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The Effect of Water on Fe‐Mg Interdiffusion Rates in Ringwoodite and Implications for the Electrical Conductivity in the Mantle Transition Zone | |
Baohua Zhang; Takashi Yoshino; Chengcheng Zhao | |
2019 | |
Source Publication | Journal of Geophysical Research: Solid Earth
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Pages | 2510-2524 |
Abstract | We determined the kinetics of Fe‐Mg interdiffusion in ringwoodite aggregates as a function of water content (up to ~6,000 wt. ppm H2O) at 20 GPa and 1,373–1,673 K by the diffusion couple method. The dependence of Fe‐Mg interdiffusivity (DFe‐Mg) on Fe concentration was determined using the Boltzmann‐Matano method. The experimentally reported DFe‐Mg in ringwoodite within 0 ≤ XFe ≤ 0.1 could be fitted by the relation |
Indexed By | SCI |
Language | 英语 |
Document Type | 期刊论文 |
Identifier | http://ir.gyig.ac.cn/handle/42920512-1/10594 |
Collection | 地球内部物质高温高压实验室 |
Affiliation | 1.Key Laboratory for High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry,Chinese Academy of Sciences, Guiyang, China 2.Institute for Planetary Materials, Okayama University, Tottori, Japan |
Recommended Citation GB/T 7714 | Baohua Zhang;Takashi Yoshino;Chengcheng Zhao. The Effect of Water on Fe‐Mg Interdiffusion Rates in Ringwoodite and Implications for the Electrical Conductivity in the Mantle Transition Zone[J]. Journal of Geophysical Research: Solid Earth,2019:2510-2524. |
APA | Baohua Zhang;Takashi Yoshino;Chengcheng Zhao.(2019).The Effect of Water on Fe‐Mg Interdiffusion Rates in Ringwoodite and Implications for the Electrical Conductivity in the Mantle Transition Zone.Journal of Geophysical Research: Solid Earth,2510-2524. |
MLA | Baohua Zhang;Takashi Yoshino;Chengcheng Zhao."The Effect of Water on Fe‐Mg Interdiffusion Rates in Ringwoodite and Implications for the Electrical Conductivity in the Mantle Transition Zone".Journal of Geophysical Research: Solid Earth (2019):2510-2524. |
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