The crystal structure of cesbronite, Cu3TeO4(OH)4: A novel sheet tellurate topology

Owen P. Missen, S. Mills, M. Welch, J. Spratt, M. Rumsey, W. Birch, J. Brugger
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引用次数: 2

Abstract

The crystal structure of cesbronite has been determined using single-crystal X-ray diffraction and supported by electron-microprobe analysis, powder diffraction and Raman spectroscopy. Cesbronite is orthorhombic, space group Cmcm, with a = 2.93172 (16), b = 11.8414 (6), c = 8.6047 (4) A and V = 298.72 (3) A3. The chemical formula of cesbronite has been revised to CuII3TeVIO4(OH)4 from CuII5(TeIVO3)2(OH)6·2H2O. This change has been accepted by the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association, Proposal 17-C. The previously reported oxidation state of tellurium has been shown to be incorrect; the crystal structure, bond valence studies and charge balance clearly show tellurium to be hexavalent. The crystal structure of cesbronite is formed from corrugated sheets of edge-sharing CuO6 and (Cu0.5Te0.5)O6 octahedra. The structure determined here is an average structure that has underlying ordering of Cu and Te at one of the two metal sites, designated as M, which has an occupancy Cu0.5Te0.5. This averaging probably arises from an absence of correlation between adjacent polyhedral sheets, as there are two different hydrogen-bonding configurations linking sheets that are related by a ½a offset. Randomised stacking of these two configurations results in the superposition of Cu and Te and leads to the Cu0.5Te0.5 occupancy of the M site in the average structure. Bond-valence analysis is used to choose the most probable Cu/Te ordering scheme and also to identify protonation sites (OH). The chosen ordering scheme and its associated OH sites are shown to be consistent with the revised chemical formula.
铜青铜矿Cu3TeO4(OH)4的晶体结构:一种新型碲酸盐片状结构
采用单晶x射线衍射、电子探针分析、粉末衍射和拉曼光谱等辅助手段对铜铜矿的晶体结构进行了测定。渗铜矿为正交体,空间群为Cmcm, a = 2.93172 (16), b = 11.8414 (6), c = 8.6047 (4) a, V = 298.72 (3) A3。铜铜矿的化学式由CuII5(TeIVO3)2(OH)6·2H2O修正为CuII3TeVIO4(OH)4。国际矿物学协会新矿物、命名法和分类委员会提案17-C接受了这一改变。以前报道的碲的氧化态已被证明是不正确的;晶体结构、键价研究和电荷平衡清楚地表明碲是六价的。铜铜矿的晶体结构是由边缘共享的CuO6和(Cu0.5Te0.5)O6八面体的波纹片组成。这里确定的结构是一个平均结构,它在两个金属位点之一具有Cu和Te的潜在顺序,指定为M,其占用率为Cu0.5Te0.5。这种平均可能是由于相邻多面体薄片之间缺乏相关性,因为有两种不同的氢键构型连接薄片,它们之间的偏移量为½a。这两种构型的随机叠加导致Cu和Te的叠加,并导致Cu0.5Te0.5占据平均结构中的M位点。键价分析用于选择最可能的Cu/Te排序方案和确定质子化位点(OH)。所选择的排序方案及其相关的羟基位点与修改后的化学式一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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