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Thermodynamic calculations of Fe-Mg interdiffusion in (Mg,Fe)(2)SiO4 polymorphs and perovskite
Baohua Zhang; Shuangming Shan
2015
发表期刊Journal of Applied Physics
卷号117期号:5
摘要 this study, we show that the temperature and pressure dependence of Fe-Mg interdiffusion in (Fe,Mg)(2)SiO4 polymorphs (olivine, wadsleyite, and ringwoodite) and perovskite can be successfully reproduced in terms of bulk elastic and expansivity data through a thermodynamic model (so-called cB Omega model) that interconnects point defect parameters with bulk properties. Under dry and wet conditions, our calculated Fe-Mg interdiffusion coefficients D-calc(Fe-Mg) (particularly for anisotropic diffusivity in olivine), activation enthalpy h(act), and activation volume nu(act) over a wide range of geologically relevant temperatures (1000-2400K) and pressures (0-100 GPa) are consistent with the experimental ones when the uncertainties are considered.
学科领域地球深部物质与流体作用地球化学
收录类别SCI
语种英语
文献类型期刊论文
条目标识符http://ir.gyig.ac.cn/handle/352002/5971
专题地球内部物质高温高压实验室_地球内部物质高温高压实验室_期刊论文
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Baohua Zhang,Shuangming Shan. Thermodynamic calculations of Fe-Mg interdiffusion in (Mg,Fe)(2)SiO4 polymorphs and perovskite[J]. Journal of Applied Physics,2015,117(5).
APA Baohua Zhang,&Shuangming Shan.(2015).Thermodynamic calculations of Fe-Mg interdiffusion in (Mg,Fe)(2)SiO4 polymorphs and perovskite.Journal of Applied Physics,117(5).
MLA Baohua Zhang,et al."Thermodynamic calculations of Fe-Mg interdiffusion in (Mg,Fe)(2)SiO4 polymorphs and perovskite".Journal of Applied Physics 117.5(2015).
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