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Influence of content of pressure-transmitting medium on structural evolution of heulandite: Single-crystal X-ray diffraction study

机译:传压介质含量对赤铁矿结构演变的影响:单晶X射线衍射研究

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摘要

The structural evolution of natural heulandite Ca2.90Na2.07Sr0.25K0.16Ba0.06(H2O)(n)[Al8.65Si27.35O72] was studied upon compression in penetrating (water-containing) and non-penetrating (paraffin) media using single-crystal X-ray diffraction data in a diamond-anvil cell. Compression in a water-containing medium results in an additional hydration of heulandite from 23 molecules per unit cell at ambient conditions to approximate to 27 at 3.27 GPa. Water molecules enter both initially vacant and partly occupied positions. Additional hydration stabilizes the crystal structure decreasing its compressibility. (C) 2015 Elsevier Inc. All rights reserved.
机译:研究了天然赤铁矿Ca2.90Na2.07Sr0.25K0.16Ba0.06(H2O)(n)[Al8.65Si27.35O72]的结构演化,方法是在渗透性(含水)和非渗透性(石蜡)介质中压缩金刚石砧盒中的单晶X射线衍射数据。在含水介质中压缩会导致在环境条件下,每单位晶格中的23个分子额外增加水润辉石的水化度,在3.27 GPa时大约达到27。水分子进入最初的空位和部分占据的位置。额外的水合稳定了晶体结构,降低了其可压缩性。 (C)2015 Elsevier Inc.保留所有权利。

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