首页> 外文期刊>The American mineralogist >The structure of monohydrocalcite and the phase composition of the beachrock deposits of Lake Butler and Lake Fellmongery, South Australia
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The structure of monohydrocalcite and the phase composition of the beachrock deposits of Lake Butler and Lake Fellmongery, South Australia

机译:南澳大利亚州巴特勒湖和费尔蒙格利湖的单方解石结构和相岩沉积物的相组成

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摘要

Samples of beachrock from Lakes Butler and Fellmongery, near Robe, South Australia, were examined by neutron and X-ray powder diffraction. Considerable variation in phase composition was observed, although all samples possessed monohydrocalcite, calcite, aragonite, and magnesian-calcite. The Rietveld refinement of the structure of monohydrocalcite showed significant changes in the orientation of water molecules and a major change in the orientation of a carbonate group with respect to the currently accepted structure. The current refinement shows that the hydrogen-bonding structure consists of three distinct networks, with each of the three carbonate groups being bonded to a single water molecule via one linear and one bifurcated hydrogen bond.
机译:通过中子和X射线粉末衍射检查了南澳大利亚州罗伯附近的巴特勒湖和费尔蒙格利湖的滩涂样品。尽管所有样品均具有单氢方解石,方解石,文石和镁方解石,但观察到相组成的变化很大。单氢方解石结构的Rietveld细化显示,相对于目前公认的结构,水分子的取向发生了显着变化,而碳酸盐基团的取向发生了重大变化。当前的改进表明,氢键结构由三个不同的网络组成,三个碳酸酯基团的每一个均通过一个线性和一个分叉的氢键与一个水分子键合。

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