Formation enthalpy of ThSiO4 and enthalpy of the thorite→huttonite phase transition

被引:50
作者
Mazeina, L
Ushakov, SV
Navrotsky, A [1 ]
Boatner, LA
机构
[1] Univ Calif Davis, Thermochem Facil, Davis, CA 95616 USA
[2] Univ Calif Davis, NEAT ORU, Davis, CA 95616 USA
[3] Oak Ridge Natl Lab, Oak Ridge, TN 37831 USA
基金
美国能源部;
关键词
D O I
10.1016/j.gca.2005.03.053
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The standard enthalpy of formation of thorite and huttonite and the enthalpy of the phase transition between these polymorphs were determined using high-temperature oxide melt solution calorimetry and transposed temperature drop calorimetry. Standard enthalpies of formation of thorite and huttonite are reported for the first time and are -2117.6 +/- 4.2 kJ/mol and -2110.9 +/- 4.7 kJ/mol, respectively. Based on our measurements, thorite and huttonite are metastable relative to SiO2 (quartz) and ThO2 (thorianite) at standard conditions, but are presumably stabilized at high temperature by the entropy contribution. Based on the measured enthalpy of the thorite-huttonite phase transition of 6.7 +/- 2.5 kJ/mol, a dP/dT slope for the transformation was calculated as -1.21 +/- 0.45 MPa/K. Copyright (c) 2005 Elsevier Ltd.
引用
收藏
页码:4675 / 4683
页数:9
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