Russian Chemical Bulletin, International Edition, Vol. 57, No. 6, pp. 1157—1159, June, 2008
1157
Thermodynamic properties of αꢀplatinum dichloride
Z. I. Semenova and T. P. Chusova
A. V. Nikolaev Institute of Inorganic Chemistry, Siberian Branch of the Russian Academy of Sciences,
3 prosp. Akad. Lavrent´eva, 630090 Novosibirsk, Russian Federation.
Eꢀmail: chu@che.nsk.su
The heat capacity of сrystalline αꢀplatinum dichloride was measured for the first time in
the temperature intervals from 11 to 300 K (vacuum adiabatic microcalorimeter) and from 300 to 620 K
(differential scanning calorimetry). In the 300—620 K temperature interval, the C° values for
p
αꢀPtCl2 (cr) coincide with the heat capacity of CrCl2 (cr) within the limits of experimental error,
which made it possible to estimate the heat capacity of αꢀPtCl2 (cr) at higher temperatures.
The approximating equation of the temperature dependence of the heat capacity in the interval from
298 to 900 K C° ( 0.8) = 63.5 + 21.4•10–3T + 0.883•105/Т2 (J mol–1 K–1) was derived using
p
the experimental values, as well as the literature data on the heat capacity of CrCl2 (cr). For
the standard conditions, the C°p,298.15 and S°298.15 values are 70.92 0.08 and 100.9 0.33 J mol–1 K,
respectively; H°298.15 – Н° = 14 120 42 J mol–1
.
0
Key words: lowꢀtemperature calorimetry, differential scanning calorimetry, platinum dichloride,
heat capacity, entropy, enthalpy.
The reduction was carried out as follows. A weighed sample of
the substance (0.08—0.15 g) was loaded into a quartz beaker, whose
weight was brought to a constant value, and the beaker was mounted
in a quartz reactor. The system was purged with hydrogen for
10 min. Then, using a special heater, the temperature in the sample
zone was gradually increased with a rate of 50 K h–1 to 473 K, and
the reaction was carried out for 40 min. Hydrogen chloride that
formed was absorbed at the reactor outlet in two consecutively
connected vessels filled with distilled water. The apparatus was
cooled to room temperature in hydrogen flow, the quartz beaker
was taken out and calcined to 1073 K to remove the adsorbed
hydrogen. The amount of platinum formed was determined by the
difference in weights. Weighing was carried out on an analytical
balance with an accuracy of 0.00005 g. The error in platinum
determination was 0.2—0.5%, depending on the sample weight.
The content of chloride ions was determined by potentiometric
titration with a 0.05 M AgNO3 solution under standard conditions
with a relative error of 0.5%. Found (%): Pt, 73.26; Cl, 26.67.
PtCl2. Calculated (%): Pt, 73,34; Cl, 26.66.
Xꢀray diffraction study of αꢀplatinum dichloride was carried
out on a DRONꢀ2 diffractometer with filtered copper radiation
(CuꢀKα radiation, Ni filter). The interplanar spacings coincided
satisfactorily with the values published1 for αꢀPtCl2. All reflections
in the Xꢀray diffraction pattern were indexed in the monoclinic unit
cell with the parameters a = 13.49 Å, b = 3.18 Å, c = 6.85 Å,
β = 107.75°, and Z = 4. These values agree well with the results
(space group С2/m, unit cell parameters a = 13.258 Å, b = 3.194 Å,
c = 6.802 Å, β = 107.75°, Z = 4) obtained in singleꢀcrystal Xꢀray
diffraction study.1
The purpose of this work is to measure the heat capacꢀ
ity of crystalline αꢀplatinum dichloride in the temperaꢀ
ture interval from 11 to 620 K and to calculate the entropy
and the enthalpy difference using the results obtained.
No experimental data on the heat capacity of crystalline
platinum chlorides have been reported so far.
Experimental
Synthesis of αꢀPtCl2. The synthesis is based on the data1 that
αꢀPtCl2 is formed by heating of βꢀPtCl2 at 773 K in an evacuated
ampule for 2 days. A weighed sample (0.5—0.8 g) of βꢀPtCl2,
which was synthesized using a standard procedure2 by thermal
decomposition of H2PtCl6•6H2O in a chlorine flow (РCl = 1 atm),
was loaded into a quartz ampule 15—18 mL in volume. T2he ampule
was evacuated at room temperature for 1 h, sealed, and heated in
a gradient furnace. The substance transfer (∼2/3 of the sample over
a period of 10 days) occurred from the "hot" (873 K) to "cold" zone
(773 K). The product precipitated represented dark violet dendrites
0.5—1.0 cm in size.
The substance synthesized was identified by elemental, Xꢀray
phase, and spectral analyses and by IR spectroscopy.
Elemental analysis was based on a method of platinum and
chlorine determination by separation of the metal from chlorine by
the reduction
PtClx (cr) + x/2 H2 (g) = Pt (cr) + x HCl (g)
with simultaneous uptake of hydrogen chloride by water. The optiꢀ
mal conditions for the reduction reaction to occur were preliminarꢀ
ily determined using a Paulik—Paulik—Erdey derivatograph.
The quantitative reduction of platinum dichloride was shown to start
above 340 K, and the rate maximum was observed at 403 K.
IR spectra were recorded on a Perkin—Elmer 325 instrument in
the region 200—400 cm–1 using СsI windows. Samples were preꢀ
pared as suspensions in anhydrous Nujol. Two strong absorption
bands were observed at 326 and 344 cm–1, which agreed with the
published data.3
Published in Russian in Izvestiya Akademii Nauk. Seriya Khimicheskaya, No. 6, pp. 1136—1138, June, 2008.
1066ꢀ5285/08/5706ꢀ01157 © 2008 Springer Science+Business Media, Inc.