X-ray diffraction and Mössbauer spectroscopy study of oxoborate azoproite (Mg,Fe2+)2(Fe3+,Ti,Mg,Al)O2(BO3): an in situ temperature-dependent investigation (5 ≤ T ≤ 1650 K)

Y. Biryukov, A. Zinnatullin, Irina O. Levashova, A. Shablinskii, M. Cherosov, R. Bubnova, F. Vagizov, M. Krzhizhanovskaya, S. Filatov, V. Shilovskikh, I. Pekov
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引用次数: 1

Abstract

This work is devoted to an investigation of elemental composition, crystal structure and thermal expansion of natural oxoborate azoproite from the Tazheran massif (Siberia, Russia) in the temperature range 5–1650 K. Elemental composition was determined by energy-dispersive X-ray spectroscopy (EDX). Its empirical formula based on five oxygen atoms is (Mg1.81Fe2+ 0.19)∑2.00(Fe3+ 0.36Ti0.26Mg0.26Al0.12)∑1.00O2(BO3). Local environment, oxidation states and ratio of Fe atoms are determined using Mössbauer spectroscopy and compared with EDX and single-crystal X-ray diffraction (SCXRD) data. A refinement of the crystal structure from SCXRD data collected at 293 K was provided for the first time. The structure could be described both in terms of cation- and anion-centered polyhedra. It is composed of vertex- and edge-sharing metal–oxygen [MO6] n − octahedra that form extended zigzag chains along the a axis building up a framework with the [BO3]3− triangles located in its distorted trigonal channels. From the other point of view, there are double chains consisting of oxocentred [OM 4] n + tetrahedra and [OM 5] n + tetragonal pyramids forming six-membered rings with the triangles in its cavities. Four non-equivalent Mn + sites are occupied by cations as follows: M(1) (2a) and M(2) (2d) – Mg, M(3) (4g) – Mg and Fe2+, M(4) (4h) – Fe3+, Ti4+, Mg and Al3+. According to differential scanning calorimetry, low- and high-temperature powder X-ray diffraction (LT- and HT-XRD) data, Mössbauer spectroscopy and magnetometry data (5 ≤ T ≤ 1650 K), there are no phase transitions obtained in the temperature range investigated. However, some anomalies in temperature dependencies of unit-cell parameters caused by a partial Fe2+ → Fe3+ oxidation are found in the range 873–1173 K. Azoproite melts at a temperature higher than 1600 K. Eigenvalues of the thermal expansion tensor are calculated for the oxoborate and thermal expansion is described in comparison with its crystal structure.
氧硼酸偶氮酸盐(Mg,Fe2+)2(Fe3+,Ti,Mg,Al)O2(BO3)的x射线衍射和Mössbauer光谱研究:原位温度依赖性研究(5≤T≤1650 K)
本文研究了俄罗斯西伯利亚塔镇然地块5 ~ 1650 K温度范围内天然氧硼酸盐偶氮proite的元素组成、晶体结构和热膨胀。元素组成由能量色散x射线光谱(EDX)测定。其基于5个氧原子的经验公式为(Mg1.81Fe2+ 0.19)∑2.00(Fe3+ 0.36Ti0.26Mg0.26Al0.12)∑1.00O2(BO3)。利用Mössbauer光谱法测定了局部环境、氧化态和铁原子比例,并与EDX和单晶x射线衍射(SCXRD)数据进行了比较。在293 K下收集的SCXRD数据首次提供了晶体结构的细化。该结构可以用正离子中心多面体和阴离子中心多面体来描述。它由顶点共享和边共享的金属氧[MO6] n -八面体组成,它们沿着a轴形成延伸的之字形链,形成一个框架,[BO3]3 -三角形位于其扭曲的三角形通道中。从另一个角度来看,双链由[OM 4] n +四面体和[OM 5] n +四面体组成,形成六元环,其腔中有三角形。四个不相等的Mn +位置被以下阳离子占据:M(1) (2a)和M(2) (2d) - Mg, M(3) (4g) - Mg和Fe2+, M(4) (4h) - Fe3+, Ti4+, Mg和Al3+。根据差示扫描量热法、低温和高温粉末x射线衍射(LT-和HT-XRD)数据、Mössbauer光谱和磁强计数据(5≤T≤1650 K),在所研究的温度范围内没有得到相变。然而,在873 ~ 1173 K范围内,由Fe2+→Fe3+部分氧化引起的单元胞参数的温度依赖性出现了一些异常。偶氮盐在高于1600k的温度下熔化。计算了氧硼酸盐的热膨胀张量特征值,并将其与晶体结构进行了比较。
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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