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Thermal expansion of fluorapophyllite KCa4[Si8O20]F center dot 8H(2)O in the 323-473 K range from X-ray powder diffraction data

机译:从X射线粉末衍射数据可知,氟皂石KCa4 [Si8O20] F中心点8H(2)O在323-473 K范围内的热膨胀

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Thermal expansion of fluorapophyllite KCa4[Si8O20]F center dot 8H(2)O has been analysed in the 323-473 K thermal range by laboratory parallel-beam transmission X-ray powder diffraction. Thermal expansion is markedly anisotropic as indicated by (alpha) over bar (alpha) of 2.205(13).10(-5) and (alpha) over bar (c) of 4.98(15).10(-6). Very minor variations of relevant bond distances are observed during heating. Anisotropy of thermal expansion has been attributed to the fact that the mean plane passing through Ca,O(4),K has a prevalent component along the (001).
机译:通过实验室平行光束透射X射线粉末衍射在323-473 K的热范围内分析了氟水杨石KCa4 [Si8O20] F中心点8H(2)O的热膨胀。热膨胀具有明显的各向异性,如α超过2.205(13).10(-5)的α和α(c)超过4.98(15).10(-6)的α所示。在加热过程中观察到相关键距的很小变化。热膨胀的各向异性归因于以下事实:穿过Ca,O(4),K的平均平面沿(001)具有主要成分。

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