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High-pressure phase behavior of SrCO3: an experimental and computational Raman scattering study

机译:SRCO3的高压相行为:实验和计算拉曼散射研究

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The high-pressure phase behavior of strontianite (SrCO3) was both experimentally and theoretically investigated by Raman spectroscopy up to 78 GPa in a diamond anvil cell and density functional theory-based calculations. Our study shows a phase transition between 23.7 and 26.8 GPa during compression from space group Pmcn to post-aragonite SrCO3, which is accompanied by significant changes in the vibrational spectrum. The excellent agreement between the observed and computed Raman frequencies and intensities implies that the high-pressure polymorph has space group Pmmn and contributes to resolving an existing disagreement concerning the correct space group symmetry of this high-pressure polymorph. It is shown that the transition pressure from the aragonite to a post-aragonite phase increases linearly with decreasing cation radius for (Ca, Sr, Ba, Pb) carbonates.
机译:斯特罗尼亚钛矿(SRCO3)的高压相行为在实验和理论上通过拉曼光谱均在金刚石砧座和密度泛函理论的计算中进行了高达78GPa的。 我们的研究表明,在从空间组PMCN压缩到后型SRCO3的压缩期间23.7和26.8GPa之间的相转变,其伴随着振动谱的显着变化。 观察和计算的拉曼频率和强度之间的良好一致意味着高压多晶型物具有空间组PMM,有助于解决关于该高压多晶型物的正确空间组对称性的现有分歧。 结果表明,来自阳离子岩相对于后吡啶岩相的过渡压力随着碳酸酯的降低而线性地增加。

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