Enthalpy of formation of CaSi2O5, a quenched high-pressure phase with pentacoordinate silicon |
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Authors: | M. Schoenitz A. Navrotsky N. Ross |
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Affiliation: | (1) Thermochemistry Facility and Center for High Pressure Research, Department of Chemical Engineering and Materials Science, University of California at Davis, Davis, CA 95616, USA, US;(2) Department of Geology, University College London, Gower St., London WC1E 6BT, UK, GB |
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Abstract: | The monoclinic titanite-like high-pressure form of calcium disilicate has been synthesized and quenched to ambient conditions to form the triclinic low-pressure phase containing silicon in four-, five- and sixfold coordination. The enthalpy of formation of the quench product has been measured by high-temperature oxide melt calorimetry. The value obtained from samples from a series of several synthesis experiments is ΔH f = (−26.32 ± 4.27) kJ mol−1 for the formation from the component oxides, or ΔH f = (−2482.81 ± 4.59) kJ mol−1 for the formation from the elements. The result is identical within experimental error to available estimates, although the previously predicted energy difference between the monoclinic and triclinic phases could not be verified. Received: 16 February 2000 / Accepted: 14 July 2000 |
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Keywords: | Oxide melt calorimetry Fivefold coordination Pentacoordinate silicon Calcium disilicate Phase transition |
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