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Thermodynamic properties of minerals and related substances at 298.15 K (25.0 C) and one atmosphere (1.013 bars) pressure and at higher temperatures
Open accessAbstract
Critically selected values for the entropy (S°288.«),molar volume (VWw), and for the heat and Gibbs free energy of formation (AH 0 f,z98.i5and AG°f.288.is) are given for 50 reference elements and 285 minerals and related substances.For 211 materials for which high-temperature heat-capacity or heat-content data are available AH°f,T, AG°f,T, S°T, logKf/r and (G°T H°298.i5/T) are tabulated at 100°K intervals for temperatures up to 2,000°K.For substances having solid-state phase changes or whose melting or boiling point is less than 2,000°K, we also have tabulated the properties listed above at the temperature of the phase change so that the heat or entropy changes associated with the transformation form an integral part of the high-temperature tables.
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Nesbitt, H. W., & Young, G. M. (1984) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(84)90408-3 · Cited by 2,368
Geochemical and mineralogical interpretation of the Viking inorganic chemical results
Toulmin, P., Baird, A. K., Clark, B. C., Keil, K., Rose, H. J., Christian, R. P., Evans, P. H., & Kelliher, W. C. (1977) · Journal of Geophysical Research · doi:10.1029/js082i028p04625 · Cited by 375
Kieffer, S. W. (1982) · Reviews of Geophysics · doi:10.1029/rg020i004p00827 · Cited by 332
Gooding, J. L. (1978) · Icarus · doi:10.1016/0019-1035(78)90186-0 · Cited by 188
Experimental determination of the solubility product of magnesite at 50 to 200°C
Bénézeth, P., Saldi, G. D., Dandurand, J.-L., & Schott, J. (2011) · Chemical Geology · doi:10.1016/j.chemgeo.2011.04.016 · Cited by 154
Metadata
- Publisher
- US Geological Survey
- Published
- 1968
- OpenAlex
- W1571370716
- Cited by
- 480
- References
- 0
- Type
- report
- Language
- en
- Open access
- gold
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