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首页> 外文期刊>Journal of Mineralogical and Petrological Sciences >Protoenstatite in MgSiO_3 samples prepared by conventional solid state reaction
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Protoenstatite in MgSiO_3 samples prepared by conventional solid state reaction

机译:传统固相反应制备MgSiO_3样品中的原生钙钛矿

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Enstatite (MgSiO_3) sample was prepared by conventional solid state reaction at 1500℃, followed by cooling to ambient temperature with different cooling rates (0.04-500 ℃/s). Quantitative analysis of enstatite phases in the samples by Rietveld refinement and ~(29)Si MAS NMR revealed that a large amount of metastable protoenstatite (30-40 mol%) along with clinoenstatite was preserved in all samples. The presence of protoenstatite was also confirmed by micro-Raman spectroscopy. The crystal structures of protoenstatite and clinoenstatite at room temperature were refined using the Rietveld method, and were essentially the same as those reported by previous studies. As the solid state reaction method is commonly used to prepare synthetic clinoenstatite, the present result implies that the 'clinoenstatite' starting materials used in previous phase equilibrium studies of MgSiO_3 pyroxene might contain overlooked protoenstatite, which could affect the interpretation for phase transition and thus those results should be reexamined.
机译:通过常规固相反应在1500℃下制备顽辉石(MgSiO_3)样品,然后以不同的冷却速率(0.04-500℃/ s)冷却至环境温度。通过Rietveld精炼和〜(29)Si MAS NMR对样品中的顽辉石相进行定量分析,结果表明所有样品中均保留了大量亚稳态的原生钙钛石(30-40 mol%)。微型拉曼光谱法也证实了原生钙钛矿的存在。使用Rietveld方法在室温下对原生钙钛矿和斜硅钙钛矿的晶体结构进行了精炼,并且与先前研究报道的晶体结构基本相同。由于通常采用固态反应方法制备合成的斜长统钙长石,因此目前的结果表明,以前的MgSiO_3辉石相平衡研究中使用的“斜长辉石”起始原料可能含有被忽略的原长辉石,这可能会影响相变的解释,因此结果应重新检查。

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