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DOI | 10.1016/j.epsl.2021.117088 |
Bridgmanite is nearly dry at the top of the lower mantle | |
Liu Z.; Fei H.; Chen L.; McCammon C.; Wang L.; Liu R.; Wang F.; Liu B.; Katsura T. | |
发表日期 | 2021 |
ISSN | 0012821X |
卷号 | 570 |
英文摘要 | Water solubility in the dominant lower-mantle bridgmanite phase remains controversial. Discrepancies between previous results highlight the importance of the growth high-quality single crystals of bridgmanite under high-pressure and high-temperature conditions corresponding to the top of the lower mantle. Here we synthesized high-quality single crystals of aluminous bridgmanite up to 300 μm in size that were saturated with hydrous melt at 24–26 GPa and 1700–1900 K using both stoichiometric and MgO-rich non-stoichiometric hydrous starting materials in a multi-anvil press. Fourier-transform infrared spectroscopy measurements on clear and pure spots of the single-crystal bridgmanites did not detect any pronounced OH-stretching bands, which were prominent in some earlier studies. The present results support that the lower-mantle dominated bridgmanite is nearly dry, at least at the top of the lower mantle, and that Al3+ and Fe3+ cannot enhance water incorporation into the crystal structure even in the presence of oxygen vacancies. Large partition coefficients of water between transition-zone minerals and dry lower-mantle dominated bridgmanite further support dehydration melting at the top of the lower mantle. We suggest that the majority of the top of a pyrolitic lower mantle is nearly dry based on the dry principal minerals and stability of hydrous phases in this region. © 2021 Elsevier B.V. |
关键词 | bridgmanitedrylower mantlesingle crystalwater solubility |
英文关键词 | Crystal structure; Fourier transform infrared spectroscopy; Magnesia; Single crystals; 'Dry' [; Bridgmanite; High Pressure and High Temperature conditions; High quality single crystals; Hydrous melts; Lower mantle; MgO; Nonstoichiometric; Synthesised; Water solubilities; Solubility; crystal structure; high pressure; high temperature; lower mantle; mineral; solubility |
语种 | 英语 |
来源期刊 | Earth and Planetary Science Letters |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/203194 |
作者单位 | Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, 95440, Germany; State Key Laboratory of Superhard Materials, Jilin University, Changchun, 130012, China; Synergetic Extreme Condition User Facility, Jilin University, Changchun, 130012, China; Center for High Pressure Science & Technology Advanced Research, Beijing, 100094, China |
推荐引用方式 GB/T 7714 | Liu Z.,Fei H.,Chen L.,et al. Bridgmanite is nearly dry at the top of the lower mantle[J],2021,570. |
APA | Liu Z..,Fei H..,Chen L..,McCammon C..,Wang L..,...&Katsura T..(2021).Bridgmanite is nearly dry at the top of the lower mantle.Earth and Planetary Science Letters,570. |
MLA | Liu Z.,et al."Bridgmanite is nearly dry at the top of the lower mantle".Earth and Planetary Science Letters 570(2021). |
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