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Title: Heat capacity and thermodynamic properties of andradite garnet, Ca/sub 3/Fe/sub 2/Si/sub 3/O/sub 12/, between 10 and 1000 K and revised values for. delta. /sub f/G/sub m//sup 0/ (298. 15 K) of hedenbergite and wollastonite

Journal Article · · Geochim. Cosmochim. Acta; (United States)

The heat capacity of synthetic andradite garnet (Ca/sub 3/Fe/sub 2/Si/sub 3/O/sub 12/) was measured between 9.6 and 365.5 K by cryogenic adiabatic calorimetry and from 340 to 990 K by differential scanning calorimetry. At 298.15 K C/sub p,m//sup 0/ and S/sub m//sup 0/ are 351.9 +- 0.7 and 316.4 +- 2.0 J(mol x K), respectively. Andradite has a lambda-peak in C/sub p,m//sup 0/ with a maximum at 11.7 +- 0.2 K which is presumably associated with the antiferromagnetic ordering of the magnetic moments of the Fe/sup 3 +/ ions. The Gibbs free energy of formation, ..delta../sub f/G/sub m//sup 0/ (298.15 K) of andradite is -5414.8 +- 5.5 kJmol, and was obtained by combining our entropy and heat capacity data with the known breakdown of andradite to pseudowollastonite and hematite at approx. 1410 to 1438 K. From a reexamination of the calcite + quartz = wollastonite equilibrium data we obtained ..delta../sub f/H/sub m//sup 0/ (298.15 K) = -1634.5 +- 1.8 kJmol for wollastonite. The authors have also used their thermochemical data for andradite to estimate the Gibbs free energy of formation of hedenbergite (CaFeSi/sub 2/O/sub 6/) for which we obtained ..delta../sub f/G/sub m//sup 0/ (298.15 K) = -2674.3 +- 5.8 kJmol.

Research Organization:
Geological Survey, Reston, VA (USA)
OSTI ID:
5099802
Journal Information:
Geochim. Cosmochim. Acta; (United States), Vol. 51:8
Country of Publication:
United States
Language:
English