Phase Equilibria in System CaO‐CO2‐H2O and Related Systems, with Implications for Crystal Growth of Calcite and Apatite
作者:
PETER J. WYLLIE,
期刊:
Journal of the American Ceramic Society
(WILEY Available online 1967)
卷期:
Volume 50,
issue 1
页码: 43-46
ISSN:0002-7820
年代: 1967
DOI:10.1111/j.1151-2916.1967.tb14969.x
出版商: Blackwell Publishing Ltd
数据来源: WILEY
摘要:
Conditions for crystallization of calcite from melts in the presence of a vapor or gaseous phase are reviewed to provide possible guidelines for growth of calcite. Phase equilibrium data for the system CaO‐CO2show that to precipitate calcite from molten CaCO3the temperature must be above 1230° C and excess CO2must be present at pressures greater than 39.5 bars. Phase equilibrium data for the system CaO‐CO2‐H2O show that calcite can be precipitated from melts at 650°C in the presence of an aqueous vapor phase at 10 bars or more. Crystallization can be induced either by introducing temperature variations, or by changing the composition of the coexisting aqueous vapor phase under isobaric, isothermal conditions. The system CaO‐MgO‐CO2‐H2O is used to show that doped calcite crystals, CaxR1‐xCO3, could be precipitated, with precisely controlled compositions, from melts in the system CaO‐RO‐CO2‐H2O. Apatite phase relatio
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