Fedotovite k2cu30o (SO4)3和Piypite k4cu40o (SO4)4·(Na,Cu)Cl的热膨胀

IF 0.8 4区材料科学 Q4 MATERIALS SCIENCE, CERAMICS

Glass Physics and Chemistry Pub Date : 2023-08-14 DOI:10.1134/S1087659623600333

A. P. Shablinskii, S. K. Filatov, Y. P. Biryukov, A. A. Yuriev, L. P. Vergasova

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引用次数: 0

摘要

本文介绍了fedotovite k2cu30o (SO4)3和piypite k4cu40o (SO4)4∙(Na,Cu)Cl矿物在较宽温度范围内的热行为研究结果。在室温下，完整型斑铁矿试样的晶体结构得到了细化。描述了晶体结构对矿物热膨胀机理的影响。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Thermal Expansion of Fedotovite K2Cu3O(SO4)3 and Piypite K4Cu4O(SO4)4·(Na,Cu)Cl

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Thermal Expansion of Fedotovite K2Cu3O(SO4)3 and Piypite K4Cu4O(SO4)4·(Na,Cu)Cl

This paper presents the results of a study of the thermal behavior of fedotovite K₂Cu₃O(SO₄)₃ and piypite K₄Cu₄O(SO₄)₄∙(Na,Cu)Cl minerals in a wide temperature range. The crystal structure of the holotype piypite specimen is refined at room temperature. The mechanisms of thermal expansion of minerals depending on the crystal structure are described.

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来源期刊

Glass Physics and Chemistry 工程技术-材料科学：硅酸盐

CiteScore

1.20

自引率

14.30%

发文量

审稿时长

6-12 weeks

期刊介绍： Glass Physics and Chemistry presents results of research on the inorganic and physical chemistry of glass, ceramics, nanoparticles, nanocomposites, and high-temperature oxides and coatings. The journal welcomes manuscripts from all countries in the English or Russian language.