao.o mommm.o omaa.o ¢>Nm¢.o ANVHU «mamm.o emfim¢.ou m0>m.0 mammm.on Advao NHmHuom.¢HUHBH mammo.o mmmmm.o «osmo.o mmmms.o Anvao mmmao.o oaomm.o smama.o «mamm.o Amvao Hmwmfi.o omHom.o mmeno.o m0~am.o Amvao mommo.o pmmmm.o aeamo.o memmm.o vaao wwomo.o memmm.o mmsmo.o sommm.o Amvao mammo.o mmmnm.o mm~>o.o mmmmm.o ANVHU mmmmO.o mnhaw.o ommmd.o mwmam.o Aavao mHUOmN.¢HUcm omwmm.o >mm¢a.o mm0>.o mmoma.o Amvao msmno.o mmmmm.o ammo.o mnemm.o Amvao mumma.o momam.o mmaa.o mmawm.o vaao mmaoo.o ommam.o mmmo.o scumm.o Amvao emeoa.o unmom.o sama.o mommm.o ANVHU 0momo.o mmamm.o ammo.o demo¢.o Advao mauom.maonm assmo.o mmomm.o mssmo.o mmmom.o Aumsumcao maooo.o mwmmw.o Hmooo.o omnam.o AHMmeVHU macaw c U c v Jlmmommnu 3oz mwoumso 0H0 Eoud chomfioo ammumso 6H0 use mcamo muasmmm zomemq on mmmumno 3oz may mchD muasmmm zoma¢q mo comflumdaoo .mm magma 182 HNN.0 fimd.0 N.0I an AmVHUIAFVHU 00fi.0 000.0 N.0I >5 AmVHUIAmVHU mad.0 mm0.0 N.0| hm AmVHUIAhVHU Namauom.¢aoflav 000.0. nmm.0 m>.0+ mm ABVHUIAmVHU mm0.0 mmo.0 >.HI >5 AmVHOIvaao 00H.0 «$0.0 0.NI nmm ANVHUIAfiVHU mmm.0 ¢¢0.0 0.0fil >5 ANVHUIAHVHU MHUOmN.“HUcm m¢0.0 ohm.0 0.0+ mm AmVHUIAevHU Nmm.0 Nfi¢.0 >0.0+ nmm ANVHUIAHVHU mwN.0 0H¢.0 #.0+ 55 ANVHUIAdVHU «.38 .3006 00 Ammmo Mmtfi a can: _m>HUU<_ _ &<_ :Hmucmfiflnmmxm: musumumemB mEOud 0cm UCDOQEOU 00? Mo mmsHm> samucmeflummxm: 0cm _U<_ mmCfluuHHmm mafia .mm manna 185 a function of the Sternheimer factors is obtained. Let us, as an example, consider Cl(1) and Cl(2) on SbC15°P0C13 (see Figure 15). These two chlorine atoms are expected to have identical molecular field gradients since they both occupy equatorial positions gig to the POCla oxygen atom. We com- pare the results of DIAG for these atoms and see that for a Sternheimer factor of +0.4 the experimental results obtained at liquid nitrogen temperatures yield the same molecular field gradient. It should be recalled that DIAG calculates a molecular field gradient with a series of trial Sternheimer factors. For a pair of chlorines which occupy nonequivalent positions in the crystal lattice.but should be identical in the isolated molecule, the "experimental" 700 is then taken as that 700 which yields an identical molecular field gradient at each of the two chlorine sites. With a Sternheimer factor of +0.07 the room temperature experimental results yield an identical molecular field gradient. These, then are the "experimental" ybo's. For SnCl4°2POC13 four nonequivalent positions (two on each P0C13 molecule) are predicted for the P0C13 chlorine atoms; however, only two resonance lines are observed. For reasons to be given in the discussion of the temperature dependence of the absorption lines, it was assumed that these two measured lines resulted from only one POClg mole- cule but it is not knoWn whether the POCls molecule containing Cl(4) and Cl(5), or that Containing Cl(6) and Cl(7) gives rise to the absorption. Therefore, the DIAG results for each pair 184 mom.0m 00.0 m.5m 0m.5m N00.0 a00.0+ 55 A50HU mom.0m 0¢.0 m.ma om.mH N00.0 Nm0.0I 55 vaH0 mom.0m 00.0 m.ma 0m.ma mm0.0 M5H.0| 55 AmVHU m 7.30m @403. 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It may be argued that, since SnCl4 accepts two POC13 molecules, the AI for this compound should be doubled. This is a matter of definition but it is interesting to note in this respect that infrared studies reveal that the negative shift of the 1500 cm"1 P-O bond of POC13 upon complex formation was 95 cm-1 in both TiCl4°2POC13 and (TiCl4-POC13)2 while that of 5110143290013 was 85 cm‘1 (128). The larger shift is correlated with a larger charge transfer from the P-O bond, hence, IR results predict that TiCl4 is a stronger acid than SnCl4 and also suggest that TiCl4 accepts the same amount of charge from POC13 whether it coordinates with one or two molecules. It should be noted that the thermodynamic data disagree with the ordering of the Lewis acids proposed here. However, this is not surprising since the base used in the thermodynamic studies was benzaldehyde, and it is often found that the order of acid strength is . changed when the standard base is changed. For example, infra- red data and the present NQR results show that, with respect to POClg, TiCl4 is a stronger acid than SnCl4 but the reverse is true if the ordering base is (C6H5)2PO (152). D. Shifts in the NQR Spectra of SnCliiand SbCls Upon Complex Formation 1) General Comments Although NQR data for only two Lewis acids, involved as components of a complex, are available, it is still prOper to 205 point out a few similarities between the spectra of the two complexed Lewis acids. The general appearance of the two spectra is quite similar, both spectra have a group of absorptions at a low frequency (two for SnCl4 and three for SbCls) which are quite close together. In both cases these absorptions belong to the chlorine atoms which lie in a plane, which for SbCls would correspond to the equatorial (basal) P plane of the free molecule (assuming that the POC13 approaches SbCls in the basal plane), and for SnCl4 would correspond to a somewhat analogous plane. The other absorption line, which in SbCls is due to the axial chlorine atoms, lies about L 2 MHz higher in frequency than that for the basal chlorine atoms. This pattern is not due to solid-state effects as the point-charge results indicate that, if this were the case, the resonance line due to the Cl(2) chlorine atom of SbCls- POC13 would be at a higher frequency than the resonance line due to the two axial Cl(5) chlorine atoms which is contrary to observation. Furthermore, the point charge effects by them- selves would put the NQR line due to Cl(1) of SnCl4'P0C13 higher in frequency than those due to Cl(2) and Cl(5), again contrary to observation. The available data suggest that the metal bonding orbitals directed towards the "basal" plane positions (from Sb to Cl(1), Cl(2), Cl(5) and O in SbC15°POC13 and from Sn to Cl(1), Cl(2) and the two POC13 oxygen atoms in SnCl4'2POC13) are different from those directed towards the "axial" positions. Possibly there is some similarity between 206 the "basal" metal atom orbitals in the SbCls complex and in the SnCl4 complex; some similarity may also exist between the bonds to the "axial" positions in the two complexes. More data is needed to substantiate or disprove this sug- gestion. 2) SnCl4-2POC13 Livingston (127) has studied the NQR spectrum of SnCl4 at 770K using a regenerative oscillator. He found four very closely spaced lines whose average frequency is 24.095 MHz. All the measured frequencies for SnCl4-2POC13 which have been assigned in this work to the SnCl4 molecule are lower in frequency than the average value of 24.095 MHz which he re— ported. This is expected if the change in frequency is due to an inductive gain of electronic charge by the SnCl4 chlorine atoms when the tin atom accepts charge from the POC13 oxygen atoms. The difference between the frequencies of the "basal" chlorines and the "axial" chlorines has already been interpreted to suggest a difference in the nature of the metal bonding orbitals directed towards the "axial" and "basal" positions. Van Der Doorn and Drago (129) have recently studied the bonding in the trigonal bipyramidal phosphorus(V) chlorofluorides by means of extended Hfickel calculations. They have interpreted the difference in the phosphorus bonding orbitals as a difference in the electronegativity of these ‘ orbitals. Because the equatorial bonds have a large 3 hybridi- zation they are more electronegative while the more 207 electropositive orbitals are directed towards the axial positions. Thus, the more electronegative atoms will be in the axial positions; this assumption suffices to predict the structuresci'all the phosphorus chlorofluorides. Also, PC14F,which is thought to retain its trigonal bipyramidal structure in the solid state (PCls does not),has been studied by NQR (111). The results show that the absorption of the axial chlorine lies about 5.5 MHz lower in frequency than the absorption of the equatorial chlorine atoms. This would be consistent with the higher ionicity of the P-Cl axial bond which is expected if the phosphorus bonds to the axial posi- tions are more electropositive and in fact points to a quite sizeable difference in ionicity between the axial and equa- torial P-Cl bonds (AI“’0.07). Furthermore, measurements performed during the present work on SbCls at 2500K show that the axial chlorine atoms absorb at about 2.4 MHz lower in frequency than the equatorial chlorine atoms (AIA/0.05). These are the only NQR measurements made on molecules which are known to retain their trigonal bipyramidal geometry in the solid-state. For the Cl(1), Cl(2), and Cl(5) NQR absorp- tions in SnCl4‘2POC13 the calculated 022 values would group the Cl(2) and Cl(5) absorptions closely together and put the Cl(1) absorption at a somewhat higher frequency. At first glance this may seen to fit the observed pattern but two things strongly argue against accepting this assignment of lines. First, from X-ray data it is apparent that the Cl(5) 208 absorption should be twice as intense as the absorption due to either Cl(1) or Cl(2). The highest frequency line is noticeably more intense than the other two lines. It seems reasonable, therefore, to assign this absorption to Cl(5). Second, if Cl(1) is assigned to the highest frequency line on the basis of crystal lattice effects, in order to account for the observed splitting in terms of the calculated 422 values (1 - 703) must be taken to be 42.0 which is quite un- reasonable. It seems then that the splitting between the high frequency line and the two low frequency lines is due to a difference in the molecular field gradients at the "axial" and "basal" chlorine sites. Since it is unlikely that the s and d hybridization at the different chlorine nuclei would change very much, the difference must be accounted for by dif- ferences in ionicity and w-character of the Sn-Cl bonds. Both of these differences would arise due to nonequivalence of the tin bonding orbitals. No additional information is gained if the Sn-Cl bond lengths for the complexed SnCl4 are studied as these seem about equal, within the standard deviations of the X—ray data. If, as a working hypothesis, we assume that the difference is entirely due to a difference in the ionicities of the two types of Sn-Cl bonds, it is possible to calculate the actual charge transferred. This is a logical extension of the idea that all the tin bonding orbi- tals are not equivalent, for if, as in the case of the phos- phorus(V) chlorofluorides, the main difference between the 209 tin bonding orbitals is that one set is more electronegative than the other, it is natural to expect that the more electro- negative orbitals will get a larger share of the charge transferred to the Sn from POC13. The Sn-Cl bonds which are formed with the more electronegative orbitals will then show a larger gain in ionicity and consequently the chlorine atom involved will have a lower resonance frequency. Table 44 is constructed to show this effect quantitatively. The column labeled AI shows the change in ionicity calculated from the equations p = 1 - I - a JTU_+ 0 and 0(SDC14'2POC13) - p(SnCl4) 3 AP = - AI(AQ« = AT: A0 =0) From the definition of Ap it is obvious that a positive AI corresponds to an increase in the ionicity of the Sn-Cl bond under consideration. The column under "corrected AI"(Table 44) was calculated after correcting thelchlorine absorption fre- quencies for solid-state effects assuming 70) = 0. This was done more as an indication of the error involved in neglecting solid-state effects rather than as a realistic attempt to make corrections since no X-ray data exist for SnCl4. The chlorine resonance frequencies for SnCl4 and SnCl4-2POC13 at 770K were used. The total charge transferred from the oxygen to the tin-atom may then be calculated from the uncor- rected values of AI by taking the weighted sum 2(0.054) + 2(0.076) = 0.260e. This is a reasonable answer but it is clear that more data on SnCl4 charge-transfer complexes of 210 Table 44. Charge Transfer in Complexed SnCl4 Compound p AI AI(corrected) SnCla , 0.459 -- -- SDCIL' ZPOC 13 01(3) 0.585 0.054 0.064 Cl(1) and Cl(2)a 0.354 0.076 0.087 aAverage of the p values measured for Cl(1) and Cl(2). 211 known crystal structure must be obtained in order to confirm or deny the conclusions drawn here. 5).SbC15°POCla The abnormal behavior with temperature for chlorine resonance frequencies in SbCls has already been discussed in Section IV. Because there are no data available (such as values of dielectric constant as a function of temperature) which Could give any information on phase changes, either for these complexes or for those of SbCls, the cause of this abnormal behavior is not known for certain. Although it is normal for absorption frequencies to change abruptly at a phase transition, the dr0p in frequency of 4.5 MHz observed for the chlorine resonance in pure SbCls is distinctly abnormal (about 0.5 MHz would be normal). A phase transition would account for the observed changes but X-ray data taken at 770K along with a study of the variation of the NQR spectrum with temperature would be needed to establish whether this is the correct explanation. The very large variation in frequency strongly affects the interpretation of the observed chlorine resonances for the chlorine atoms of SbCls in SbC15°POC13. If the interpretation of the NQR results for the complex are based on the data for SbCls at 2500K there would be an un- explained rise in frequency for the axial chlorine atoms whereas a drop would be expected. Similarly the drops in frequency for the equatorial chlorine atoms would become smaller than expected. It would not be easy to explain these 212 changes, especially since the X-ray data show no dramatic changes in the bond lengths of the Sb-Cl bonds and large decreases in s hybridization and/or double bonding in the Sb-Cl bonds would be needed to explain these changes (an examination of Table 40 will show that solid-state effects cannot account for the changes). On the other hand, if we accept the NQR results at 770K and also assign the higher frequency group at 50.4 MHz to the equatorial chlorines, the results agree quite well with those found for SnCl4. Again, the axial chlorine atoms receive a smaller charge than do the equatorial chlorine atoms. If, as expected, the complexed SbCls retains some identity with the uncomplexed SbCls there is every reason to believe that the Sb-Cl bonds involving Cl(1), Cl(2), and Cl(5) will be different from those involving Cl(6). Further,if theresults of Van der Doorn and Drago can be extended from PC15 to SbCls, and this seems like a reason- able extension, then the basal positions should receive the largest change. Table 45 presents results similar to those of 44 using the frequencies for SbCls'POCls and for SbCls measured at liquid nitrogen temperatures. The values of p for the equatorial SbCls chlorine atoms and for Cl(1) and Cl(2) of SbCls-POCla are obtained by taking an average of the observed resonance frequencies.v The column "AI corrected"(Table 45) gives the value of AI calculated after correcting the observed ean for the solid-state effects assuming 7a): 0. In this case the correction is quite small. However, it should be emphasized 215 Table 45. Charge Transfer in Complexed SbCls Compound p AI AI(corrected) SbCls _ (axial) 0.512 -- —_ (equatorial) 0.554 -- __ SbCls'POClg Cl(1) and 01(2)a 0.474 0.080 0.083 01(3) 0.445 0.109 0.106 Cl(6) 0.498 0.014 0.014 aAverage of p values measured for Cl(1) and Cl(2). that these corrected values of AI are probably not any better than the uncorrected values and only serve to give an idea of the error involved if the solid-state effects are neglected since there is considerable uncertainty over the value of 700' Also, in correcting for the solid-state effects only p for the complex has been corrected and solid-state effects in SbCls and SnCl4 themselves have been neglected. The total charge transferred from POC13 to SbCls may be calculated as 2(0.080) + 2(0.014) + 0.109 = 0.297e. Comparison of this result with that calculated for SnCl4-2POC13 (0.260e) shows that both are about the expected magnitude and their relative magnitudes also look right. 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Tyree, J. Am. Chem. Soc., 59, 4775 (1958). P. Van Der Doorn and R. Drago, J. Am. Chem. Soc., 55, 5255 (1966). C. Branden and I. Lindqvist, Acta Chem. Scand., 41, 555 (1965). C. Branden, A. Hansen, Y. Hermodsson and I. Lindqvist, U. S. Dept. of Comm., Office Tech. Service, AD265, 516 (1961). J. Sheldon and S. Tyree, J. Am. Chem. Soc., _4, 2290 (1959). APPENDIX The computer programs ROTATE and DIAG, written during this work, have already been discussed; they are listed here along with a description of their input parameters. It should be noted that, although ROTATE is completely general, it should be used with care for any crystal whose unit cell is less symmetric than hexagonal. Also, DIAG was written for the case in which the molecular field gradient is cylindically symmetrical. The input parameters are discussed below. 1) ROTATE NCASE-IS format gives the number of tensors to be rotated. X1, Y1, Z1, X2, Y2, Z2 - The coordinates of the two atoms forming the bond to which the z-axis of the calculated tensor is to be rotated, X2, Y2, 22 refer to the coordinates of the quadrupolar nucleus. A1, A2, A5 - The crystalline unit cell a, b, c parameters. These must be in the same order as used for LATSUM. ALPH, BET, GAM - The angles between A2 and A5, A1 and A5 and A1 and A2, respectively. Q(I,J) - The elements of the tensor to be rotated. The value of NCASE is only given once, the other input parameters must be repeated for each case. 225 224 2) DIAG (Q(I,J) - The elements of the rotated tensor as obtained from ROTATE. V(I) - The first guess for the molecular field gradients on the diagonal (for example V(5) refers to qzz(mol)). ST - The starting value for (1 - 700). VV(I) - The diagonal elements of the measured field gradient tensor. At present only VV(5) = q(exp) is used in the program. NN - The continuation parameter, if NN = 0 the program stops, otherwise it reads the next set of Q, V, VV and ST values. 15 20 16 21 22 25 17 225 PROGRAM ROTATE DIMENSION s(3.3).ST(3,3),Q(5.3).QR(3,3),SQ(3,3) READ 15,N0A5E FORMAT(IS) D0 14 M=1,NCASE READ 1,X1,Y1,Z1,X2,Y2,22 FORMAT(6F10.0) PRINT 2 FORMAT(///,*INPUT PARAMETERS*,/) PRINT 5,X1,Y1,Z1,X2,Y2,Z2 E0RMAT(3P12.6,/,3P12.6) READ 20,A1,A2,A5 READ 20,ALPH,BET,GAM FORMAT(5F10.4) FORMAT(5F12.6) PRINT 16,A1,A2,A3 PRINT 16,ALPH,BET,GAM PI=ATANE(1.)*4. CONV=PI/180. AA=CONV*ALPH BB=CONV*BET G=CONV*GAM THETA=(GAM-90.000) T=ABSF(THETA)*CONV D=ASINF(SQRTF(COSF(AA)**2+COSF(BB)**2-2.*COSF(AA)* 1COSF(G)*COSF(BB))/SINF(G)) x2=x2*A1 X1=X1*A1 IF(THETA)21,22,22 Y1=A2*COSF(T)*Y1 Y2=A2*COSF(T)*Y2 so T0 23 Y1=(A2/COSF(T))*Y1 Y2=(A2/COSF(T))*Y2 Zl=A5*COSF(D)*Z1 z2=A3*005F(D)*z2 R2=(X2-X1)**2+(Y2-Y1)**2+(22-Z1)**2 R=SQRTF(R2* z=z2-z1 B=ACOSF(Z/R) Y=Y2-Y1 x=x2—x1 A=ATANF(Y/X) PRINT 4,A,B.R F0RMAT(3P12.6,/) PRINT 17 F0RMAT(/,*TEN50R*,/) D0 5 I=1,5 READ 6, (Q(I,J),J=1,5) 5 6 11 10 18 12 15 14 226 PRINT 6.(Q(I,J),J=1,3) FORMAT(5F10.5) 8(1,1)=COSF(A)*COSF(B) 8(1,2)=-SINF(A) s(1,3)=SINE(B)*COSF(A) S(2,1)=SINF(A)*COSF(B) S(2.2)=COSF(A) S(2,5)=SINF(A)*SINF(B) S(5,1)=-SINF(B) s(3,2)=0 s(3,3)=COSE(B) DO 7 I=1,5 DO 7 J=1,5 ST(I,J)=s(J,I) DO 8 I=1,5 D0 8 J=1,5 SUM=0 DO 9 K=1,5 SUM =SUM+5T(I,K)*Q(K,J) SQ(I,J)=SUM DO 10 I=1,5 DO 10 J=1,5 SUM=0 DO 11 K=1,5 SUM=SUM+SQ(I,K)*s(K,J) QR(I.J)=SUM PRINT 18 PORMAT(///,*R0TATED TENs0R*,/) DO 12 I=1,5 PRINT 13,(QR(I.J),J=1,3) P0RMAT(/.3P14.6,/) CONTINUE END 59 12 10 15 16 18 19 20 25 25 227 PROGRAM DIAG DIMENSION Q(5,5).V(5),VV(5),VL(5),T(5),A(5,5),VALU(5) 1,VAL(3),QQ(3.3) COMMON A.QQ.VALU,ITER,ITP DO 2 I=1,5 READ 1,(Q(I,J),J=1,5) FORMAT(5F10.0) READ 3,(V(I),I=1,3),ST,(VV(I),I=1,3) FORMAT(7F10.0) PRINT 4 FORMAT(*INPUT PARAMETERS*,//,*TRIAL.QS*,/) PRINT 5,(V(I),I=1,5),(VV(I),I=1,5) FORMAT(5F15.5) PRINT 6,ST FORMAT(/,*ST= *,F6.5,//) DO 7,I=1.5 PRINT 8,(Q(I,J),J=1,3) FORMAT(5F12.5) DO 57 K=1,10 ITER=1 ITP=0 D0 39 I=1,3 D0 59 J=1,3 QQ(I,J)=Q(I,J)*ST DO 12 I=1,5 VL(I)=V(I) DEL=0 AB=100. KTR=0 DELTA=0.1 VL(1)=VL(1)70.5*DEL VL(2)=VL(2)-0.5*DEL VL(5)=VL(5)+DEL DO 13 I=1,5 QQ(I,I)=QQ(I,I)+VL(I) CALL QDIAG KK=4 DO 16 I=1,3 T(I)=ABSF(VALU(I)) DO 17 I=1,3 KK=KK~1 IP(T(1)-T(2))18,18,19 J=2 00 T0 20 J=1 IE(T(3)-T(J))21,23,24 PRINT 25 F0RMAT(//,*MISTAKE*,//) 21 24 17 52 60 15 28 29 50 22 11 54 56 45 55 57 55 56 228 GO TO 17 VAL(KK)=VALU(J) T(J)=o. GO TO 17 VAL(KK)=VALU(3) T(5)=0. CONTINUE AA=ABSF(VAL(5))-ABSF(VV(5)) AA=ABSF(AA) IF(AA-0.001)11,11,52 DO 60 I=1,5 QQ(I,I)=QQ(I.I)-VL(I) IF(AB-AA)15,15,22 KTR=KTR+1 VL(1)=VL(1)+0.5*DEL VL(2)=VL(2)+0.5*DEL VL(3)=VL(3)-DEL DELTA=-DELTA IF(KTR-5)22,22,29 DELTA=DELTA/2. DD=ABSP