SPECIFIC HEAT STUDIES OF MN(C2H3OZ)24HZO AND FEBIZ 4H20 IN THE LIQUID HELIUM TEMPERATURE REGION The“: for Hm Degree of M. S. MECHIGAN STATE UNEVERSETY Sister M. Charles Joseph Zinn. O. P. 1962 m IIIIII II IIII IIIIIIIII III ' 312993 01743 0152 M LIBRARY LI Michigan State " Univcrfiity r mayor:- in I 3122.19 Innahv i5 :97 5’3 s‘c. 3'“; tr ABSTRACT SPECIFIC HEAT STUDIES OF Mn(C2H302)2-HH20 AND FeBr2~HH20 IN THE LIQUID HELIUM TEMPERATURE REGION by Sister M. Charles Joseph Zinn, O.P. In this investigation the heat capacity of single crystals of ferrous bromide and manganous acetate were studied in the helium temperature range. Basically the method used was to cool the sample to the desired temperature region in a conventional double Dewar system, isolate it, and then put measured amounts of heat into the crystal while observing the corresponding temperature rise. A small carbon resistor embedded in the crystal served as a thermometer and a fine wire coil wrapped around it provided a mechanism for heating. At these low temperatures (l°—H.5° K) the lattice heat capacity, which varies as T3, is negligibly small and therefore anomalies due to magnetic ordering processes and other effects are observable. A-type anomalies in the heat capacity curves were observed at 1.28 L 0.02°K in the case of ferrous bromide and at 3.17 ; 0.02°K for manganous acetate. The latter is be- lieved to be the Curie temperature for a paramagnetic- ferromagnetic transition. The magnetic entropies associated Sister M. Charles Joseph Zinn, O.P. with these transitions are 2.6m cal/moleodeg and 1.61 cal/ mole-deg respectively. The first is in fair agreement with the theoretical value, 3.19 cal/moleodeg, if the Spin of the magnetic ion (Fett) is taken as 2 in R 1n(28+l). In the case of manganous acetate, however, one finds disagreement by more than a factor of 2 between the entrOpy calculated from measured values and that obtained from R 1n(28+l). These are 1.61 and 3.58 cal/moleodeg respectively. SPECIFIC HEAT STUDIES ‘HH 0 2 2 2 IN THE LIQUID HELIUM TEMPERATURE REGION OF Mn>e, CV -—~ 3R. This is the classical value which agrees with eXperiment. However, as T —+ 0, Cv -+ O exponentially, which is not observed experimentally. Nernst modified Einstein's expression by postulating two frequencies, u>and % in order to obtain better agreement with observations. But he was not able to find any theoreti- cal basis for his choice of the two frequencies. Debye extended Einstein's theory by replacing the single frequency with a frequency spectrum. [2] In place of many independently vibrating atoms, Debye adOpted for his model a continuous medium capable of supporting a set of elastic standing waves. The frequencies of these waves range up to a maximumcgm corresponding to a wave length of the 5 order of the interatomic distances. We will first apply this simplification to the case of a one-dimensional crystal and then extend the method to three dimensions. The internal energy of the one-dimensional crystal may be expressed from quantum theory as, -2 ““k u - km (s) e kT - 1 where the summation is over all normal modes of vibration. A quantized lattice vibration is commonly referred to as a phonon. For a large number of oscillators we replace this sum by an integral, I103 - where w(k)dk is the number of modes between k and k + dk. For a one-dimensional line of oscillators there is one mode for each interval Ak = E where L is the length of the line. L Therefore, w Debye used the continuum approximation, us: vok, which is valid for a homogeneous line. In this approximation 31:; is simply %—, the reciprocal for wave velocity. Therefore, 0 L c0m _ m k U ‘ "TVOJ‘O ehm/kT _ l d“ (9) 6 The fact that the line is actually composed of discrete oscillators is brought into the theory in order to limit the number of modes and thereby the range of frequencies. In actual substances the order of magnitude of the limit on k islkm|='§:3108 cm‘l where a is the lattice constant. [3] In order to determine the w(k) for the three- dimensional case we apply the method of periodic boundary conditions, requiring periodicity of the vibrational wave at the boundaries of a cube of side L. Then ka’ k L, and Y kzL must be multiples of 2fl‘so that a cubic lattice may be constructed of lattice constant fiflzin which the points re- present the allowed values of k. The number of states with wave number less than Ikl is represented by the volume of a 3 sphere of radius Ikl, measured in units of %E i.e.,(ufljfl: . 2 L 3k2 2112 The appearance of the factor 3 is due to the exis- Therefore, for one unit volume, w(k) = tence of two transverse and one longitudinal modes of vibra- tion in an isotrOpic medium. Therefore, we may write the internal energy per unit volume as, km 2 : -———AL— «gunk—I— U f0 ehw/kT .. 1 2W2 dk (10) or using the Debye or continuum approximation, a): vok, O u : ____3h m_______w3dw (11) 2W2V03 0 ehQ/kT _ 1 Since the total number of modes must equal 3N, where N is the number of atoms per unit volume, we may determine the upper limits of km andcum, 3 m = 3N (12 211 7? |\.) Rewriting Equation (11) and letting x =‘%%’ 318%” med z MI “Ji— <13) ---- - -- (611’2N)l/3= $- (11+) This equation defines the Debye characteristic temperature 9. Differentiating with respect to temperature we obtain the heat capacity, XIII c = 9Nk(I)3 955145-—- (15) V 9 0 (ex- 1)2 At T>>9 this eXpression approaches the classical Dulong and Petit value quite well. At very low temperatures, the upper limit in the above integral approaches infinity and we have, x3ch 1TH - - l - f - 6r ( ) 5 T 5 (l ) where5°(H) is the Riemann zeta function. Thus for T-<< 6 u U = 3";ng1‘ (17) and - Q! - 12 I. 3 - I. 3 cv - dT - 5n“Nk(o ) - 23uNk(e ) (18) This is the well-known Debye T3 approximation for low temp- 8 eratures. It may be seen from this equation that the slope of the graph of cv versus T should approach zero as T —+.0. Both this prediction and the T3 variation of cv agree well with eXperiment in the temperature range 0° tog%o. Magnetic Contributions to the Specific Heat. The above consideration of lattice vibrations represents only one of several ways in which the crystal system can absorb energy. Other sources of absorption are due to (1) free electrons, (2) anomalies which occur with ferromagnetics and anti-ferromagnetics at the Curie and Neel points, (3) anoma- lies with superconductors at their transition temperatures, and (4) nuclear interaction with the electronic field. The first of these, the free electron contribution, is assumed negligible in the cases of the two salts considered in this investigation because the salts are dielectrics. The super- conductivity consideration is also non-applicable here. How- ever, both salts exhibit anomalies in the specific heat curve which seem indicative of magnetic order-disorder transitions and one of the salts, the tetrahydrate of manganous acetate, might possible indicate a nuclear contribution to the speci- fic heat in the region T (29) i n=l where‘<§nofi>is the yet undetermined expectation value of the Operator SnOP of one of the z nearest neighbors to atom i. Each atom is now effectively in a molecular field, S o -2|J|:§:-n p h=l gym Taking the direction of this field to be the z direction (30) (shop) = ($13,013) = 0 (31) And SiZOP has expectation values S, 8-1, ... -S+l, -S. VanVleck restricts himself here to crystal lattices for which none of the nearest neighbors of an atom are near- est neighbors of each other. For a system in thermodynamic equilibrium, the mean value of S2 is the same for all atoms on sub-lattice B, and the average moments of the atoms on the two sub-lattices are equal and opposite. VanVleck Shows that the molecular field on an atom of sub-lattice A is l 2|J| (32) To determine the variation of S with temperature we must substitute this eXpreSSion in place of H in Equation (19). This yields, 1H 2|J|zSS -__ET_- S = SBSE J (33) The solution S of this equation is S as T -+ 0 but falls to 0 as T -+ TC. The physical meaning here is that at the abso- lute zero all the Spins on one sub-lattice will be perfectly aligned pointing in one direction and all those on the other sub-lattice will be oppositely oriented. AS the system ab- sorbs energy its disorder increases and when the critical temperature is reached all long-ordering completely vanishes. Above TC, i.e., in the paramagnetic state, S = 0. From Equation (33) we have - -NIJIZSZ (3a) m I Therefore, a In. = -2NIJIz§ (35) min. H ["1 CV = d H This may be shown [7] to reduce to 1611‘2 '62 a c = Nk[-—--] = —— (36) V 271“2 T2 in the paramagnetic state, where t is the characteristic temperature defined by 2 ’t = 2.4921118 <3 + 1) <37) Coupling the expressions of Debye and VanVleck we may write for the heat capacity above TC Cv = I7 + bT3 (38) 15 where the first term gives the magnetic contribution and the second refers to the lattice heat capacity. In the region of interest in this paper, the second term remains at all times negligible, within the limits of experimental error, since b is quite small for each of the two salts being considered. In the case of ferromagnetic materials, Spin wave theory predicts a contribution to the specific heat propor- tional to the temperature to the three-halves power. [8] The values obtained for the heat capacity of manganous acetate in the present study seem to give good agreement with this "T3/2 law." Nuclear Specific Heat. In their work on the Specific heat of ferrites Pollack and Atkins [8] report a nuclear con- tribution to the Specific heat which is proportional to %7, in the case of cobalt ferrite. This nuclear heat capacity comes about because the Co59 nucleus has an intrinsic magnetic moment, and therefore interacts with the hyperfine field at the nucleus due to orbital electrons. Pollack and Atkins suggest that it may be possible to observe this effect in manganese ferrites. Although manganous acetate is not a ferrite, an attempt has been made to relate the rise in the Specific heat below 1.H°K to a nuclear Specific heat con- tribution. Another possible reason for this rise in the heat capacity observed at very low temperatures for manganous acetate is that there may be another transition below 1.2°K. 16 The work of Dzialoshinskii [9] has demonstrated the possibi- lity of an intermediate state existing between the true anti- ferromagnetic state and the paramagnetic state. This inter- mediate state comes about when, instead Of attaining an ordered state in one step as the temperature approaches abso- lute zero, certain substances seem to have a first transition in which the spins of the atoms on one sub-lattice shift into canted positions with respect to those of the other sub- lattice and then a second transition occurs in which com- plete order ensues. Thus it is apparent that this inter- mediate state will give the appearance of being a weak type of ferromagnetism, since because Of the canting, atoms Of one sub-lattice will always have some components of spin that cannot be cancelled out by the oppositely directed spins of atoms on the other sublattice. Moriya eXplainS the physical interactions responsible for canting by suggesting two distinct mechanisms which may give rise to this effect. [10, 11] The first mechanism Operates because of the dif- ferences in the single spin magnetocrystalline anistropy for differing Sites. The second mechanism is through an anti- symmetric exchange coupling. Entropy Consideration. From statistical mechanics, one Obtains the following expression for the change in entrOpy of a paramagnetic system at low temperatures and zero magnetic fields, [12] A4 = R 1n (28 + 1) (39) 17 where R is the gas constant, and S is the ground state spin of the paramagnetic ion. From this equation we obtain a theoretical value for the entrOpy which is to be compared with our calculated values. We are also interested in the amount of entrOpy change occurring above the transition temperature as com- pared with that taking place below TC. This gives us a measure of the degree of order still remaining in the crystal above the transition point. CHAPTER II EXPERIMENTAL APPARATUS Dewar System and Calorimeter. The specific heat measurements are made in an adiabatic calorimeter, which is mounted in a conventional double Dewar system. This system consists of one Dewar flask, 90.7 cm long, (for liquid helium)mounted inside a second Dewar flask, 92 cm long, (for liquid air or nitrogen). Both Dewars are strip Silvered, for convenience in viewing the liquid levels. Figure 1 shows this Dewar arrangement. Attached to the top of the helium Dewar is a two-inch COpper tee. The side arm of this tee is connected to the liquid helium pumping system, while the top arm is used for mounting Of the calorimeter. The adiabatic calorimeter is shown in Figure 2. The calorimeter can is made of COpper, one mm in thickness, (h = 15.9 cm; d = u.0 cm). The top plate, labelled A ianigure 2, is held to this can by eight 6/32" screws. To ensure a vacuum seal (at helium temperatures), a fuse wire "0" ring is used. The leads from the thermometer and heater on the sample are brought out of the calorimeter through four tungsten glass seals which are mounted on the tOp plate Of the calorimeter. A 1/2" stainless steel tube is also soldered to the tOp plate for evacuating the calorimeter. A small radiation shield, D, is incorporated into the 18 19 L to I pump 5.” cm I ll glass 1 ( I flange L_A J 'I 6.Hcm 4 I N \ x \ \. \ \ \ \. \ \ vacuum -————4 \ liquid air \ vacuum \ liquid He \ 92 cm s \ K N N x \ x N \ \ \ Figure l. Dewar System .1, 2O to ionization fl gauge I ‘\ f for admission of -:j I liquid helium to pump <——— to manometer H——\\ I B ———+L I I 7H cm =—\_/ / [£“1JLILr-—1[ lower view 15.9 cm e‘u.1 ‘I cm Figure 2. Adiabatic Calorimeter 21 pumping line to reduce the heat leak into the calorimeter. The pumping tube is connected at the top of the helium Dewar to a brass flange, labelled B in the diagram, which in turn is sealed to the top of the c0pper tee by means of a neoprene "O" ring. An ionization gauge (NRC - 507) and a vacuum valve (Veeco: 1/2") are connected to the pumping tube above the brass flange. Several other Openings in this flange are used for introducing the liquid helium into the Dewar, for taking out the electrical leads, and for connections to the pressure manometers. Preparation of the Sample. The sample, a single crystal, is grown from an aqueous solution at room tempera- ture; usually it weighs between 0.5 gram and 2 grams. A hole is drilled through the center of the crystal and a small car- bon resistor is inserted to serve as a thermometer, (56 ohms, Type TR, l/10 w, Allen-Bradley). Wrapped around the sample is approximately one foot of fine manganin wire which serves as a heater wire, (H00!1/ft., enamel insulation). The leads to both resistor and heater are of copper, teflon insulated, (A.W.G. 3A). The sample is coated with glyptal to prevent its dehydration and also to fix the heater coil in position. It is mounted inside the calorimeter as Shown in Figure 2. A nylon thread, passed through a small hole in the radiation shield, provides for suspension of the sample. Circuits. The temperature of the crystal is deter- mined by measuring the voltage drOp across the carbon resistor. (See Figure 3.) This provides a direct indication 22 10011 l K-2 J Potentiometer K-3 Potentiometer @ RT §__l ___l Figure 3. Circuit for Crystal Thermometer : I 1-1 {HI "\ Potentiometer \ W— W Heater Figure u. Std: 10011 Measurement of Heater Voltage and Current 23 of resistance since a lOPa current is maintained in this cir- cuit at all times. Voltage is read on a Leeds and Northrup Type K-3 Potentiometer, used in conjunction with a L 8 N Speedomax Recorder. The bridge circuit for providing a steady lOPa current is shown in Figure 3. With the L 8 N potentiometer K-2 set at 10-3 volts, the variable resistor Rv is adjusted until the galvanometer (a high sensitivity wall galvanometer: L 8 N No. 2285) in the output of the potentiometer circuit shows zero deflection. This adjustment is made before each voltage reading. In order to calculate the heat input to the sample in a given interval of time, it is necessary to know the voltage drOp across the heater coil, the current in it, and the time during which the sample is heated. The circuit for this measurement is shown in Figure H. When the DPDT switch is in position 1, the potentiometer (L 8 N Type K-l using a No. 2M20-B Galv.) reads the drop across the heater. In position 2, it reads the drOp across a lOOIlstandard resistor in the heater circuit. Since the current is the same for both the resistor and the heater, this voltage reading is readily converted to current. The time of heating is deter- mined by means of a stOp watch which can be read to 0.1 second. Measurement and Control of the Liquid Helium Bath Temperature. TO lower the temperature of the liquid helium bath below u.2°K, it is necessary to reduce the vapor 21+ pressure of the liquid. This is done in the present experi- ment by using a large capacity vacuum pump, (Kinney KDH-130). The vapor pressure is read by a conventional Hg manometer for temperatures above the Arpoint (2.2°K), and an octoil manometer for temperatures below the A-point (this increases the reading scale by a factor of approximately 1”). These vapor pressure readings are converted to temperatures using the 1958 He” temperature scale. [13] In order to maintain a constant temperature Of the bath for purposes of calibration, two methods are used. Above the.1rpoint, control is achieved by adjusting the pumping speed of the vacuum pump. A set of coarse and fine adjustment vacuum valves is used. Below the.2:point, because of the large thermal conductivity of the liquid, it is pos- sible to use a small wire wound heater (a noun) in the bath together with a carbon thermometer (220flw 1/2 w, Allen- Bradley). Figure 5 shows the circuit used for this method of control. By first adjusting Rv SO that the galvanometer reads null, the current through the HOOIIheater is continually controlled in order to maintain a galvanometer null. Tempera- tures can be controlled in this manner to at least 0.001°K. Vacuum System for Calorimeter. The two branches of the calorimeter vacuum system, one for the high vacuum side and the other for roughing purposes, are diagrammed in Figure 6. The pumps employed in this system are a Welch Duo-seal pump and a conventional oil-diffusion pump. The latter is protected by a liquid air trap. Pressure readings 25 Resistor in Bath ( Thermometer ) Figure 5. Circuit for Temperature Control Below 2.2° K 26 T-C Gauge To Calorimeter._——» Liq. Air Trap '+L.Oil Diffusion Pump T-C Gauge I2: For Admission of Exchange Gas To Fore-pump I Ballast I Figure 6. Calorimeter Vacuum System 27 are taken in the two branches by means Of two thermocouple gauges, type 501. The vacuum system is connected to the COpper tee through a brass bellows allowing a degree of flexibility at this joint. The positions of the five valves in this system may be seen in the diagram. The samples used in these experiments were Single crystals weighing between 0.5 — 2.5 grams and measuring approximately 1.0 - 1.5 cm on a side. The chemicals used to prepare the aqueous solutions from which they were grown were obtained from the J. T. Baker Chemical Company and were of analytical reagent grade. The ferrous bromide crystals were of hexagonal type and were dark brown in color. The manganous acetate crystals were monoclinic and were pink in color. An analysis was made of one of the ferrous bromide crystals by the Schwarzkopf Microanalytical Laboratory, 56-19 37th Avenue, Woodside, New York. CHAPTER III EXPERIMENTAL PROCEDURE When the sample has been suspended from the top of the calorimeter as explained in Chapter I, the calorimeter can is screwed securely into place. The "0" ring, as shown in Figure 2, seals the can against liquid helium. The entire apparatus is then sealed inside the Helium Dewar Of Figure l and the valve to the calorimeter is closed to pre- vent dehydration of the sample while the rest of the system is being pumped down. After removing the air from the Helium Dewar, gaseous helium is admitted and then pumped out. This is repeated several times in order to remove the last traces of air, and then the helium is finally left at atmos- pheric pressure. The outer flask is filled with liquid air in order to pre-cool the calorimeter system. It usually takes several hours for the calorimeter to reach liquid air temperature. It is the usual practice in the present eXperi- ment to allow the pre-cooling process to continue overnight. The calorimeter is evacuated after liquid air tem- peratures have been reached (this is evident by the resis- tance reading of the carbon thermometer on the sample which has increased to approximately 60 ohms) and a good vacuum obtained. Helium gas, at a pressure of 1 mm Hg is then ad— mitted to the calorimeter to serve as an exchange gas during 28 29 the calibration process. The transfer of the liquid helium is carried out in the following way: a large (25 l.) flask containing the helium is placed on a hoist next to the experimental appe- ratus. A long transfer tube is simultaneously lowered into both flasks while the hoist is raised. Then helium gas is pumped into the portable flask in order to force the liquid helium over. When the inner flask is full, the helium gas flow is cut off and the transfer tube extracted. It will be recalled that the carbon resistor was embedded in the sample to serve as a thermometer. To carry out the calibration of this resistor, it is necessary to know its resistance at fixed temperatures. Usually about twelve calibration points are taken, starting from H.2°K and going down to approximately l.2°K. It is assumed that the sample is at the same temperature as the bath during this calibra- tion, due to the presence of the exchange gas inside the calorimeter. In practice, the manometers are connected into the system just after helium transfer and a reading taken at atmospheric pressure. Then the cooling is started by opening the valve to the Kinney pump to increase the rate of evapora- tion of the bath. By controlling the pumping speed, tem- perature readings are taken at about 10 cm (Hg) pressure intervals. This consists of reading the manometers, and voltage drop across the carbon thermometer. The voltage drOp is a measure of resistance Since the 10p; current in the thermometer is held constant at all times. The vapor 30 pressure readings of the manometer are converted to tempera- ture by using the helium vapor pressure tables. [13] The lowest reading taken on the mercury manometer is usually about 5 cm. Then the oil manometer is connected to the system and is used down to the lowest temperatures. When the calibration is complete the He exchange gas is pumped out of the calorimeter. Specific Heat readings are taken in this manner: the recording potentiometer is set in the zero position and the voltage is noted. A short period elapses during which the temperature is slowly rising due to the heat leak. When the trace is sufficiently long to establish the lepe of this heat leak curve, power is turned on in the heater of the sample. A stOp watch is used to determine the time of power input to the nearest 0.1 second. Readings of voltage, current, and time are made and another interval of heat leak recorded. The method for subtraction of the tempera- ture rise due to heat leakage during the period of power input will be eXplained in the next chapter. This process is repeated for as many points as possible in the range under investigation. During an average run, between sixty and seventy points are obtained. CHAPTER IV DATA PROCESSING AND CALCULATIONS Calibration. All the pressure readings are eXpressed in terms of cm Hg, those taken on the oil manometer being multiplied by the ratio of the density of the Oil to that of mercury. These are converted to temperature readings by ref- erence to the Helium Vapor Pressure tables mentioned in Chapter II. Since the carbon thermometer acts like a semiconduc- tor in the liquid helium region, one would expect that its resistance would vary with the temperature as follows: R = Aea/T where A and a are constants. By plotting log R as a function of l/T, a straight line is Obtained. This curve may now be used to obtain temperatures and temperature dif- ferences caused by power input. Since the carbon thermome- ter's resistance is not reproducible, it is necessary to take a separate calibration curve for each run. Figure 7 shows a typical record of a fore, during, and after heating cycle. The steeper regions, between (1) and (2) and between (3) and (H) called the fore and after heating periods respectively indicate the rate of heat leak, while the mid-section of the curve (between 2 and 3) shows a more rapid temperature rise which is due to the heating of the sample by the power input. The voltage readings cannot be taken at points (2) 31 32 Time ? (\Ik VI + Temp. (-V) Figure 7. Typical Recorder Trace for Specific Heat Measurement 33 and (3) directly, however, since a part of this temperature rise is due to the heat that leaked into the sample while power was being supplied. Therefore, to subtract this con- tribution, we extend both heat leak regions as shown in the figure. Then lines a and b parallel to the voltage axis are drawn through points (2) and (3) and their median, line c, is located with a divider. The points of intersection of this line c and the extensions of the heat leak curves are taken as indications of the actual temperature rise due to power input. This is equivalent to extrapolating back to the mid- point of the heating period. To obtain the voltages corresponding to these points, we must know what the voltage was at point (1) and the cali- bration of the chart in volts/div., characteristic of this temperature. The former is already known since the voltage on the K-3 potentiometer is read at the start of each new point and the latter may be found from the calibration curve of the potentiometer. Thus, by counting the scale divisions from the left time axis to the points of intersection, multi- plying by the proper volts/div. value,and subtracting from the voltage at point 1, the voltageS--and therefore the resistances of the thermometer at the points of intersection-- are obtained. The lOgarithms of these resistances are then plotted on the calibration curve and the corresponding l/T values recorded. Temperatures are thus determined, and by subtraction we know the AT for each power input. The average of each pair of temperatures is also obtained as we assume 3.. the value of specific heat will be approximately constant over this small interval. The heat capacity of the sample at this average temperature may then be calculated by divi- ding the total heat input by'AIB The heat input is Obtained by multiplying the voltage and current readings of the heater with the time of heating. CHAPTER V RESULTS AND CONCLUSIONS Ferrous Bromide Tetrahydrate (FeBPZ'uH2O)- The cal- culated values of T,t>T, and C for five experimental runs on the ferrous bromide crystals may be found in Appendix I. The values of heat capacity have been corrected for energy dissipated across the leads and for the heat capacities Of the thermometer and the glyptal. These losses amounted to less than one per cent of the total energy input. A plot of the heat capacity as a function of temperature in the range 1.16°K - H.20°K is shown in Figure 8. The sharp peak occur- ring at l.28°K may well be indicative of a magnetic transi- tion although no confirmation of this has been obtained by other methods. However, some indirect evidence exists from the magnetic susceptibility work on the isomorphous crystal of FeClzoquO. [1%] It will be noted, however, that the curve does not drOp to a constant value above the transition temperature immediately but has a small tail extending over about 0.2°K. This seems to indicate a slow diminution of the short-range ordering above the transition temperature. It is of interest to calculate the entropy change taking place during this transition. Using the method de- velOped by Friedberg [15], and Kapadnis and Hartmans [16], we may evaluate the changes in the entrOpy above and below 35 ovfleonm muoHAOh.Ho huaowmwo poem .w onumfih oh ...—... “ OWN m _ _ b 00PM _ _ L _ OWN . . _ _ _ 00H 1 . q 1 a 4 q q _ q _ — o x x ...-n... .x x.+x+x+ .u. . o o x X.“ 0.. .0 «4:3 *6. 0 In x I If i ...“... I... I an o ‘00. o W. s.m0.° . + +++ ++ + .... +1.. «.... «aura... +x+£. 9. MM!” 00+! +W+$ J... shaggy-flea dMMw .. N .... x 0 1.. o % ..m .. O a .. . 000 1| 0 II o o O % . SS .2 Esme -- m x «boa .oH mundane e . News .0 sumsnas mo .Mnoa . Homa .s nonaooon A Mao o 33 .H 93503 37 the critical temperature separately, in order to observe the total magnetic entrOpy change. We assume that above TO the magnetic heat capacity varies inversely with the square of the temperature while the lattice heat capacity varies directly with the cube of T in accord with Debye and VanVleck as given in Equation (38) where a and b are the spin and lattice heat capacity constants. These are seen from the CT2 versus T5 curve of Figure 9 to have the values, a = 3.05 911L933; b = 0.078 cal ——. Above To, there- mOle mole odegu fore, we may obtain the magnetic contribution to the entropy change by evaluating the integral, no N A} = (5111‘ = M—gndi‘ (00) To i.u T The value of T0 was determined from the plot of Figure 9, by noting the temperature at which the curve deviates from linearity. This integral yields a value of 0.79 cal/mole-deg for the magnetic contribution to the entropy above To. Below TO a plot of C/T versus T was made and the entrOpy contribution from 0°K.to l.u°K.waS obtained graphi- cally. We assume here that the lattice contribution to the specific heat in this region is negligible compared to the magnetic contribution. This plot is shown in Figure 10 and measurement of the entropy contribution yielded the value 1.85 cal/moleodeg. Combining the magnetic contributions above and below the TO therefore, we obtain the total entrOpy change for this transition 1.85 + 0.79 = 2.69 cal/moleodeg. This is seen to be in fair agreement with the value obtained 38 X 0.0.28.5 36.30% you 9 SEE on . m newsman “O O SS .3 E835 nos” .3 Sam... 32 .m snags _ a 11 l m m Bo 39 31$ B 0330.8 mayhem no.“ onspmhomSoa admnob .39“an .oa oBmHm m2” 0..” m. _ _ 1 _ A lq _ u 4 I a 00 from the theoretical expression: AJ = R ln(2S + l) in which the ferrous ion (Fe++) is taken to have Spin (S) = 2:A.J= R ln5 = 3.19 cal/mole-deg. It should be pointed out that about thirty per cent of the entropy change occurs above To, indicating the persistence of short—range ordering above To. Manganous Acetate Tetrahydrate [Mn(C2H302)2oHH20], The corrected values of T}.AI'and C for the five experimental runs taken on manganous acetate samples are shown in Appendix II, and a plot of these data may be seen in Figure 11. A gradual rise in the heat capacity, from about one cal/mole- deg at 2°K.to about three cal/mole‘deg at TC 3.17°K, indi- cates a second—orderuA-type transition. TC is believed to be the Curie temperature for manganous acetate, the salt being weakly ferromagnetic below this point, as reported by ; Flippen and Friedberg. [17] As in the case Of the ferrous bromide, the behavior of the heat capacity above TC may be described by the equa- tion C = $7 + bT3o This is verified by the CT2 versus T5 curve shown in Figure 12. The constants were found from this curve by the method of least squares: a = 15.31; b = 0.00363. (The solid line appearing above TC in the C versus T plot of Figure 11 is a plot Of the above equation. Below TC the heat capacity does not approach zero as T —+-0 but drops smoothly to a value of approximately one cal/mole- deg at 2°K, remains constant there for about 0.6°K, and then begins to rise again as T —+ 0. Pollack and Atkins found a similar rise below 3°K with cobalt ferrite [8] and following 093004 Handmade Mo .mfiodmdo poem ...H 093m . $2 ... ens . $3 ...N genes . 33 .8 82. x 32 .3 s3. . 3% .mm 23h. 3334 Sandman: mom me 3693 mac .3” Penman o 83 83 08 .m. _ 4 .I . _ d a a _ A q _ A. . . . . . . _ _ x x x X XX (Xx «KthJNX-XX( ( K I I} .. X ”KN Kx x x I “x l\ k X“ H X x “I! p. X i i I K K K I14 ‘XX x ‘ X XX X X 1+2 on 90 H3 the suggestion of Bleaney [18] and Marshall [19] have shown this heat capacity to be inversely prOportional to the square of the temperatureo It is believed that this con- tribution is the nuclear heat capacity arising from the inter- action between the nuclear magnetic moment and the magnetic field set Up at the nucleus by the orbital electrons. Pollack and Atkins predicted that a similar effect should be observed in the case of manganese salts. The present experi- ment seems to lend some support to this theory. When the quantity E§97 is plotted against T3/2 as in Figure 13, a linear graph is not achieved. However, if suc- cessive values of lg-are subtracted from the experimentally T . . cv - F/TQ. . determined Cv's and the quantity T3/2 is plotted against T3/2 a well-defined straight line results. The smallest de- viation from the linear plot was obtained by choosing for the constant x*the value l.u6. Reading the constants from the graph, we may write for the linear equation, = [.1uT3/2 + .029T3] ———99i-— (ul) Cmag mole-deg When this eXpression for the magnetic heat capacity is plotted as a function of temperature and the equation, 1.U6 cal Cnuclear : T2 l:mole-deg] (”2) is plotted on the same graph, the sum of the two curves yields the observed heat capacity versus temperature curveo uu opmpoo¢ msonwmnds now mdao no poam ¢ .MH on:mam was i ‘r i 1. "x? *r -L- X. X K . m grids Ame $0.0 + Qmaflov u use . hdoaoon AMKHMO v NB\©¢3H N o cur-N -b db- HS Prior to the calculation taking into account the nuclear contribution, several analytical functions were tried in an attempt to fit the eXperimental curve. Below TC the heat capacity was found to vary with T according to the equation 1DCT2=Ae‘B/T where A = 8.935 and B = 3.6Q°K. Further, the entropy curve obtained from the experimental data is shown in Figure 1”, together with the theoretical magnetic and nuclear contributions. Again, to a good approximation, the entropy change calculated from the measurements is equal to the sum of the other two, except for the slight disagree- ment in the range l.2°K.» l.3°K. A calculation of the entrOpy change in this tran- sition was carried out, using Equation (38) for the change above TO and Equation (kl) for the magnetic part of the entropy change below To. For the change above To, we have 3° 00 AJ=J %=J§3dt (1+3) T 3 3T 0 ° _ ‘ The values of a and T0 were obtained from the CT2 versus TS graph of Figure 12, and the lattice term is again ignored in the integration as in the case of ferrous bromide, due to the small value of b (0.0036). This integral yields an entrOpy change of 0.70 cal/molecdeg. Below To, we may eXpress the entropy change by the integral, 3.3 AJ =f 3°3.1uT1/2dT +f .029T2dT (an) 0 0 3334 323mg: no.“ 0932359 mumnob hmonvnm .3 Pun—mam O o . A mov a a o.m 9m 04 . o ILI.I._I+I_..I!._FI... _ _ _ _ _ _ a _ _ _ a _ . - ' XI... '1 ' 'K’ _ ’ x, . I. 1 a . . I + b ‘ — ... + ‘1 § 8 £10 I t+ x 1. x. c. l I. O O p. 0 £3.64 “vfix 0...“ 010%”?! “a... / oioo~.343o of...... v 40! $ 0...... c: to... Cg I C. O . ‘ C 0+3. K 0000‘ o I I 0.... 6 0 +5. s o o r/ . nae. / ++ ..... I 1 Duo 9 v...;/ .L . . .. oA . z w .. ma , 34 u o M I , I X I. , + 33 K has , . 32 Km gamma . $2 .3 was ,_ so . 33 .3 33. x 3% .mm 25s u? yielding for the change in entropy the value 0.91 cal/mole deg. Combining the entropy gains above and below To, we obtain 1.61 cal/moleodeg. This differs from the theoretical value, calculated by means of Equation (39), by more than a factor of 224.1: R ln6 = 3.58, taking 5/2 for the ground state spin of the Mn++ ion. This poor agreement in the entrOpy calculation may lend support to the possibility that another transition exists below l.2°K as was discussed in Chapter I. In other words, the entrOpy change for the lower transitions must be added to the above, which may possibly improve the agreement. This argument is made in spite of the fact that the curve fitting suggests a nuclear contribution. In summary we have, in these experiments, shown that a definite transition, possibly magnetic in origin, occurs very close to l.28°K in the case of FeBrzouHZO. We have calculated the entropy change above and below the transition temperature and have seen that at least thirty per cent of the total change is due to persistence of short-range order- ing, not taken into account in the theory of VanVleck. As for Mn(C2H302)2°uH20, we have identified a second order transition at about 3.17°K. The latter may be due to a nuclear contribution of the form %% which seems in very good agreement with our measurements. It may also be due to another transition occurring at a temperature lower than our methods were able to achieve. The resolution of this question must await further investigation. 1) 2) 3) u) 5) 6) 7) 8) 9) 10) 11) 12) 13) 1”) 15) 16) 17) 18) 19) LIST OF REFERENCES F. Richarz, Ann. Physik i8, 708 (1893). P. J. Debye, Ann. Physik 39, 789 (1912). C. Kittel, Introduction to Solid State Physics, (John Wiley and Sons, Inc., 1953), p. 63.. C. Kittel, Introduction to Solid State Physics, (John Wiley and Sons, Inc., 1953), p. 1H7. A. B. Lidiard, Rep. Progr. Phys. 11, 201 (195%). J. H. VanVleck, J. Chem. Phys. 2, 85 (19M1). J. H. VanVleck, J. Chem. Phys. 5, 320 (1937). S. R. Pollack and K. R. Atkins, Phys. Rev. 125, 12H8 (1962). "‘— J. Dzialoshinskii, Soviet Phys. JETP 6, 1130 (1958). T. Moriya, Phys. Rev. 117, 635 (1960). T. Moriya, Phys. Rev. 20, 91 (1960). A. W. Wilson, Thermodynamics and Statistical Mechanics, (Cambridge University Press, 1957), p. 303. F. G. Brickwedde, H. van Dijk, M. Durieux, J. R. Clement, and J. K. Logan, J. Research Nat'l Bur. Standards 6HA, l (1960). R. D. Pierce and S. A. Friedberg, J. App. Phys. 33, 665 .(1961). S. A. Friedberg, Physica 18, 714 (1952). D. G. Kapadnis and R. Hartmans, Physica 32, 181 (1956). R. B. Flippen and S. A. Priedberg, Phys. Rev. 121, 1591 (1961). B. Bleaney, Phys. Rev. 18, 21% (1950). w. Marshall, Phys. Rev. 110, 1280 (1958). H8 APPENDICES T(°K.) 1.4286 1.4354 1.4473 1.4575 1.4670 1.4802 1.5158 1.6428 1.5572 1.5662 1.5916 1.6036 1.6144 1.6270 1.6394 1.6507 1.6640 1.6771 1.6913 1.7053 1.7203 1.7355 1.7508 1.7735 Heat Capacity Data of Ferrous T(°K.) .0031 .0027 .0028 .0030 .0032 .0031 .0023 .0031 .0032 .0025 .0040 .0046 .0029 .0037 .0035 .0032 .0030 .0037 .0037 .0041 .0042 .0042 .0038 .0041 APPENDIX I December 1, 1961 1 C(mole. eg) 1.64 T(°K.) 1.7868 1.8045 1.8233 1.8470 1.8667 1.8887 1.9064 1.9318 1.9552 1.9820 2.0080 2.0411 2.0701 2.0977 2.1243 2.1454 2.1699 2.1906 2.5390 2.6316 2.7552 2.7770 2.9621 3.0047 Bromide T(°K.) .0032 .0043 .0037 .0046 .0035 .0061 .0054 .0048 .0042 °0043 .0041 .0056 .0047 .0035 .0050 .0037 .0052 .0048 .0058 .0056 .0084 .0062 .0158 .0190 C( cal mole-deg ) 1.27 1.30 T(°K.) 3.3536 3.4560 3.5329 3.9502 T(°K.) .0191 .0203 .0237 .0171 December 7, 1.8477 1.8629 1.8816 1.8997 1.9166 1.9387 1.9585 1.9791 1.9986 2.0180 2.0436 2.0666 2.0863 2.1174 2.1363 2.1594 2.1818 2.2037 2.2381 2.2727 2.3116 .0061 .0042 .0031 .0036 .0048 .0030 .0062 .0047 .0044 .0045 .0039 .0035 .0043 '".0041 .0046 .0047 .0053 .0039 .0050 .0062 .0054 C( 1961 cal 51 \ mole-deg) 1.08 1.10 T(°K.) 2.3521 2.3886 2.4334 2.4706 2.6656 2.7148 2.7578 2.8059 January 9, 1962 1.8426 1.8703 1.8910 1.9164 1.9411 1.9638 1.9914 2.0200 2.0487 2.0775 2.1083 2.1367 2.1917 2.2219 2.2504 2.2787 2.3097 T(°K.) .0061 .0051 .0065 .0055 .0064 .0066 .0061 .0081 .0096 .0095 .0093 .0102 .0095 .0108 .0100 .0102 .0101 .0099 .0098 .0119 .0121 .0084 .0096 .0089 .0090 C I car 1.39 1.61 1.44 1.60 1.27 1.58 \ ‘mole-deg’ 52 T(°K.) T(°K.) c T(°K.) T(°K.) c< 1:?fieg> 2.3551 .0122 1.40 3.6798 .0122 1.19 2.3980 .0103 1.46 3.7341 .0112 1.39 2.4381 .0078 1.58 3.7893 .0144 1.35 2.4746 .0086 1.69 3.8402 .0088 1.59 2.5141 .0108 1.55 3.8925 .0091 1.51 2.5536 .0078 1.76 3.9447 .0093 1.81 2.5997 .0101 1.65 3.9721 .0111 1.58 2.6441 .0098 1.43 4.0241 .0098 1.61 2.6841 .0093 1.61 4.1008 .0117 1.23 2.7236 .0081 1.58 4.1194 .0119 1.64 2.7708 .0108 1.38 January 16, 1962'. 2.8205 .0087 1.45 1.2855 .0039 3.94 2.8591 .0107 1.40 1.2956 .0069 3.01 2.9018 .0101 1.50 1.3067 .0056 2.72 2.9537 .0096 1.59 1.3170 .0065 2.51 2.9931 .0108 1.39 1.3281 .0067 2.36 3.0371 .0101 1.51 1.3404 .0089 2.21 3.0902 .0114 1.50 1.3566 .0079 2.15 3.1387 .0098 1.43 1.3738 .0076 2.14 3.1806 .0121 1.41 1.3909 .0077 2.00 3.2294 .0114 1.39 1.4063 .0081 2.02 3.2760 .0097 1.43 1.4252 .0061 1.88 3.4358 .0106 1.43 1.4462 .0086 1.78 3.4928 .0098 1.50 1.4672 .0076 1.77 3.5523 .0101 1.58 1.4968 .0099 1.69 3.6172 .0117 1.42 1.5191 .0085 1.69 T(°K.) 1.5513 1.8521 1.6087 1.6449 1.6743 1.7089 1.7325 1.7613 1.7959 1.8238 1.9013 1.9372 1.9920 2.0439 2.0822 2.1141 2.1563 2.1908 2.2451 2.2872 2.3215 2.3778 2.4245 2.4804 2.5246 2.5749 ,53 T(°K.) c