Journal
PHYSICS AND CHEMISTRY OF MINERALS
Volume 32, Issue 5-6, Pages 374-378Publisher
SPRINGER
DOI: 10.1007/s00269-005-0003-8
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The low-temperature heat capacity of magnesioferrite (MgFe2O4) was measured between 1.5 K and 300 K, and thermochemical functions were derived from the results. No heat capacity anomaly was observed. From our data, we suggest a standard entropy (298.15 K) for magnesioferrite of 120.8 +/- 0.6 J mol(-1) K-1, which is about 2.4 J mol(-1) K-1 higher than previously reported calorimetric studies; but is in rough agreement with predictions from sets of internally consistent thermodynamic data.
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