氧化硼酸盐岩热膨胀的各向异性

IF 0.8 4区材料科学 Q4 MATERIALS SCIENCE, CERAMICS Glass Physics and Chemistry Pub Date : 2023-11-16 DOI:10.1134/S1087659623600503

Y. P. Biryukov, R. S. Bubnova, S. K. Filatov

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引用次数: 0

摘要

本文首次利用低温和高温x射线衍射在93 ~ 513 K的温度范围内对过渡金属氧硼酸盐沃wickite (Fe2+，Mg)Fe3+(BO3)O进行了研究。揭示了其热膨胀具有明显的各向异性。从阳离子多面体和氧中心多面体的作用两方面给出了膨胀机理的结构解释。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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Anisotropy of Thermal Expansion of Oxoborate Warwickite

In this paper, the transition metal oxoborate warwickite (Fe²⁺,Mg)Fe³⁺(BO₃)O is studied for the first time by low- and high-temperature X-ray diffraction in the temperature range from 93 to 513 K. The sharply anisotropic nature of its thermal expansion is revealed. A structural interpretation of the expansion mechanism is given both in terms of the contribution of cationic and oxocentered polyhedra.

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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.