Victoria A. Ginga, Oleg I. Siidra, Vera A. Firsova, Dmitri O. Charkin, Valery L. Ugolkov
{"title":"Phase evolution and temperature-dependent behavior of averievite, Cu5O2(VO4)2(CuCl) and yaroshevskite, Cu9O2(VO4)4Cl2","authors":"Victoria A. Ginga, Oleg I. Siidra, Vera A. Firsova, Dmitri O. Charkin, Valery L. Ugolkov","doi":"10.1007/s00269-022-01213-6","DOIUrl":null,"url":null,"abstract":"<div><p>The exhalation copper oxychloride vanadates attract increasing interest in the fields of both physics and chemistry. Based on the results of HT X-ray diffraction study of synthetic analogs of averievite (<b>1</b>) and yaroshevskite (<b>2</b>) and products of their thermal decomposition in air within the temperature range from 25 °C to 800 °C, it was found that <b>1</b> is stable up to 500 °C, and <b>2</b> is stable up to 480 °C. Both copper oxychloride vanadates expand anisotropically, but exhibit completely different thermal expansion patterns. <b>1</b> demonstrates an expansion in the direction perpendicular to the [O<sub>2</sub>Cu<sub>5</sub>]<sup>6+</sup> layers, but inside the layer, the expansion is isotropic. The thermal expansion of <b>2</b> is much more anisotropic. The compression direction α<sub>33</sub> is close to the <i>c</i> axis, along which the structure tends to align the chains [O<sub>2</sub>Cu<sub>6</sub>]<sup>8+</sup> into positions they would occupy in the layers [O<sub>2</sub>Cu<sub>5</sub>]<sup>6+</sup> of the kagome type which exist in averievite. Meanwhile, the expansion direction <i>α</i><sub>11</sub> is close to the <i>a</i> axis, along which the [O<sub>2</sub>Cu<sub>6</sub>]<sup>8+</sup> chains shift tending to arrange as fragments of [O<sub>2</sub>Cu<sub>5</sub>]<sup>6+</sup> layers. The thermal decomposition proceeds with loss of chlorine (most likely, both via hydrolysis/oxidation and evaporation of copper halides) and formation of copper vanadates.</p></div>","PeriodicalId":20132,"journal":{"name":"Physics and Chemistry of Minerals","volume":"49 9","pages":""},"PeriodicalIF":1.2000,"publicationDate":"2022-08-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physics and Chemistry of Minerals","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s00269-022-01213-6","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"MATERIALS SCIENCE, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
The exhalation copper oxychloride vanadates attract increasing interest in the fields of both physics and chemistry. Based on the results of HT X-ray diffraction study of synthetic analogs of averievite (1) and yaroshevskite (2) and products of their thermal decomposition in air within the temperature range from 25 °C to 800 °C, it was found that 1 is stable up to 500 °C, and 2 is stable up to 480 °C. Both copper oxychloride vanadates expand anisotropically, but exhibit completely different thermal expansion patterns. 1 demonstrates an expansion in the direction perpendicular to the [O2Cu5]6+ layers, but inside the layer, the expansion is isotropic. The thermal expansion of 2 is much more anisotropic. The compression direction α33 is close to the c axis, along which the structure tends to align the chains [O2Cu6]8+ into positions they would occupy in the layers [O2Cu5]6+ of the kagome type which exist in averievite. Meanwhile, the expansion direction α11 is close to the a axis, along which the [O2Cu6]8+ chains shift tending to arrange as fragments of [O2Cu5]6+ layers. The thermal decomposition proceeds with loss of chlorine (most likely, both via hydrolysis/oxidation and evaporation of copper halides) and formation of copper vanadates.
期刊介绍:
Physics and Chemistry of Minerals is an international journal devoted to publishing articles and short communications of physical or chemical studies on minerals or solids related to minerals. The aim of the journal is to support competent interdisciplinary work in mineralogy and physics or chemistry. Particular emphasis is placed on applications of modern techniques or new theories and models to interpret atomic structures and physical or chemical properties of minerals. Some subjects of interest are:
-Relationships between atomic structure and crystalline state (structures of various states, crystal energies, crystal growth, thermodynamic studies, phase transformations, solid solution, exsolution phenomena, etc.)
-General solid state spectroscopy (ultraviolet, visible, infrared, Raman, ESCA, luminescence, X-ray, electron paramagnetic resonance, nuclear magnetic resonance, gamma ray resonance, etc.)
-Experimental and theoretical analysis of chemical bonding in minerals (application of crystal field, molecular orbital, band theories, etc.)
-Physical properties (magnetic, mechanical, electric, optical, thermodynamic, etc.)
-Relations between thermal expansion, compressibility, elastic constants, and fundamental properties of atomic structure, particularly as applied to geophysical problems
-Electron microscopy in support of physical and chemical studies
-Computational methods in the study of the structure and properties of minerals
-Mineral surfaces (experimental methods, structure and properties)