K[(CuII,MnII,MnIII)2(TeO3)3]∙2H2O,第一个基于jahn - teller扭曲框架的zemanite型结构

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Mineralogy and Petrology Pub Date : 2023-03-18 DOI:10.1007/s00710-022-00808-9
Felix Eder, Ronald Miletich, Matthias Weil
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引用次数: 2

摘要

在温度≤220℃的水热条件下,以k20 - mno - cuo - teo2体系为原料,在过浓碱性水溶液中合成了K[(CuII,MnII,MnIII)2(TeO3)3]·2H2O单晶。用单晶x射线衍射方法研究了亚面体单晶。这种新型菱铁矿代表的晶体结构为单斜双上部结构。单位胞体积的加倍伴随着六边形到单斜对称性的减少,导致具有单个晶体域的三重孪晶,遵循空间群对称P21。位点占用因子的改进和键价的评估表明,二价和三价阳离子在八面体配位的M位点上的分布比例(CuII + MnII):MnIII接近1:1。基于对阳离子大小和单个键价和的争论,可以假设cui1 - xmniiix和MnIIx - mnii1 - x在四个M位点中的每两个上的分布,x在~ 0.14和~ 0.50之间。通道内的K+阳离子和H2O分子位于偏离通道中心轴的位置。与大多数其他已知的锌锰矿型相相比,框架外原子显示出完全的占位,而不是无序的。通道内容的分布支持周围框架的各向异性变形,这遵循框架内八面体协调M位点的Jahn-Teller畸变所需的局部对称性减少。变形河道的排列可以理解为现存上层建筑的起源。
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K[(CuII,MnII,MnIII)2(TeO3)3]∙2H2O, the first zemannite-type structure based on a Jahn-Teller-distorted framework

Synthetic single crystals of K[(CuII,MnII,MnIII)2(TeO3)3]·2H2O were obtained from an overconcentrated alkaline aqueous solution in the system K2O-MnO-CuO-TeO2 under hydrothermal conditions at T ≤ 220 °C. Subeuhedral single crystals have been investigated by means of single-crystal X-ray diffraction. The crystal structure of this new zemannite-type representative adopts a monoclinic twofold superstructure. The doubling of the unit-cell volume is accompanied by a hexagonal-to-monoclinic symmetry reduction, resulting in threefold twinning with individual crystal domains following the space group symmetry P21. Refinements of site-occupation factors and the evaluation of bond valences suggest a distribution of di- and trivalent cations at the octahedrally coordinated M sites with a ratio (CuII + MnII):MnIII approximating 1:1. Based on arguments about the cation sizes and the individual bond valence sums, a distribution of CuII1–xMnIIIx and MnIIx MnIII1–x at each two of the four M sites can be assumed with x between ~ 0.14 and ~ 0.50. The K+ cations and H2O molecules inside the channels are located off the central channel axis. In contrast to most other known zemannite-type phases, the extra-framework atoms show full occupancies and are not disordered. The distribution of the channel contents supports the anisotropic deformation of the surrounding framework, which follows the local symmetry reduction as required for the Jahn-Teller distortion of the octahedrally coordinated M sites within the framework. The arrangement of the deformed channels can be understood as the origin of the existing superstructure.

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来源期刊
Mineralogy and Petrology
Mineralogy and Petrology 地学-地球化学与地球物理
CiteScore
2.60
自引率
0.00%
发文量
0
审稿时长
1 months
期刊介绍: Mineralogy and Petrology welcomes manuscripts from the classical fields of mineralogy, igneous and metamorphic petrology, geochemistry, crystallography, as well as their applications in academic experimentation and research, materials science and engineering, for technology, industry, environment, or society. The journal strongly promotes cross-fertilization among Earth-scientific and applied materials-oriented disciplines. Purely descriptive manuscripts on regional topics will not be considered. Mineralogy and Petrology was founded in 1872 by Gustav Tschermak as "Mineralogische und Petrographische Mittheilungen". It is one of Europe''s oldest geoscience journals. Former editors include outstanding names such as Gustav Tschermak, Friedrich Becke, Felix Machatschki, Josef Zemann, and Eugen F. Stumpfl.
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