角绿石和森林石的晶体结构、XANES和电荷分布研究:au - xagxte2族矿物中Au-Te和Te-Te键的分析。

Ginga Kitahara, A. Yoshiasa, M. Tokuda, M. Nespolo, H. Hongu, Koichi Momma, R. Miyawaki, K. Sugiyama
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引用次数: 1

摘要

介绍了两种金银碲化物[Au1+xAgxTe2,角绿石(x = 0.11-0.13)和sylvanite (x = 0.29-0.31)]的结构细化和XANES研究,并与钙钙石(x = 0.08-0.10)的原型结构进行了比较。众所周知,后者在环境条件下会发生不相称的调制,而克雷纳石和森林石都不存在任何调制。这是由于两种矿物中存在较强的Te-Te键(键距< 2.9 Å),而钙钙石中不存在Te-Te键(键距> 3.2 Å)。在这两种碲化物中,三价金呈轻微扭曲的方形配位,而一价金部分被一价银取代,呈2+2+2配位,对应于扭曲的菱形双棱形。通过计算有效配位数(ECoN),得到了成键和非成键接触的区别。电荷分布(CHARDI)分析对两种碲化物都是令人满意的,但表明[Te3]2阴离子中的Te-Te键不是完全同极性的。因此,这两种碲化物可以被描述为马德隆型化合物,尽管在这两种结构中都存在Te-Te。
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Crystal structure, XANES and charge distribution investigation of krennerite and sylvanite: analysis of Au-Te and Te-Te bonds in Au1-xAgxTe2 group minerals.
The structure refinement and XANES study of two gold-silver-tellurides [Au1+xAgxTe2, krennerite (x = 0.11-0.13) and sylvanite (x = 0.29-0.31)] are presented and the structures are compared with the prototype structure of calaverite (x = 0.08-0.10). Whereas the latter is well known for being incommensurately modulated at ambient conditions, neither krennerite nor sylvanite present any modulation. This is attributed to the presence of relatively strong Te-Te bonds (bond distances < 2.9 Å) in the two minerals, which are absent in calaverite (bond distances > 3.2 Å). In both tellurides, trivalent gold occurs in slightly distorted square planar coordination, whereas monovalent gold, partly substituted by monovalent silver, presents a 2+2+2 coordination, corresponding to distorted rhombic bipyramids. The differentiation between bonding and non-bonding contacts is obtained by computation of the Effective Coordination Number (ECoN). The CHARge DIstribution (CHARDI) analysis is satisfactory for both tellurides but suggests that the Te-Te bond in the [Te3]2- anion is not entirely homopolar. Both tellurides can therefore be described as Madelung-type compounds, despite the presence of Te-Te in both structures.
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