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

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

引用次数: 0

Abstract

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.

Abstract Image

查看原文本刊更多论文

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

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。

求助全文

约1分钟内获得全文求助全文

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.