{"title":"K[(CuII,MnII,MnIII)2(TeO3)3]∙2H2O,第一个基于jahn - teller扭曲框架的zemanite型结构","authors":"Felix Eder, Ronald Miletich, Matthias Weil","doi":"10.1007/s00710-022-00808-9","DOIUrl":null,"url":null,"abstract":"<div><p>Synthetic single crystals of K[(Cu<sup>II</sup>,Mn<sup>II</sup>,Mn<sup>III</sup>)<sub>2</sub>(TeO<sub>3</sub>)<sub>3</sub>]·2H<sub>2</sub>O were obtained from an overconcentrated alkaline aqueous solution in the system K<sub>2</sub>O-MnO-CuO-TeO<sub>2</sub> under hydrothermal conditions at <i>T</i> ≤ 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 <i>P</i>2<sub>1</sub>. Refinements of site-occupation factors and the evaluation of bond valences suggest a distribution of di- and trivalent cations at the octahedrally coordinated <i>M</i> sites with a ratio (Cu<sup>II</sup> + Mn<sup>II</sup>):Mn<sup>III</sup> approximating 1:1. Based on arguments about the cation sizes and the individual bond valence sums, a distribution of Cu<sup>II</sup><sub>1–<i>x</i></sub>Mn<sup>III</sup><sub><i>x</i></sub> and Mn<sup>II</sup><sub><i>x</i></sub> Mn<sup>III</sup><sub>1–<i>x</i></sub> at each two of the four <i>M</i> sites can be assumed with <i>x</i> between ~ 0.14 and ~ 0.50. The K<sup>+</sup> cations and H<sub>2</sub>O 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 <i>M</i> sites within the framework. The arrangement of the deformed channels can be understood as the origin of the existing superstructure.</p></div>","PeriodicalId":18547,"journal":{"name":"Mineralogy and Petrology","volume":null,"pages":null},"PeriodicalIF":1.4000,"publicationDate":"2023-03-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s00710-022-00808-9.pdf","citationCount":"2","resultStr":"{\"title\":\"K[(CuII,MnII,MnIII)2(TeO3)3]∙2H2O, the first zemannite-type structure based on a Jahn-Teller-distorted framework\",\"authors\":\"Felix Eder, Ronald Miletich, Matthias Weil\",\"doi\":\"10.1007/s00710-022-00808-9\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Synthetic single crystals of K[(Cu<sup>II</sup>,Mn<sup>II</sup>,Mn<sup>III</sup>)<sub>2</sub>(TeO<sub>3</sub>)<sub>3</sub>]·2H<sub>2</sub>O were obtained from an overconcentrated alkaline aqueous solution in the system K<sub>2</sub>O-MnO-CuO-TeO<sub>2</sub> under hydrothermal conditions at <i>T</i> ≤ 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 <i>P</i>2<sub>1</sub>. Refinements of site-occupation factors and the evaluation of bond valences suggest a distribution of di- and trivalent cations at the octahedrally coordinated <i>M</i> sites with a ratio (Cu<sup>II</sup> + Mn<sup>II</sup>):Mn<sup>III</sup> approximating 1:1. Based on arguments about the cation sizes and the individual bond valence sums, a distribution of Cu<sup>II</sup><sub>1–<i>x</i></sub>Mn<sup>III</sup><sub><i>x</i></sub> and Mn<sup>II</sup><sub><i>x</i></sub> Mn<sup>III</sup><sub>1–<i>x</i></sub> at each two of the four <i>M</i> sites can be assumed with <i>x</i> between ~ 0.14 and ~ 0.50. The K<sup>+</sup> cations and H<sub>2</sub>O 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 <i>M</i> sites within the framework. The arrangement of the deformed channels can be understood as the origin of the existing superstructure.</p></div>\",\"PeriodicalId\":18547,\"journal\":{\"name\":\"Mineralogy and Petrology\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":1.4000,\"publicationDate\":\"2023-03-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://link.springer.com/content/pdf/10.1007/s00710-022-00808-9.pdf\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Mineralogy and Petrology\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://link.springer.com/article/10.1007/s00710-022-00808-9\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Mineralogy and Petrology","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s00710-022-00808-9","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
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.
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.