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Phase transitions induced by shock compression on a gypsum mineral: X-ray and micro-Raman analysis

机译:通过冲击压缩石膏矿物引起的相变:X射线和显微拉曼分析

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As a part of systematic researches of phase transitions induced by shock compression in phosphates, silicates, germanates and sulfates, in this article we report preliminary results obtained from shock recovery experiments on powders of a gypsum mineral. The shock experiment was performed in a light gas gun until a pressure close to 14GPa reached. The experimental techniques employed to analyze the shock effects on recovered samples were: Scanning Electron Microscopy (SEM), X-ray Powder Diffraction (XRD) and Micro-Raman Spectroscopy (MRS). The SEM observations show a high plasticity in the impacted sample composed mainly by gypsum and bassanite quantified by Rietveld analysis of the XRD. The results indicate the partial dehydration of gypsum as a result of impact. The MRS analysis suggests the presence of micro-mixtures of gypsum, bassanite and anhydrite heterogeneously distributed throughout the recovered sample.
机译:作为对磷酸盐,硅酸盐,锗酸盐和硫酸盐中的冲击压缩引起的相变进行系统研究的一部分,在本文中,我们报告了从石膏矿物粉末的冲击恢复实验中获得的初步结果。在轻型气枪中进行冲击实验,直到达到接近14GPa的压力。用于分析冲击波对回收样品的实验技术为:扫描电子显微镜(SEM),X射线粉末衍射(XRD)和显微拉曼光谱(MRS)。 SEM观察表明,受冲击的样品具有较高的可塑性,该样品主要由XRD的Rietveld分析定量的石膏和重钙铝石组成。结果表明,由于撞击,石膏部分脱水。 MRS分析表明,在回收的样品中存在不均匀分布的石膏,重钙铝石和硬石膏微混合物。

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