Noble gases in silicate perovskite: Solubility, dissolution mechanism and influence on the equation of state

硅酸盐钙钛矿中的稀有气体:溶解度、溶解机制及其对状态方程的影响

基本信息

项目摘要

We have carried out some preliminary experiments suggesting significant noble gas solubility in (Mg,Al)(Si,Al)O3 perovskite, the main constituent of Earth´s lower mantle. Measured argon contents are in the 500 ppm range, but actual solubilities may be much higher, since the samples may not have been saturated with argon. If noble gases were highly soluble in perovskite, this would provide the long-sought reservoir for primitive volatiles in the deep Earth. It would also have implications for high-pressure research in general, since ultrahigh-pressure experiments are usually carried out in diamond cells using a noble gas pressure medium. The inferred solubilities are high enough to affect equations of state and the location of phase boundaries. In this project, (i) the solubilities of argon and xenon in silicate perovskite shall be systematically studied in multi-anvil and diamond anvil cell experiments (ii) the effect of argon in the perovskite on the equation of state shall be studied by in-situ X-ray diffraction (iii) the substitution mechanism of noble gases in silicate perovskite shall be investigated by ab-initio modeling.
我们已经进行了一些初步的实验,表明在地球下地幔的主要成分(Mg,Al)(Si,Al)O3钙钛矿中存在显着的惰性气体溶解度。测得的氩含量在500 ppm范围内,但实际溶解度可能高得多,因为样品可能没有被氩饱和。如果稀有气体在钙钛矿中高度可溶,这将为地球深处的原始挥发物提供长期寻找的储存库。这也将对一般的高压研究产生影响,因为超高压实验通常是在使用惰性气体压力介质的金刚石单元中进行的。推断的溶解度是足够高的状态方程和相边界的位置的影响。本项目将采用多砧实验和金刚石对顶砧实验系统研究氩和氙在硅酸盐钙钛矿中的溶解度;采用原位X射线衍射研究钙钛矿中氩对状态方程的影响;采用从头算模型研究稀有气体在硅酸盐钙钛矿中的替代机制。

项目成果

期刊论文数量(1)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
The origin of the terrestrial noble-gas signature
  • DOI:
    10.1038/nature11506
  • 发表时间:
    2012-10
  • 期刊:
  • 影响因子:
    64.8
  • 作者:
    S. Shcheka;H. Keppler
  • 通讯作者:
    S. Shcheka;H. Keppler
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Professor Dr. Hans Keppler其他文献

Professor Dr. Hans Keppler的其他文献

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{{ truncateString('Professor Dr. Hans Keppler', 18)}}的其他基金

High-pressure laboratories of Bayerisches Geoinstitut
巴伐利亚地质研究所高压实验室
  • 批准号:
    324662608
  • 财政年份:
    2017
  • 资助金额:
    --
  • 项目类别:
    Core Facilities
Nitrogen in the deep mantle
地幔深处的氮
  • 批准号:
    299072134
  • 财政年份:
    2016
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Electrical conductivity and dissociation of fluids in crust and mantle
地壳和地幔中流体的电导率和解离
  • 批准号:
    238445505
  • 财政年份:
    2013
  • 资助金额:
    --
  • 项目类别:
    Research Grants
High-pressure laboratories of Bayerisches Geoinstitut
巴伐利亚地质研究所高压实验室
  • 批准号:
    233476351
  • 财政年份:
    2013
  • 资助金额:
    --
  • 项目类别:
    Core Facilities
In-situ observation of the crystallization kinetics and texture evolution of basalts
玄武岩结晶动力学和结构演化的原位观察
  • 批准号:
    129863361
  • 财政年份:
    2009
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Hydrogen in Minerals - HydroMin (FP 21)
矿物质中的氢 - HydroMin (FP 21)
  • 批准号:
    18674428
  • 财政年份:
    2006
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Transition metal ions and water in the Earth´s mantle
地幔中的过渡金属离子和水
  • 批准号:
    5304430
  • 财政年份:
    2001
  • 资助金额:
    --
  • 项目类别:
    Research Grants
Überkritisches Verhalten von wasserhaltigen Silikatschmelzen in der Erdkruste
地壳中含水硅酸盐熔体的超临界行为
  • 批准号:
    5126894
  • 财政年份:
    1998
  • 资助金额:
    --
  • 项目类别:
    Priority Programmes
Subduction fluids and the source of metals in porphyry deposits
俯冲流体和斑岩矿床中的金属来源
  • 批准号:
    519958573
  • 财政年份:
  • 资助金额:
    --
  • 项目类别:
    Priority Programmes
On the stability of organic molecules in subduction zone fluids
俯冲带流体中有机分子的稳定性
  • 批准号:
    500785120
  • 财政年份:
  • 资助金额:
    --
  • 项目类别:
    Research Grants

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