t ”:(‘3 . 23%fl004' lllllllll\lllll“Ill“Illll“Illlllwlllilillllllll 31293 00611 This is to certify that the thesis entitled LIBRARY Michigan State University -— v'wy'v Synthesis and Characterization of Ytterbium Diiodide Hydrates presented by BoYoung Kim has been accepted towards fulfillment of the requirements for M ‘ 4 degree in (”he WHH'V/ WWW Date H’é ’88 0-7 639 r professor MS U is an Affirmative Action/Equal Opportunity Institution PLACE IN RETURN BOX to remove this checkout from your record. TO AVOID FINES return on or before date due. DATE DUE DATE DUE DATE DUE MSU Is An Affirmative Action/Equal Opportunity Institution SYNTHESIS AND CHARACTERIZATION OF YTTERBIUM DIIODIDE HYDRATES BY BoYoung Kim A THESIS Submitted to Michigan State University in partial fulfillment of requirements for the degree of MASTER OF SCIENCE Department of Chemistry 1988 5079242. ABSTRACT SYNTHESIS AND CHARACTERIZATION OF YTTERBIUM DIIODIDE HYDRATBS BY BoYoung Kim The previously unreported ytterbium diiodide hydrates, YbIZ.HéO and YbI2.2H20 have been prepared. Both hydrates possess orthorhombic symmetry; Lattice parameters for YbI2.H20 and Yb12.2H20 are: a = 16.012(5) A, b = 8.140(2) A, c = 4.5079(9) A ; and a = 13.025(5) A, b = 10.455(5) A, c = 4.507(3) A, respectively. The monohydrate YbIZ.H20 was prepared by a solvent procedure, and the dihydrate YbI2.2H20 by a solid-vapor procedure. These hydrates have been characterized by powder X-ray diffraction, IR, NMR, and elemental and water analyses. The ytterbium diiodide hydrates are compared and contrasted with analogous alkaline earth and lanthanide dihalide hydrates. ACKNOWLEDGMENT I wish to thank Professor Harry A. Eick for his guidance, and support throughout this study. I appreciate advice of my guidance COImnittee, Dr. C.K. Chang, and Dr. T.J. Pinnavaia. I also gratefully" acknowledged Dr. S.A. Hodorowicz who helped in TGA-DTA measurement and in powder X—ray diffraction studies. I thank to Dr. L.D. Le for his help with the solid state NMR work. Thanks go to Dr. R.H. Schwendeman, H.H. Nam and H.R. Kim for their aid in the YbIZ.H20 FT IR work. Financial support is gratefully acknowledged from the National Science Foundation DMR 83-00739 and from the department of chemistry, Michigan State University. Finally, I appreciate my parents and my husband, Jineun, for their patience, encouragement and support. This work was partially supported by the Department of Energy Office of Basic Energy Sciences, the National Science Foundation (CHE-9816108), and the American Chemical Society Petroleum Research Fund. iii Chapter Page CHAPTER ONE: INTRODUCTION ........................... 1 A. Preparatory and Structural Background ........ 1 CHAPTER TWO: EXPERIMENTAL .......................... 12 A. _Chemicals ................................... 12 B. Synthesis Equipment ......................... 14 C. Synthesis Procedures ......................... 14 1. Anhydrous ytterbium diiodide ............ 14_ 2. Ytterbium diiodide monohydrate .......... 17 3. Ytterbium diiodide dihydrate ............ 20 D. Elemental and Water Analyses ................ 21 1. Ytterbium ............. _ .................. 21 2. Iodine .................. ................ 21 3. Water ................................... 21 E. Instruments ................................. 21 1. Powder X-ray diffraction ................ 21 2. Infrared ................................ 22 3. NMR ..................................... 22 CHAPTER THREE: RESULTS ............................. 24 A. Anhydrous Ytterbium Diiodide ................ 24 B. Ytterbium Diiodide Monohydrate .............. 26 C. Ytterbium Diiodide Dihydrate ................ 32 CHAPTER FOUR: DISCUSSION ........................... 35 A. Synthesis ................................... 35 B. Powder X-ray Diffraction .................... 39 C. Infrared .................................... 44 D. NMR ......................................... 47 E. Elemental and Water Analyses ................ 48 Future Work .......................................... 50 References ........................................... 51 TABLE OF CONTENTS iv Tables I II III IV VI VII VIII IX XI LIST OF TABLES Page Lattice parameters, space groups and colors of lanthanide trihalide hexahydrates ............... 3 Lattice parameters and symmetries of selected lanthanide dihalide hydrates ........... 8 Lattice parameters and symmetries of selected alkaline earth halide monohydrates ..... 9 Chemicals used for synthesis work .............. 13 Observed and calculated interplanar d—spacings and intensities for anhydrous YbI2 ............. 25 Observed and calculated interplanar d-spacings and observed intensities of YbIZ°H20 .......... 28 Observed and calculated interplanar d-spacings and observed intensities of YbIZ'ZHZO .......... 33 Elemental and water analysis results ............ 34 Vapor pressure of selected species .............. 36 Comparison of the structure types of some lanthanide dihalides with those of alkaline earth dihalides ................................. 43 Comparison of the IR frequencies of water with those in YbIz‘HZO .............................. 46 LIST OF FIGURES Figure Page 1 Schematic representation of anhydrous Yblz synthesis apparatus ............................ l6 2 Apparatus used for the synthesis of YbIZ'HZO ..19 3 Infrared spectrum of YbIZ'HZO ................. 30 4 NMR spectra of YbIZ°H20 at 250C -— 750C ........ 31 vi CHAPTER ONE: INTRODUCTION A. Preparatory and Structural Background Lanthanide elements form a number of hydrates which belong to diverse structure types. Some methods for the preparation of lanthanide halide hydrates have been reported in the literature and are discussed below. The chloride and bromide halide hydrates have been studied extensively. 1. Lanthanide trihalide hydrates The general preparatory procedure for hydrated lanthanide trichlorides (MCl3‘xH20; M = lanthanide) is dissolution of the lanthanide oxides in concentrated hydrochloric acid with subsequent precipitation of the hydrate upon removal of the acid. The thermal decomposition of MC13°xH20 (x = 6,7) has been investigated with Differential Thermal Analysis (DTA) by numerous workers [1-5]. Wendlandt found that the heavier lanthanide (from Eu to Lu) trichloride hexahydrates begin to lose water of hydration in a slow stream of air in the temperature range 650C to 950C [2]. He also found that as fl} the basicity of the cation decreases, igeL, as the cationic radii decrease in size, the possibility of forming intermediate hydrates increases. When the trichloride hexahydrate was heated at 360°C — 425°C in air, the metal oxidechloride, the quantity of which increased as the basicity’ of the cation decreased, was found to be the product. Ashcroft and Mortimer studied the thermal decomposition of the trichloride hydrates MC13’xH20 using a Bufferential Scanning Calorimeter (DSC) [6]. Decompositions carried out in [a nitrogen atmosphere at relatively low temperatures, around 280°C, gave the anhydrous trichloride as the final product. They found three intermediate hydrates (x = 3, 2, 1) for M = La, Ce, Pr, Nd, Eu, and Gd, and two (x = 4, 1) for M = Sm, Tb, Er, Tm, Yb, and Lu. The trichloride hexahydrate structures have been characterized by single crystal X-ray diffraction. Graeber, et al. demonstrated that MC13°6H20 phases were describable with monoclinic symmetry ,space group P2/n and two molecules in a cell [8], as shown in Table I. The structure contains the 8-coordinate complexes [MC12(OH2)6] that one third of the chlorine atoms form no bonds with metal atom. The MC13'7H20 structure was determined by Brouty and . Herpin [7]. They reported for this heptahydrate triclinic symmetry, space group P1, 2 = 2, amd a cell that contains the 9-coordinate complex [MC12(OH2)7]. Table I. Lattice parameters,space groups and colors of lanthanide hexahydrates. Compound Color Space Lattice Parameters Ref Group a(A) 9(3) g(A) B(°) Smel3°6820 Yellow PZ/n 9.67 6.55 7.96 93.67 [8] EuCl3‘6Hé0 Colorless PZ/n 9.68 6.63 7.96 93.67 [8] GdCl3’6H20 Colorless PZ/n 9.64 6.53 7.93 93.67 [8] TbCl3'6H20 Colorless P2/n 9.63 6.51 7.89 93.67 [8] DyCl3'6HZO Yellow P2/n 9.61 6.49 7.87 93.67 [8] HoCl3‘6H20 H. Y. Pz/n 9.58 6.47 7.84 93.67 [8] ErCl3’6H20 L. P. PZ/n 9.57 6.47 7.84 93.67 [8] TmCl3'6H20 Green Pz/n 9.55 6.45 7.82 93.67 [8] NdBr3'6H20 Blue P2/n 10.073 6.785 8.212 93.52 [10] GdBr3°6H20 White PZ/n 10.014 6.753 8.149 93.43 [10] TbBr3 6HZO White PZ/n 10.000 6.744 8.139 93.35 [10] DyBr3’6H20 White P2/n 9.969 6.733 8.102 93.30 [10] HoBr3’6H20 P. Y. P2/n 9.937 6.717 8.085 93.32 [10] ErBr3'6HZO Pink P2/n 9.925 6.700 8.073 93.33 [10] TmBr3‘6HZO White P2/n 9.920 6.698 8.056 93.44 [10] YbBr3 6HZO White PZ/n 9 920 6.693 8.046 93.43 [10] LuBr3 6H20 White P2/n 9.902 6.678 8.024 93.42 [10] H. Y.= Honey Yellow L. P.= Light Pink P. Y. = Pale Yellow The synthesis procedure for the lanthanide tribromide hydrates is similar to that for the trichloride hydrates. Mayer and Zolotov indicated [9] that tribromide monohydrates could be obtained as an intermediate phase during thermal decomposition of tribromide hexahydrates in air. They hypothesized that the decomposition proceeds according to the steps detailed in (l): MBr3.6H20-’>MBI3.H20-->MBr3-->MOBr-->M203 (1) M = Pr, Nd, Sm and Eu Monohydrates were not observed with the heavier lanthanide elements; the hexahydrates decomposed directly through the oxidebromide according to (2): MBr3‘6H20-->MBr3 + MOBr-->MOBr-->M203 (2) M = Gd, Tb, Dy, Ho, Er, Tm, Yb and Lu In addition, it is interesting to note that the U, Np, and Am tribromide hexahydrates were prepared as evidenced by the mass increase of the appropriate anhydrous tribromide upon exposure to oxygen-free water vapor in an inert atmosphere. The structural properties of lanthanide tribromide hexahydrates were discussed by Brown, et al. [10]. All of the tribromide hexahydrates are isostructural with the trichloride hexahydrates; they exhibit monoclinic symmetry, space group P2/n, with two molecules per unit cell. The space group, lattice parameters, and colors of these hexahydrates are summarized in Table I. Due to the intrinsic chemical instability of triiodide hydrates to undergo spontaneous decomposition to oxideiodides and HI, it is difficult to prepare the lanthanide triiodide hydrates. As a consequence they are only characterized to a limited degree. 2. Lanthanide dihalide hydrates Several lanthanide dihalide hydrates (MX2°xH20, x s Cl, Br, I) have also been reported. Their lattice parameters and symmetries are summarized in Table II. Although SmIz°H20 is reported in the table to be orthorhombic, lattice parameters could not be found. Europium dichloride dihydrate was characterized by Hasse and Brauer [11]. They’ prepared EuC12'2H20 from a solution of Eu203 in dilute hydrochloric acid by employing amalgamated zinc for reduction of Eu3+ followed by precipitation with concentrated hydrochloric acid. They found that EuC12°2H20 ”belongs to the monoclinic crystal system, space group C2/c, with z = 4 (see Table II). It is obvious that the atomic arrangement of EuC12°2H20 is nearly the same as that of SrClZ’ZHZO which has square antiprismatic coordination for the metal ions. They described that coordination shell of the Eu2+ ion as probably consisting of two hemispheres, one of four chlorine atoms and the other of four water molecules arranged to form the coordination number of 8. Haschke and Eick prepared the dihalide monohydrates, MXZ’HZO, (M = Sm, Eu; X = Br, I) for samarium and europium by vapor phase hydration of the anhydrous phase [12-14]. Powder X-ray data showed that the SmBr2°H20 phase was indexable on orthorhombic symmetry .with systematic extinctions consistent ‘with. space group ana. They“ also discovered an intermediate hydrate, EuBrZ‘HZO, when an anhydrous EuBr2 specimen hydrolyzed in a powder X-ray diffraction camera [13]. This hydrated dibromide phase-was isostructural with SrBrz’HZO (and presumably with SmBrz'HZO), and was indexable on orthorhombic symmetry, space group ana. The diiodide monohydrates, SmIz'HZO and EuIZ'HZO, have been identified [14,15]. Wang investigated the hydration of Smlz [15]. A hydrated anhydrous SmI2 specimen was obtained with water absorbed on silica gel serving as the hydrating reagent. The powder X-ray diffraction pattern showed this SmIz'HZO phase to be indexable as B-Sm12 which is orthorhomic and isomorphous with EuIZ. EuI2°H20 was obtained by hydration of anhydrous Eulz with atmospheric moisture when a specimen was not rigorously isolated from the atmosphere. This monohydrate phase showed orthorhombic symmetry and is isostructural with BaClZ’HZO, space group anm. 3. Alkaline earth halide hydrates Lattice parameters and symmetries of selected alkaline earth dihalide hydrates are summarized in Table III. Because of their similar size and like charge the divalent lanthanide halides behave similarly to the alkaline earth halides. The crystallographic data presented in Tables II and III show the presence of structural similarities between MX2.H20 (M = Sr, Ba, X = Cl, Br, I) and LnX2.H20 (Ln = 8m, Table II. Lattice parameters and symmetries of selected lanthanide dihalide hydrates EuC12.HZO Orthorhombic 10.86 8.80 4.16 [19] EuClz.ZHZO Monoclinic 11.66 6.40 6.69 105.37 [11] SmBr2.H20 Orthorhombic 11.43 9.18 4.32 [12] EuBr2.HZO Orthorhombic 11.46 9.20 4.29 [13] SmIZ.HZO Orthorhombic [15] EuIZ°HZO Orthorhombic 12.37 9.67 4.48 [14] Table III. Lattice parameters and symmetries of selected alkaline earth halide hydrates BaClz'HZO Orthorhombic 11.094 4.500 9.054 452.0 [18] BaBrz’HZO Orthorhombic 11.643 4.604 9.438 505.9 [18] BaIZ'HZO Orthorhombic 12.494 4.772 10.014 597.1 [18] SrClZ'HZO Orthorhombic 10.881 4.162 8.864 401.4 [18] SrBrZ’HZO Orthorhombic 11.464 4.295 9.229 454.4 [18] SrIZ’HZO Orthorhombic 12.474 4.495 9.741 546.2 [18] CaClZ’ZHZO Orthorhombic 5.893 7.469 12.070 531.3 [16] CaIZ'4HZO Monoclinic 6.825 7.846 9.637 110.47 509.1 [17] CaI2'6.5H20 Monoclinic 6.755 8.162 17.878 107.76 2426.8 [17] 10 4. Spectroscopic studies Infrared spectrocopy In general, lattice water exhibits vibrational frequencies at 3550 - 3200 cm-1 (antisymmetric and symmetric —OH stretching) and at 1630 - 1600 cm”1 (HOH bending). Lattice water also shows "libration modes" in the low- frequency region because of rotational oscillations of the water molecule. These rotations are restricted by interactions with neighboring atoms [23]. Lutz and Christian studied by infrared spectroscopy-the iSotypic alkaline earth halide monohydrates, MX2°H20, with M = Sr and Ba and X = Cl, Br, and I [22]. They found that the water molecules are asymmetrically bonded in the chloride and bromide hydrates and symmetrically bonded in the case of the iodide hydrates. NMR spectroscopy Nuclear magnetic resonance spectroscopy has become a useful tool for the study of the atomic arrangement and the electron charge distributions in a given specimen. It is a highly characteristic feature of NMR that spectral lines of liquids are much narrower than those of solids. This substantial difference in line broadness arises from the static anisotropic interactions present in solids. In liquid specimens these interactions are averaged by the isotropic motions of the nuclei. 11 A good example to illustrate this difference in line broadness is the 1H-NMR linewith of water and ice. The resonance line of ice has a width of the order of 105 Hz whereas that of liquid water is but a few Hz [43]. Line broadness in solids results from magnetic dipolar and Fquadrupolar interactions and from chemical shift anisotropy. Due to the restricted molecular motions present in solids, but not in liquids, the anisotropic interactions are not averaged out in time. In powdered samples these interactions give rise to NMR line broadening. To overcome this problem the Magic Angle Sample Spinning (MASS) technique was developed by Andrew, et a1. [37] in 1959. It is capable of partially suppressing the anisotropic broadening. Numerous NMR hydrate studies have been reported since Pake’s first study in 1948 of the proton resonance absorption lines of the hydrated crystal, CaSO4'2H20_ [24]; Pake determined the distance between hydrogen nuclei in the water molecules of hydration and the orientation of the line connecting the proton pair in the water molecule. The analysis of broad proton NMR absorption curve of the powder CaSO4’2H20, was also described to show that structural information about the water molecule could be obtained. I!» CHAPTER TWO: EXPERIMENTAL A. Chemicals Chemicals used in.1flua synthesis experiments described in this work are listed in Table IV. 12 Table IV. Chemicals used for syntheses Compound or Element Manufacturer —-_—_-—————nun——--_-—-——————-——-——-————.—a—-~-—---——--—--———u——— Ytterbium metal Mercury iodide Methyl alcohol Acetone Dimethyl ether Diethyl ether Calcium hydride Benzo- phenone Nitric acid Silver nitrate Ferric ammonium sulfate Ammonium thiocaynide Analytical reagent grade 99.82 Anhydrous GR Analytical reagent grade Analytical reagent grade Analytical reagent grade 952 ACS/reagent grade 99.92 Analytical reagent grade Cerfified ACS grade Research Chemicals. Phoenix, AZ Mallinckrodt St.Louis, MO EM Science Cherry Hill, NJ J.T. Baker Chemical Co Phillpsburg, NJ Matheson Mallinckrodt St.Louis, MO EM Science Cherry Hill, NJ Fisher Scientific Springfield, NJ EM Science Cherry Hill, NJ Sargent-Welch Skokie, IL Mallincrodt St.Louis, MO Fisher Scientific Springfield, NJ __-____--—___—-_________-_-__-____--_-___-_—__—_--_—---_. 14 B. Synthesis Equipment A high vacuum line which can be pumped to 10’7 - 10'5 Torr must be used for the synthesis of ytterbium diiodide monohydrate. The liquid-nitrogen-trapped vacuum line used in this work consisted of a mercury diffusion pump, a CENCO roughing pump, and an all glass manifold as described by Shriver [26]. All manipulations of reactants and products were carried out in a glove box. The argon atmosphere of this box was continuously recirculated and purged of water with molecular sieves and of oxygen with heated BASF catalyst. C. Synthesis procedures 1. Anhydrous ytterbium diiodide Metal chips were cut from a block of_ytterbium kept in the glove box. Weighed pieces of Yb chips and Hg12 in the molar ratio of 1:8 were placed in the lower bulb of a two bulb Pyrex reaction vessel. The Pyrex vessel was removed from the glove box, connected to the vacuum line, and evacuated to 10"3 Tbrr. The vessel was shaken gently to facilitate removal of trapped gases, sealed, and cut from the vacuum line at the end of second bulb with a hand torch. The sealed Pyrex vessel was situated into a tubular Fir, 15 furnace for 7 days as is shown in Figure 1 and maintained at a temperature of 365°C. When mercuric iodide was removed from the reaction bulb by sublimation, the green anhydrous ytterbium diiodide remained. The absence of water' was verified. by infrared analysis. diiodide synthes aaaaaaaaaaaa 17 2. Ytterbium diiodide monohydrate Ytterbium diiodide monohydrate was prepared in the apparatus shown in Figure 2. This H-shaped apparatus was cleaned before use in the following manner: It was first rinsed with an acid solution which contained 33% HNO3, 5% HF, and 60% H20, then filled with aqua regia and allowed to sit overnight. The aqua regia was removed and the apparatus then rinsed with distilled water several times. It was then dried in an oven. Ytterbium (diiodide monohydrate synthesis experiments were attempted with three solvents: methyl alcohol, dimethyl ether, and acetone. An elaborate purification procedure was developed for the solvent ultimately used. That procedure is described here. About 75 ml of dimethyl ether was stirred for 24 h over 0.5 g of CaH2 in a round flask situated in a dry ice bath to removelzmoisture, then. distilled under high ‘vacuum (10-5 Torr), frozen with liquid nitrogen, and evacuated. It was necessary to repeat these stir-freeze-pump cycles several times, then distill the dimethyl ether into a pre-evacuated bottle which contained Na-K alloy (1:3) and benzophenone.. When the color of the solution remained violet-blue, indicative of the absence of moisture, the ether was distilled into the H-shaped reaction vessel. A weighed amount of powdered anhydrous ytterbium l8 diiodide was placed in chamber (a) [see Figure 2] through the Fisher-Porter stopcock. The same molar amount of water was purified by freeze and thaw cycles and distilled into a 5 mm o.d. glass ampoule which was then sealed. The sealed water ampoule was also introduced into chamber (a). About 20 ml of purified dimethyl ether was then distilled into chamber (a) of the H-shaped reaction vessel which had been pre-evacuated to 10'6 Torr to dissolve the anhydrous ytterbium diiodide. The apparatus was removed from the vacuum line and kept at a temperature lower than the boiling point of dimethyl ether (~250C) in an isopropyl alcohol-dry ice bath (-40°C). The water ampoule was broken by several freeze-shake- thaw cycles. As the water reacted with the ytterbium diiodide, the color of the dimethyl ether solution changed from green to white. The solution was then filtered through the coarse frit in the H-vessel from chamber (a) into chamber (b). Finally, the white solution in chamber (b) was pumped to dryness by evacuating the H-vessel to 10"5 Torr on the high vacuum line. A bright greenish-yellow powder later demonstrated to be ytterbium diiodide monohydrate remained. Powder X-ray diffraction confirmed that the powder was a new phase. 19 Figure 2. Apparatus used for the synthesis of ytterbium diiodide monohydrate. 20 3. Ytterbium diiodide dihydrate Ytterbium diiodide dihydrate was prepared by the hydration method described by Kwapisz [27]. A weighed amount of anhydrous ytterbium diiodide situated in a pyrolytic graphite boat was placed in a Pyrex tube in the glove box. The Pyrex tube was removed from the glove box, connected to the vacuum line, and evacuated. A quantity of cupric sulfate weighed according to equation (3) to give the appropriate molar ratio of water was inserted into a silica boat. 5Yb12(s)+ 2[CuSO4‘5H20](s) —-> 5[Yb12°2H20](s) +2CuSO4(s) (3) The tube was filled with argon, and as the gas flowed through the Pyrex tube, the silica boat was introduced. The tube was then evacuated to 10"3 Torr. During the hot weather in summer, the hydration reaction was conducted in a refrigerator (4°C) over a period of 2 weeks. As time passed, the color of the anhydrous ytterbium diiodide changed from green to [dark green. The change of mass of each. reagent indicated that anhydrous ytterbium diiodide was hydrated by the cupric sulfate, and that ytterbium diiodide dihydrate was produced. X-ray powder diffraction confirmed that the product was identical to that prepared by Kwapisz. 21 C. Analysis 1. Ytterbium Ytterbium metal content was determined by gravimetric procedures. A 6N HNO3 solution was added to the sample confined in a platinum crucible to remove iodine, direct ignition at 950°C produced the sesquioxide. 2. Iodine The product was analyzed for iodine by' the Volhald method [28] in acid medium. In this process an excess of standard silver nitrate was added to the solution and. the excess Ag+ was back-titrated with a standard potassium thiocyanate solution. A 40% ferricammonium sulfate solution served as indicator. 3. Water Water analyses was conducted by Galbraith Laboratories, Inc., by the Karl Fisher water analysis method. 22 D. Instruments 1. Powder X-ray Diffraction The hydrated products were characterized by powder X- ray diffraction analysis. Interplanar d-spacings were determined with an evacuated Guinier camera (114.6 mm diameter) by' using CuKal .radiation Lt a1 = 1.54050 A). Silicon powder (a = 5.43082(3) A) was employed as an internal standard. Paraffin oil and ScotchR tape served to protect the silicon-sample inixture from further reaction with moisture. For the anhydrous ytterbium diiodide specimens, powder X-ray diffraction was carried out with the sample confined in 0.3 mm o.d. sealed Lindemann glass capillaries. 2. Infrared IR spectra were recorded with a BOMEM model DA3 Fourier-transform infrared spectrometer between 4000 cm"1 and 800 cm'1 at 3 cm'1 resolution. The sample which was mixed with nujol and pressed between NaCl plates was maintained under vacuum during analysis. 3. NMR NMR spectra were measured with the powdered sample in a sealed 5 mm o.d. NMR tube at 250 MHz on a Bruker WM-250 23 Spectrometer. The 16 step phase-cycled spin-echo [29] NMR procedure was used for removal of base line distortion due to ringing of the transmitter/probe circuits and dead time of the receiver. Two 90 degree pulses (P1 = 9.5 and P2 = 9.5 microsec), two delay times (D1 = 50 and D2 = 44 microsec) and recycle times (10 microsec) were used. Temperatures at which the measurements were taken varied in the range of 250C and 75°C . CHAPTER THREE: RESULTS A. Anhydrous ytterbium diiodide The powder X—ray diffraction pattern of the anhydrous YbIZ prepared by reaction with excess HgI2 with Yb showed about 20 reflections which could be ascribed to a hexagonal cell with a = 4.504(3) A and c = 6.970(5) A. Interplanar d-spacings and intensity values ' for anhydrous YbIz prepared' in this study together' with the values calculated by the program POWD12 [35] with the positional and thermal parameters reported for Cd12 by Wyckoff [30] are given in Table V. 24 25 Table V. Observed and calculated interplanar d-spacings and intensities of anhydrous YbI2 h k l Iobs Icalc dobs(A) dcalc(A) 0 0 1 M 31.8 6.53 6.972 1 0 0 VW 1.9 4.037 3.900 0 O 2 VW 1.4 3.476 3.486 1 0 1 VS 100.0 3.343 A 3.404 1 0 2 S 59.0 2.597 2.599 1 l 0 M 40.0 2.228 2.252 1 1 1 W 12.1 2.138 2.143 1 0 3 w 24.2 1.997 1.996 2 0 1 W 20.2 1.878 1.877 2 0 2 VW 8.9 1.703 1.702 2 1 1 W 18.8 1.444 1.442 1 1 4 VW 18.2 1.379 1.378 3 0 0 W .7.5 1.301 1.300 2 0 4 VW 0.1 1.301 1.299 2 1 3 VW 0.1 1.247 1.245 2 2 0 VW 4.7 1.127 1.126 1 0 6 VW 2.3 1.110 1.114 2 2 1 VW 2.3 1.110 1.114 2 2 2 w 1.069 1.111 3 1 l W 1.069 1.111 * VS,very strong;$,strong;M,medium;w;weak; VW,very weak. 26 B. Ytterbium diiodide monohydrate It was indicated previously (Chapter two,sec 2.) that several synthesis attempts were made with methyl alcohol, acetone, and dimethyl ether. The results obtained with each solvent are presented here. The green Yblz powder produced bubbles when it contacted the water-methanol solvent. As it reacted gas evolution persisted and a green solution resulted. When diethyl ether was added to the methyl alcohol solvent to precipitate Yb12°H20, a yellow precipitate formed; its color changed to white. When acetone was used as solvent, the Yb12 dissolved readily at room temperature to form a dark violet solution. The Violet color probably results from ionization of the iodide ion in the acetone solution and its subsequent complexation with acetone. When the acetone was removed under vacuum by heating about 20 minutes with a heat gun, the green powder appeared again. By powder X-ray diffraction it was verified that the green powder was anhydrous YbIZ. In other experiments with the YbIZ-acetone solution the acetone solvent was removed slowly by inserting into liquid nitrogen the end of the chamber of the H-shaped vessel that did not contain the specimen. AS the acetone was removed slowly, the violet color disappeared and the yellow powder again formed. Prof. Dr. Hodorowicz determined the water of hydration by DTA-TGA and demonstrated that the yellow powder 27 was YbIZ'IOHZO. This DTA-TGA result shows that it is possible to form higher hydrates of divalent ytterbium iodide. The powder X-ray pattern of YbIZ'HZO was characteristic of an orthorhombic cell with the lattice parameters; a = 16.012(5) A, b = 8.140(2) A, and c:== 4.5080(9) A. The interplanar d-spacings were indexed and the parameters refined by the programs ITO9 [33] or TREOR [34]. In Table VI the observed interplanar d—spacings and correspOnding intensities and the calculated d-spacings of YbIZ‘HZO are presented. Every reflection is indexed and the figure-of- merit is 29.0 [46]. Extinctions are consistent with space 28 Table VI. Observed and calculated interplanar d-spacings and observed intensities of YbI2.H20 o o h k l Iobs dcalc(A) dexp(A) 2 0 0 VS 8.006 8.018 1 1 0 VS 7.256 7.247 2 1 0 M 5.708 5.722 3 1 0 W 4.463 4.474 0 2 0 VW 4.070 4.080 4 0 0 VW 4.003 4.007 0 1 1 VW 3.945 3.944 1 1 1 W 3.829 3.833 4 1 0 M 3.592 3.594 2 1 1 VS , 3.537 3.535 3 2 0 W 3.236 3.238 3 1 1 W 3.172 3.173 O 2 1 S 3.021 3.021 4 O 1 8 2.993 2.993 1 2 1 VW 2.969 2.971 4 2 0 8 2.854 2.855 2 2 1 S 2.826 - 2.826 4 1 1 M 2.809 2.809 1 3 0 VW 2.675 2.675 3 2 l W 2.629 2.631 29 The infrared spectrum of YbI2°H20 was recorded to help characterize the environment of the water molecule.inIZ°H20 exhibits the infrared spectrum shown in Figure 3. The principal features of this infrared spectrum are the bands between 1600 cm"1 and 3600 ‘ cm‘l. Figure 3 shows bands at 3430 cm"1 and 1610 cm'1 which result from the O-H asymmetric stretching and HOH bending modes of the water molecule, respectively. Solid-state powder static proton NMR spectra of YbIZ'HZO are shown in Figure 4. Spectra from 25°C and 750C are compared, and the effects of temperature on -the appearance of the NMR spectra are illustrated in Figure 4. The results of the elemental and water analyses are tabulated in Table VIII. 30 .ON:.NHQW wo Esuuowmm cmHMHHGH .m Guzman 7.2 u 8.2. ooeu comm oooe P — . 00m F BONVIIIWSNVHI 31 Figure 4. NMR spectra of Yb12.H20 at 25°C -- 75°C. 75°C 32 C. Ytterbium diiodide dihydrate Several attempts were made in summer months to prepare YbIz'ZHZO with CuSO4'5H20 as the hydrating agents in anticipationthat Yb12°2H20 would be the product. However, anhydrous YbIz formed a different hydrate at room temperature in the Pyrex reaction vessel. When the reaction was carried out for tWo weeks in the refrigerator (4°C) in summer, the YbIz surface became dark green, but a yellow- colored solid had formed beneath it. X-ray powder diffraction showed the surface to be YbIZ’ZHZO, with other unidentified compounds present in the lower part of the product. This inhomogeneous product apparently results from the differential absorption of water by the anhydrous YbIz. As might be expected, YbIZ'ZHZO was produced on the surface with a lower hydrate beneath the surface. According to the program ITO9 [33] the d-spacings of this dark-green colored hydrate are indexable on orthorhombic symmetry with a figure-of-merit of 22.9. The observed and calculated d-spacings and the observed intensity data for Yb12°2H20 are presented in Table VII. The lattice parameters were refined by program APPLEMAN [36]: a = 13.024(5) A, b = 10.455(5) A, and c = 4.507(3) A. Metal and iodine analysis data of ‘the dihydrate are: presented in Table VIII. 33 Table VII. Observed and calculated interplanar d-spacings and observed intensities of Yb12.2H20 h k l Iobs dca1c(z) dobs(X) 1 1 o 5 8.153 8 160 2 o 0 5 6.512 6.496 0 2 0 VW 5.228 5.228 1 2 o 5 4.851 4.846 2 2 o 5 4.077 4.075 3 l 0 vw 4.010 4.010 1 1 1 VW '3.945 3.948 0 3 0 vs 3.485 3.488 0 2 1 W 3.414 3.413 3 2 0 M 3.340 3.347 1 2 1 M 3.302 3.299 4 o 0 VW 3.256 3.255 2 2 1 vs ‘ 3.023 3.022 3 1 1 W 2.996 2.997 4 2 0 VW 2.764 2.766 3 3 0 5 2.718 2.718 1 3 1 vw 2.697 2.699 3 2 1 5 2.684 2.683 4 3 0 VW 2.397 2.383 4 2 1 VW 2.359 2.359 34 Table VIII. Elemental and water analysis results compound Yb(Z) 1(2) water(1) YbI2°H20 cal. 38.90 57.05 4.05 exp. 38.95(4) 58.85(7) 4.05(29) YbIZ°2H20 cal. 37.38 54.83 7.78 exp. 38.33(3) 53.90(8) CHAPTER FOUR: DISCUSSION A. Synthesis Anhydrous ytterbium diiodide Anhydrous Yblz was prepared by chemical reaction (4) in an excess of HgIZ. Yb(s) + HgIZ(l)-—-> YbIZ(s) + Hg(l) (4) Hg212 was also a probable product. No effort was made to separate the Hg from either the excess of HgI2 or from Hg212 that may have formed. The vapor pressure data of each reaction component as shown in Table IX substantiate that HgIZ should be separable quantitatively by sublimation from YbIZ. Oxidation of ytterbium by Hglz took place easily: ytterbium metal is a powerful reducing agent, (Yb+3 + 3e" ———> Yb, E0 = -2.27 v ) (Yb+3 + e‘ ———> Yb+2, E0 = -1.21 V) This large reduction potential coupled with the large vapor pressure difference between Hg and HgI2 and YbI2 assured quantative reduction [47] 35 36 Table IX. Vapor pressure of selected compounds at various temperatures Compound Vapor Pressure Temp Ref CaSOA'ZHZO 0.005 mg/l 25°C [41] Cuso4 1.4 mg/l 25°C [41] ngz 100 Torr 262°C [41] Hg 100 .Torr 262°C [41) YbI2 1.9xlo‘16 Torr 260°C [47] 2 Torr 790°C 37 Ytterbium diiodide monohydrate Although, methyl alcohol, ethyl alcohol, acetone, dimethyl ether, and diethyl ether were considered as solvents for the synthesis reaction, dimethyl ether proved to be the solvent of choice. Methyl alcohol whose boiling point is 64.50C was chosen initially for the preparation. It was thought that this solvent could be removed easily and that it would not react with YbIZ. However, with dimethyl ether as solvent significantly more pure YbIz°H20 could be prepared than was obtained with either methyl alcohol or acetone. Accordingly, this solvent has proved to be the best found to date for the preparation of YbIZ'HZO. The fact that dimethyl ether must be kept at a temperature below its boiling point, -25°C, somewhat complicates the synthesis procedure. From the IR spectrum it is clear that dimethyl ether did not form complex with YbIz. Some of the problems encountered in this YbIz’HZO synthesis procedure are decomposition of the solutions during synthesis because of impurities not removed or leakage in the high vacuum system, air sensitivity of the components, the length of time required for the synthesis procedure, and purification of the solvent. However this method also has some advantages. The exceedingly high'vapor pressure of dimethyl ether allows' very easy solvent removal and its low dielectric constant tends to increase the YbI2°H20 yield. 38 Ytterbium diiodide dihydrate This preparation was attempted first via a sodid-vapor procedure in a Pyrex reaction vessel by Kwapisz [27]. He prepared a ytterbium diiodide hydrate specimen which he thought was the monohydrate, but which was later demonstrated to be the dihydrate, YbI2°2H20. Some of the problems encountered in this synthesis procedure ‘were selection. of a suitable hydrating agent, variable reaction time with respect to the environment, low thermodynamic stability of the product, and production of an inhomogeneous layered product. Kwapisz prepared YbI2'2H20 according to equation (5). 5Yb12(8) + 2[CUSO4.5H20](S) --> 5[Yb12.2H20](S) + 2CUSO4(S) (5) He found that with CuSO4°5H20 as a hydrating agent one or two water molecules could readily be donated for this Yb12°2H20 synthesis. CaSO4°2H20 *was initially’ used. as a hydrating agent by Kwapisz, but with it the YbIZ did not evidence any hydration whatsoever. Since the residual. H20 vapor in dried air for CaSO4 is 0.005 mg/liter and that for anhydrous CuSO4 is 1.4 mg/liter [41], the absence cf hydration with CaSO4°2H20 is readily understandable. The partial pressure of H20 in the reaction environment must be controlled. carefully' to avoid production of higher ‘YbIz hydratesprior to completion of the desired hydration 39 reaction. Several generalizations of YbIz'ZHZO synthesis experiments made by the solid - vapor method indicate the following: First, the formation of YbIZ'ZHZO was complete within 7 days at room temperature. Since the H20 tensimetric pressure of the hydrating agent is greater in summer than in winter, the hydration reaction proceeds more rapidly in summer than in winter. Second, the vapor pressure of water required for hydration must either equal or be slightly less than that of CuSO4'5H20 since hydration can be achieved. Third, YbI2'2H20 must possess greater thermodynamic stability than does the monohydrate since monohydrate was never observed in a product prepared by this procedure. However, this dihydrate may be metastable toward either further hydration or hemihydration. B. Powder X-ray diffraction Anhydrous ytterbium diiodide The standard deviations of the parameters derived from the observed reflections by localLy written programs were very small, typically less than t 0.005 A an indication that the parameters are well determined. This good fit is considered evidence that YbIZ exhibits the hexagonal symmetry CdIZ-type structure. The CdIZ—type structure is the 40 only reported structural form for YbIZ. This structure consists of a layer-like atomic arrangement and exhibits in its physical properties the characteristics of layered compounds [38]. The CdIZ layered structure in the crystal can be viewed as hexagonal close-packing of iodine ions with the small cadmium ions nested in the octahedral holes between every two layers of iodine ions. To maintain stoichiometry half of the octahedral holes must be vacant. These vacancies result in the two adjacent layers of iodine atoms being held together by van der Waal’s forces. According to Asprey and Kruse [38] Yblz does not exibit the polytypism so characteristic of the CdIZ-type structure. With the atomic positibnal and thermal parameters reported by Asprey and Kruse, the reflection intensities could be calculated. by' the jprogram. POWD12. The agreement. between calculated and observed intensities for YbIz as shown in Table V substantiates that the metal ions occupy'the 1a positions and the iodide ions the 2d positions in the space group. Ytterbium diiodide monohydrate The symmetry of YbIZ‘H2O is the same as those of SrClZ'HZO, MBrz'HZO (M = Sm, Eu,and Sr), and EuIZ'HZO. The lattice parameters observed for the YbI2.H20 are: Q can be as big as by a factor of approximately 1.5 of the above related divalent halide monohydrates, and p and Q are 41 consistent with those reported previously for the divalent halide monohydrates, as is illustrated in Table II and Table III. The YbIZ'HZO unit cell volume of 587.63 A3 can be regarded as the summation of the volume of anhydrous YbIZ, 61.2 A3, and that of H20, 36.74 A3, derived from the structure of solid water [30]. This summation would imply that the cell contains six YbIZ'HZO moieties, or that z = 6. It was thought initially that EuIZ.H20 structure (z=4) expected to be the structure type for Yb12.H20 with Yb atom substituted for Eu atom. The lattice parameter a which is calculated from the hypothetical cell containing six Eu12.H20 moieties is 18.05 A. The EuBr2.H20 structure (2 = 4) was also considered. The lattice parameter a, 17.19 A, is calculated from the hypothetical large cell containing six EuBr2.H20 moieties. On the basis of these above calculations it is clear that the calculated lattice parameter a, 17.19 A, from the EuBr2.H20 structure is closer to the lattice parameter a, 16.012 A, of the observed present investigation, Yb12.H20. Thus it is suggested that the best struCturral model for the Yb12.H20 would entail, probably, EuBr2.H20 ‘with. positional coordinates transformed. t0"the large cell. Numerous attempts were made to calculate a theoretical powder pattern for YbIZ‘Hzo by using positional parameters of related hydrates which have the same space group, P212121, and reasonably similar values Of z, with estimated 42 thermal parameters. For example, CeOSO4'H20 and TiOSO4°H20 were used as model structures. For these calculations the ytterbium atom was situated in the cation site, one X occupied the O atom site, and the second X occupied the S atom site. The water molecule occupied its established position. Lattice parameters for YbIZ'HZO were used for the calculation. run“; of the theoretical intensities matched the observed pattern. ' The CRYSTDAT data base was also searched for an appropriate structural model for YbIQ'HZO; this search was not fruitful [42]. As was discussed. earlier (Chapter one, sec 3) _the lanthanide(II) and the alkaline earth halides form similar hydrates. Since the radius of Ca2+ with coordination number 8 is 1.26 A and that of Yb2+ 1.28 A [32], there should be structual similarities between CaXz and Lnxz (Ln = Yb and adjacent elements, Tm and Lu; X= Cl, Br, I). Thus, their halide hydrates would be expected to Show some similar structure types as is evident in Table X. 43 Comparison of the structure types of some lanthanide dihalide with those of alkaline earth halides Table X. M\X Cl Sm PbClZ(9)a CaF2(8) Eu PbC12(9) CaF2(8) Tm SrIZ(7) Yb SrIZ(7) Ba PbClZ(9) Fe2P(9) CaF2(8) Sr PbC12(9) CaF2(8) Ca SrI (7) CaC 2(6) a-Pb02(6) a PbC12(9) SrBr2(8) SrBr2(8) PbC12(9) SrIZ(7) CaC12(6) CaC12(6) PbC12(9) PbC12(9) ,SrBr2(8) CaC12(6) a-Pb02(6) Ti02(6) a-Pb02(6) T102(6) _ a m EuI2(7) PbC12(7) m-EuIZ(7) PbC12(9) Sr12(7) CdI2(6) CdIz(6) .PbC12(9) FeZP(9) PbClZ(9) SrI2(7) CdI2(6) [39] [39] [39] [39] 44 Ytterbium diiodide dihydrate The symmetry of YbIZ'ZHZO, orthorhombic by the program ITO9, is the same as those of SrClz‘HZO, MBrZ'HZO (M:= Sm, Eu, Sr). The unit cell volume of 613.81 A3 can be regarded as the summation of the volume of YbIZ, 61.2 A3, derived from the unit cell volume of anhydrous YbIZ, and that of H20, 35.8 A3, derived from the structure of solid water. When these volumes are compared to that of the dihydrate, it is apparent that the unit cell contains four Yb12°2H20 moieties, or that z = 4. Several attempts were made to calculate theoretical X- ray powder diffraction patterns of YbI2'2H20 by using positional and thermal parameters of related hydrates which have the same space group, anm. None of the theoretical intensities matched the observed pattern. The CRYSTDAT data base was also searched for an appropriate structural model for YbI2'2H20; this search was not successful. C. Infrared spectra YbI2°H20 exhibited the infrared spectra shown in Figure 3. The O-H stretching frequency of the water observed at 3325 cm"1 is shifted to a lower wavenumber than that of free water because the rigidity of the crystalline lattice constrains the H20 molecule. This observation suggests that the hydroxy group is probably weakly hydrogen-bonded to the anion. However, if only weak hydrogen-anion bonds are 45 present, the shifting of the O-H stretching modes is more influenced by the nature of the metal ions than by the strength of hydrogen bridges [22]. In general, lattice water molecules are trapped in the crystalline lattice either by weak hydrogen-bonds to anions or by weak ionic bonds to the metal ions. On the basis of literature data, the structures of the iodide monohydrates are more symmetric with respect to the H-bonds than those of the tmomide and chloride monohydrates. This behavior was predicted previously [22]. For example, iodide monohydrates possess C2V symmetry, whereas bromide and chloride monohydrates do not. From the appearance of two uncoupled O—H stretching modes, the water molecules in the latter two monohydrates are unsymmetrically bonded, with a symmetry lower than sz. These modes are also shifted to lower wavenumbers because the rigidity of the crystalline lattice constrains the H20 molecule. 46 Table XI. Comparison of IR absorption frequency of water with that in YbIZ'HZO. Free H20(cm—l) Crystal H20(cm_l) Assignment 3430 . 3435 ”asym stretch 3325 3330 ”sym stretch 1610 1620 47 D. NMR In this work the available MASS-NMR instrument could not be used because of a malfunctioning contact and its relatively slow spinning speed (2-5 kHz). In order to achieve line narrowing of very wide homogeneous proton NMR lines, a very high spinning speed (about 20 kHz) is required. Also, if the line shape is Gaussian, the static NMR line width is directly related to the second moment, M, according 'to the Van Vleck equation (6): 2 (6) M = 0.180 ( Av1/2 ) where 1301/2 is full width at half-height [44]. Therefore, the STATIC NMR technique had to be utilzed. The line width and the second moment can be used to characterize tflue broad featureless absorptions obtained in solid-state proton NMR studies. The second moment, M, of nuclear spin, I, is the sum of M(hetero) and M(homo) as follows: M(hetero) = (l/3)yzzyg2f125(s+1)'i[(1-3COSZQfi)2/I_fi:] (7) J, '6 Jo M(homo) = (3/4)714I12I(I+1) .Efi[(1-3COSZ0;*)2/r:] (8) 4 . 4 where I and S are nuclear spins, y is the magnetogyric ratio of spin I or S, 0 is the angle between the field direction and the internuclear vector, r, and h is h/2n (h = Plank's 48 constant). Any rapid molecular motion will tend to partially average the dipolar interactions (i.e., the angular parts of the above equations), so that the second moment will appear to be decreased below its rigid lattice value. spin-spin relaxation time (T2) will then increase. In particular, at the melting point or above the onset of molecular motion,thesecond moment drops to a relatively small value. The hydrate spectra shown in figure 5 are markedly temperature - dependent. There is a large decrease in the second moment parameters at 750C, an indication that water molecular? motion. is ‘taking’ place» As the temperature_ is raised from 250C, hindered rotational and vibrational motion of water molecules increases and free rotational motion of water probably occurs between 650C and 750C. E. Elemental and water analysis Ytterbium diiodide monohydrate The standard deviation of duplicate Karl Fisher water analyses of YbIZ’Hzo indicated that the average water content. agreed well with the theoretical value. Elemental ytterbium and iodide analyses agreed with the expected formula, YbIZ‘HZO. Ytterbium diiodide dihydrate Metal and iodine analyses indicate that the ytterbium 49 and iodine content exhibit good agreement with values calculated for a dihydrate. However, water analysis by the Karl Fisher method was inconsistent with that expected for a dihydrate product. It is presumed that the product became hydrated further either during analysis or transfer. SUGGESTIONS FOR FUTURE WORK The single crystal of YbIZ°H20 should be prepared by the solvent procedure for a better understanding of the properties of hydrates by single crystal X—ray diffraction procedures. It is necessary that high quality crystal be used, therefore the crystallization techniques must be improved. A thermal decomposition study of YbIz'HZO by TGA-DTA is needed for qualitative identification. TGA-DTA has become a useful analytical tool that enables one to determine phase transitions of hydrates. Solid-state NMR studies of YbIZ'HZO should be achieved by the Magic Angle Spinning technique to obtain structural information. The YbI2'2H20, which was prepared by only the solid- vapor procedure, might be synthesized by the solvent procedure. By varing the water stoichiometry, various other hydration numbers might be determined and a phase diagram constructed. 50 10. 11. 12. 13. 14. 15. 16. REFERENCES W. W. Wendlandt, J. Inorq. Nucl. Chem. 5, 118 (1957). W. W. Wendlandt, J. Inorq. Nucl. Chem. 9, 136 (1959). W. W. Wendlandt, Anal. Chem. Acta 21, 439 (1959). J. E. Powell and H. R. Burkholder, J. Inorq. Nucl. Chem. 14, 65 (1960). V. K. Il'in, V. A. Krenev, and V. I. Evdokimov, Russ. J. Inorq.Chem. 10, 17 (1972). J. S. Ashcroft and C. T. Mortimer, J. Less—Common Met. 14, 403 (1968). C. Brouty and P. Herpin, C. R. Acad. Sci., Paris, Ser. C. 272, 2079 (1972). ‘ E. J. Graeber, G. H. Conrad, and S. F. Duliere, Acta Cryst. 21, 1012 (1966). I. Mayer and S. Zolotov, J. Inorq. Nucl. Chem. 27, 1905 (1965). D. Brown,S. Fletcher, and D. G. Holah, J. Chem. Soc. (A),l889 (1968). A. Hasse and G. Brauer, Acta Crystallogr. 331, 290 (1975). J. M. Haschke, Inorg. Chem. 15, 298 (1976). J. M. Haschke and H. A. Eick, J. Inorq, Nucl. Chem. 32, 2153 (1970). J. M. Haschke, Inorqg Chem. 15, 508 (1976). S. H. Wang, unpublished results. P. A. Leclaire and M. M. Borel, Acta Crystalloqr. BB3, 1608 (1977). 51 17. 18. 19. 20. 21. 22. 23. 24. 25. 26. 27. 28. 29. 30. 31. 32. 33. 34. 52 G. Thiele and D. Puzas, Z. anorq. allq. Chem. 519, 217 (1984). H. D. Lutz, W. Buchmier, and B. Engelen, Acta Crystallogr. B43, 71 (1987). A. Hasse and G. Brauer, Z. anorq. allq. Chem. 450, 36 (1979). B. Engelen, C. Freiburg, and H. D. Lutz, Z. anorq. allg. Chem. 497, 151 (1983). H. D. Lutz, W. Becker, Ch. Mertins, and B. Engelen, Z; anorq. allq.Chem. 457, 84 (1979). H. D. Lutz and Hi. Christian, J. Mol. Struc. 96, 61 (1982). ‘ K. Ichida, Y. Kuroda, D. Nakamura, and M. Kubo, Spectrochimica Acta 28A, 2433 (1972). G. E. Pake, J. Chem. Phys. 16, 327 (1948). S. Yano, J. Phy. Soc. Japan 14, 942 (1959). D. F. Shriver, "The Manipulation of Air-Sensitive Compounds", p.4, McGraw-Hill, New York, (1969). ,R° Kwapisz, unpublished research results, (1986). I. M. Kolthoff, E. B. Sand28. I. M. Kolthoff, E. B. Sandell, E. J. Meehan, and S.Bruckenstein, "Quantitative Chemical Analysis" 4th ed., p. 724, Macmillan, New York, (1969). A. C. Kunwar, G. L. Turner, and E. Oldfield, J. Maqn. Reson. 69, 124 (1986). R. W.'G. Wyckoff, "Crystal Structures", Vol. 1, 2nd Ed., p. 322 Wiley, New York (1965). H. Lipson and. H. Steeple, "Interpretation of X—ray Powder Diffraction. Patterns", p. 79, .Macmillan, New York, (1970). R. D. Shannon, Acta Crystallogr. A32, 751 (1976).. J. Visser, J. Appl. Crystalloqr. 2, 89 (1969). L. Erikson and M. Westdahl, J. Appl. Crystalloqr. 18, 367 (1985). 35. 36. 37. 38. 39. 40. 41. 42. 43. 44. 45. 46. 47. '53 D. K. Smith, M. C. Nichqls,) and M. E. Zolensky, "A FORTRAN IV Program for Calculating X-ray powder Diffraction Patterns-Version 10. " The Pensylvania State University, University park, PA (1983). D. E. Appleman, D. S. ’Handwerker, and. HuT. Evans, "Program X-ray." Geological Survey, U. S. Department of Interior, Washington, D. C. (1966). ’ E. R. Andrew, A. Bradbury, and R. G. Eades, Nature 183, 1802 (1959). , . L. B. Asprey and F. H. Kruse, J. Inorq. Nucl. Chem. 13, 32 (1960). - M. Eitel, Ph. D. Dissertation, University of Karlsruhe (1985). ’ 4 ' . "International Tables for X-ray Crystallography," Vol. 4, J. A. Ibers and W. C. Hamilton, Eds., Kynoch press, Birmingham, England (1974).» "Handbook of Chemistry and Physics," 43rd Edition, C. D. Hodgman, R. C. West, and S. M. Selby, Eds., The Chemical Rubber Publishing Co., Cleveland (1961). CRYSTDAT, Canada Institute for Scientific and Technical Information, National Research Council of Canada, Ottawa Canada KIA 052 (1987). E. R. Endrew, Phil. Trans. (London) A299, 505 (1981). J. H. Van Vleck, Phys. Rev. 74, 1168 (1948). C. P. Slichier, "Principles of Magnetic Resonance," p. 70, 2nd. Ed. Springer-Verlag, New York (1978). P. W. DeWolff, J. Appl. Crystalloqr. l, 108 (1968). C. A. Voos-Esquivel, M. S. Thesis, Michigan State University, 1986. -. l.. .. ... 2. . . .. ...\. n... 51.215.930.41) 1:41. SH. . NIV. LIBRQR ES Hill I ll 1 . [” "1.1111111 61 7836