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High-pressure high temperature 57Fe Mössbauer spectroscopy in laser-heated diamond anvil cells: Applications for the mineralogy of Earths´s lower mantle and core

High-pressure high temperature 57Fe Mössbauer spectroscopy in laser-heated diamond anvil cells: Applications for the mineralogy of Earths´s lower mantle and core
激光加热金刚石砧室中的高压高温 57Fe 穆斯堡尔光谱:在地球下地幔和地核矿物学中的应用
批准号:
24797886
负责人:
Privatdozentin Dr. Catherine McCammon
金额:
$0.0万
依托单位国家:
德国
项目类别:
Priority Programmes
财政年份:
2006
资助国家:
德国
项目状态:
已结题
起止时间:
2005-12-31 至 2013-12-31

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中文摘要
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英文摘要
Earth scientists have always been directly concerned with the identity and properties of materials that constitute the Earth. However, as we explore deeper regions of the planet with increasingly sophisticated remote-sensing technology and interpret its history in greater detail for scientific understanding of its mineral and energy resources, it becomes clearer than ever that we must exploit technological advances in high-pressure research to enable in situ studies, with the goal of a full-scale characterisation of the physical and chemical properties of Earth materials at extreme pressures and temperatures. Mössbauer spectroscopy is a powerful tool for such studies, but so far its potential for high pressure and temperature applications has not been exploited. The aim of the proposed project is to design, assemble, commission and make operational a laser heating facility optimised to operate in situ with in-house Mössbauer spectroscopy facilities, which will then be used to study the structures (crystallographic, magnetic, and electronic), phase relations, and chemical reactions of iron-containing Earth materials (ferropericlase, aluminium-bearing magnesium-silicate perovskite and post-perovskite, iron-nickel alloys) at conditions of the Earth¿s lower mantle and core.
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Fe spin transition in the Earth's mantle: insight from X-ray Raman scattering and X-ray absorption spectroscopy
Elastic properties of carbonates at high pressures and temperatures
The effect of pressure, temperature and oxygen fugacity on the stability of subducted carbonates and implications for the deep carbon cycle
Iron-bearing minerals in Earth's lower mantle and core-mantle boundary: Development and application of a synchrotron Mössbauer source
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