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Discovery of a hexagonal ultradense hydrous phase in (Fe,Al)OOH.


ABSTRACT: A deep lower-mantle (DLM) water reservoir depends on availability of hydrous minerals which can store and transport water into the DLM without dehydration. Recent discoveries found hydrous phases AlOOH (Z = 2) with a CaCl2-type structure and FeOOH (Z = 4) with a cubic pyrite-type structure stable under the high-pressure-temperature (P-T) conditions of the DLM. Our experiments at 107-136 GPa and 2,400 K have further demonstrated that (Fe,Al)OOH is stabilized in a hexagonal lattice. By combining powder X-ray-diffraction techniques with multigrain indexation, we are able to determine this hexagonal hydrous phase with a = 10.5803(6) Å and c = 2.5897(3) Å at 110 GPa. Hexagonal (Fe,Al)OOH can transform to the cubic pyrite structure at low T with the same density. The hexagonal phase can be formed when ?-AlOOH incorporates FeOOH produced by reaction between water and Fe, which may store a substantial quantity of water in the DLM.

SUBMITTER: Zhang L 

PROVIDER: S-EPMC5866593 | biostudies-literature | 2018 Mar

REPOSITORIES: biostudies-literature

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Discovery of a hexagonal ultradense hydrous phase in (Fe,Al)OOH.

Zhang Li L   Yuan Hongsheng H   Meng Yue Y   Mao Ho-Kwang HK  

Proceedings of the National Academy of Sciences of the United States of America 20180305 12


A deep lower-mantle (DLM) water reservoir depends on availability of hydrous minerals which can store and transport water into the DLM without dehydration. Recent discoveries found hydrous phases AlOOH (<i>Z</i> = 2) with a CaCl<sub>2</sub>-type structure and FeOOH (<i>Z</i> = 4) with a cubic pyrite-type structure stable under the high-pressure-temperature (<i>P-T</i>) conditions of the DLM. Our experiments at 107-136 GPa and 2,400 K have further demonstrated that (Fe,Al)OOH is stabilized in a h  ...[more]

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