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New Synthetic High-Density Nickel Sulfide: A Plausible Component of the Earth's Core and Terrestrial Planets

机译:新型合成高密度硫化镍:地球核心和陆地行星的合理组成部分

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摘要

New phase Ni_(3-x)S with a structural type of Ni_3P in equilibrium with metallic nickel was synthesized in the subsolidus area of pseudo-binary system Ni-Ni_3S_2 at a temperature of 800℃ and hydrostatic pressure of 20 GPa. This phase is stable at a pressure >9-10 GPa. The structural analogy with the high-density Fe_3S phase allows us to assume the existence of wide area of solid solutions (Fe,Ni)_3S, which should be accounted for in the models of core composition of the Earth and other planets.
机译:在准二元体系Ni-Ni_3S_2的亚固相区,温度为800℃,静水压力为20 GPa的条件下,合成了结构形式为Ni_3P与金属镍平衡的新相Ni_(3-x)S。该相在> 9-10 GPa的压力下稳定。与高密度Fe_3S相的结构相似性使我们可以假设存在宽范围的固溶体(Fe,Ni)_3S,这应该在地球和其他行星的核心成分模型中加以考虑。

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  • 来源
    《Doklady Earth Sciences》 |2010年第2期|P.771-774|共4页
  • 作者单位

    Institute of Experimental Mineralogy, Russian Academy of Sciences, Chernogolovka, Moscow oblast, Russia;

    rnNikolaev Institute of Inorganic Chemistry, Siberian Branch, Russian Academy of Sciences, Russia Bavarian Geoinstitute, Bayreuth, Germany;

    rnBavarian Geoinstitute, Bayreuth, Germany;

    rnBavarian Geoinstitute, Bayreuth, Germany;

    rnBavarian Geoinstitute, Bayreuth, Germany;

    rnBavarian Geoinstitute, Bayreuth, Germany;

    rnBavarian Geoinstitute, Bayreuth, Germany University of Heidelberg, Germany;

    rnInstitute of Experimental Mineralogy, Russian Academy of Sciences, Chernogolovka, Moscow oblast, Russia;

    rnInstitute of Experimental Mineralogy, Russian Academy of Sciences, Chernogolovka, Moscow oblast, Russia;

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