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首页> 外文期刊>American Mineralogist >Amorphous materials: Properties, structure, and durability: Solubility and solution mechanisms of NOH volatiles in silicate melts at high pressure and temperature--amine groups and hydrogen fugacity
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Amorphous materials: Properties, structure, and durability: Solubility and solution mechanisms of NOH volatiles in silicate melts at high pressure and temperature--amine groups and hydrogen fugacity

机译:非晶态材料:性能,结构和耐用性:高温高压下硅酸盐熔体中NOH挥发物的溶解度和溶解机理-胺基和氢逸度

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摘要

The solubility and solution mechanisms of nitrogen in silicate melts have been examined via nitrogen analyses and vibrational spectroscopy (Raman and FTIR). Pressure (P), temperature (T), hydrogen fugacity (fH2), and silicate melt composition (degree of melt polymerization) were independent variables in experiments in the 1–2.5 GPa pressure and 1300–1500 °C temperature ranges. The fH2 was controlled at values defined by the magnetite-hematite (MH), Mn3O4-MnO (MM), NiO-Ni (NNO), magnetite-wustite (MW), and iron-wustite (IW) buffers together with H2O.
机译:通过氮分析和振动光谱分析(拉曼光谱和傅立叶变换红外光谱),研究了氮在硅酸盐 熔体中的溶解度和溶解机理。压力(P),温度(T), 氢逸度(f H 2 )和硅酸盐熔体成分(度 熔融聚合)是实验 在1–2.5 GPa压力和1300–1500°C温度 范围内的自变量。将f H 2 控制在磁铁矿-赤铁矿 (MH),Mn 3 O < sub> 4 -MnO(MM),NiO-Ni(NNO),磁铁矿-铁矾石(MW), 和铁-铁矾石(IW)缓冲液以及H 2 < / sub> O.

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  • 来源
    《American Mineralogist》 |2008年第12期|1760-1770|共11页
  • 作者单位

    Geophysical Laboratory, Carnegie Institution of Washington, Washington, D.C. 20005, U.S.A.;

    Institute for Study of the Earth’s Interior, Okayama University, Misasa, Tottori 682-0193, Japan;

    Geological Faculty, Moscow State University, Moscow 119899, Russia;

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