Thermal equation of state and spin crossover of (Fe2+, Fe3+)-bearing Al-Phase D
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下载链接：
https://doi.esrf.fr/10.15151/ESRF-ES-1838724332
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资源简介：
Hydrous silicate phase D is considered to be a potentially important carrier and reservoir in Earth’s deep interior. The experiments aim to investigate the crystal structural evolution, thermal equation of state, spin state of iron, and hydrogen bond configuration in (Fe2+, Fe3+)-bearing Al-Phase D utilizing the Single-Crystal X-ray diffraction and Synchrotron Mössbauer Source spectroscopy at high pressure-temperature conditions (up to 80 GPa and 1200 K), and to determine their potential influences on the properties of the Earth’s deep interior.
提供机构：
China University of Geosciences, State Key Laboratory of Geological Processes, 388 Lumo Road, Hongshan District, Wuhan City, 430074 Wuhan, China; Universitaet Bayreuth, Bayerisches Geoinstitut, Universitaetsstrasse 30, 95440 Bayreuth, Germany; CNRS UMR 5306, Institut Lumiere Matiere, Université Claude Bernard Lyon 1 Domaine Sci, Entifique De La Doua Bâtiment Kastler, 10 Rue, 69622 Lyon, France; University of Muenster, Institut für Mineralogie, Corrensstrasse 24, 48149 Muenster, Germany; Institute of Physics Academy of Science China, Songshan Lake Materials Laborary, Building A1, Innovation City Songshan Lake, 523808 Dongguan, China; ESRF, 71 avenue des Martyrs, CS 40220, 38043 Grenoble Cedex 9, France
创建时间：
2027-01-01
