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Laboratory parallel-beam transmission X-ray powder diffraction investigation of the thermal behavior of calcite: comparison with X-ray single-crystal and synchrotron powder diffraction data

机译:方解石热行为的实验室平行光束透射X射线粉末衍射研究:与X射线单晶和同步加速器粉末衍射数据的比较

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摘要

Thermal behavior of calcite has been analyzed in the 303-1098 K thermal range by laboratory parallel-beam transmission X-ray powder diffraction. Present results provide a clear indication of the possibility to extract high-quality structural data from such instrumental set up. Such quality has been proved to be at the same level of a mid eighties X-ray single crystal investigation. Analysis of the spontaneous strain e_(33) provides a critical exponent β of 0.2499(5) consistent with the value of ? expected for a tricritical behavior. Structure refinements seemengly support the Ising model of disorder.
机译:方解石的热行为已通过实验室平行光束透射X射线粉末衍射在303-1098 K温度范围内进行了分析。目前的结果清楚地表明了从这种仪器设置中提取高质量结构数据的可能性。这种质量已被证明与80年代中期X射线单晶研究处于同一水平。对自发应变e_(33)的分析提供了0.2499(5)的临界指数β,与?的值一致。预期具有三重性行为。结构改进似乎支持无序的伊辛模型。

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