| Reference Type | Journal (article/letter/editorial) |
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| Title | The entropy of zinc chromite (ZnCr2O4) |
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| Journal | Mineralogical Magazine |
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| Authors | Klemme, S. | Author |
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| van Miltenburg, J. C. | Author |
| Year | 2004 (June) | Volume | 68 |
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| Issue | 3 |
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| Publisher | Mineralogical Society |
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| DOI | doi:10.1180/0026461046830202Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 243553 | Long-form Identifier | mindat:1:5:243553:8 |
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| GUID | 0 |
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| Full Reference | Klemme, S., van Miltenburg, J. C. (2004) The entropy of zinc chromite (ZnCr2O4) Mineralogical Magazine, 68 (3) 515-522 doi:10.1180/0026461046830202 |
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| Plain Text | Klemme, S., van Miltenburg, J. C. (2004) The entropy of zinc chromite (ZnCr2O4) Mineralogical Magazine, 68 (3) 515-522 doi:10.1180/0026461046830202 |
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| Abstract/Notes | AbstractThe low-temperature heat capacity of zinc chromite (ZnCr2O4) was measured between 6.5 K and 400 K using adiabatic calorimetry, and some thermochemical functions (CP(T),S(T), S°298,H(T)-H(0)) were derived from the results. The standard entropy (S°298= 128.6±0.3 J mol-1K-1) for zinc chromite was calculated from the results. Our calorimetric measurements indicate one extremely large anomaly in the heat capacity curve at ∼12.3 K which is related to the cubic-tetragonal transition in ZnCr2O4. |
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