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首页> 外文期刊>Journal of Materials Science >Solid solutions between ettringite, Ca6Al2(SO4)(3)(OH)(12)center dot 26H(2)O, and thaumasite, Ca3SiSO4CO3(OH)(6)center dot 12H(2)O
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Solid solutions between ettringite, Ca6Al2(SO4)(3)(OH)(12)center dot 26H(2)O, and thaumasite, Ca3SiSO4CO3(OH)(6)center dot 12H(2)O

机译:钙矾石,Ca6Al2(SO4)(3)(OH)(12)中心点26H(2)O和高岭土Ca3SiSO4CO3(OH)(6)中心点12H(2)O之间的固溶体

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摘要

A series of solid solution phases between ettringite, Ca6Al2(SO4)(3)(OH)(12). 26H(2)O, and thaumasite, Ca3SiSO4CO3(OH)(6). 12H(2)O, have been prepared and analysed by X-ray powder diffraction and full pattern fitting. Solid solutions were shown to exist with both the ettringite structure (space group P31c) and the thaumasite structure (space group P6(3), c-axis halved). A possible discontinuity was identified, characterised by a gap in the a-dimension of the solid solution phases produced. This discontinuity is believed to correspond to a switch between the ettringite space group and the thaumasite space group. It is suggested that any discontinuity in the solid solution is caused by differences in the hydrogen bonding of the two structures. (C) 2000 Kluwer Academic Publishers. [References: 18]
机译:钙矾石Ca6Al2(SO4)(3)(OH)(12)之间的一系列固溶相。 26H(2)O和高岭土Ca3SiSO4CO3(OH)(6)。已准备好12H(2)O,并通过X射线粉末衍射和全图拟合进行了分析。固溶体显示既有钙矾石结构(空间群P31c)也有硅铝石结构(空间群P6(3),c轴减半)同时存在。确定了可能的不连续性,其特征在于所产生的固溶体相的a尺寸间隙。认为该不连续性对应于钙矾石空间群和硫马石空间群之间的转换。建议固溶体中的任何不连续性是由两个结构的氢键的差异引起的。 (C)2000 Kluwer学术出版社。 [参考:18]

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