Crystal structure refinement, low- and high-temperature X-ray diffraction and Mössbauer spectroscopy study of the oxoborate ludwigite from the Iten'yurginskoe deposit.

IF 1.3 3区 化学 Q3 CHEMISTRY, MULTIDISCIPLINARY
Yaroslav P Biryukov, Almaz L Zinnatullin, Irina O Levashova, Andrey P Shablinskii, Rimma S Bubnova, Farit G Vagizov, Valery L Ugolkov, Stanislav K Filatov, Igor V Pekov
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引用次数: 0

Abstract

This paper reports an investigation of the chemistry, crystal structure refinement and thermal behavior (80-1650 K) of ludwigite from the Iten'yurginskoe deposit (Eastern Chukotka, Russia). Its chemical composition was determined by electron microprobe analysis, giving an empirical formula (Mg1.70Fe2+0.29Mn0.01)Σ2.00(Fe3+0.90Al0.08Mg0.02)Σ1.00O2(BO3). A refinement of the crystal structure from single-crystal X-ray diffraction data (SCXRD) was provided for the first time for ludwigite from this deposit (R = 0.047). The structure can be described as a framework composed of [MO6]n- octahedra and isolated [BO3]3- triangles located in triangular interstices of the framework. Based on a comprehensive analysis of SCXRD and Mössbauer spectroscopy data, the M1 site is occupied by Mg, M2 and M3 by Mg and Fe2+, M4 by Fe3+, Mg and Al. There are also oxo-centered [O4M4]n+ and [O2M5]n+ polyhedra building up a framework with the [BO3]3- triangles located in its hexagonal interstices. No indications of magnetic ordering are found in the temperature range investigated. The Fe2+ → Fe3+ oxidation occurs above 600 K, and is accompanied by a decrease of the unit-cell parameters and subsequent incomplete solid-phase decomposition with the formation of hematite, warwickite and magnetite. The mineral melts at temperatures above 1582 K. The thermal expansion of ludwigite is slightly anisotropic, which is explained by a dense packing of the [MO6]n- octahedra as well as a virtually perpendicular orientation of the oxo-centered double chains to each other. At room temperature, maximum expansion is along the c axis (αc = 9.1 × 10-6 K-1) and minimum expansion is in the ab plane (αa = 8.6 × 10-6, αb = 7.6 × 10-6 K-1), which is due to the preferred orientation of the [BO3]3- triangles. A comparison of the thermal behavior of three oxoborates of the ludwigite group, namely azoproite (Mg,Fe2+)2(Fe3+,Ti,Mg,Al)O2(BO3), vonsenite (Fe2+,Mg)2(Fe3+,Mn2+,Sn,Al)O2(BO3) and ludwigite (Mg,Fe2+,Mn)2(Fe3+,Al,Mg)O2(BO3), is provided.

Abstract Image

Iten'yurginskoe矿床含氧硼酸盐的晶体结构细化、低温和高温X射线衍射及穆斯堡尔谱研究。
本文报道了(80-1650 K) 来自Iten'yurginskoe矿床(俄罗斯楚科奇东部)的绿柱石。用电子探针分析测定其化学成分,给出了经验公式(Mg1.70Fe2+0.29Mn0.01)∑2.00(Fe3+0.90Al0.08Mg0.02)∑1.00O2框架的空隙。根据SCXRD和Mössbauer谱数据的综合分析,M1位点被Mg占据,M2和M3被Mg和Fe2+占据,M4被Fe3+、Mg和Al占据。此外,以氧为中心的[O4M4]n+和[O2M5]n+多面体在其六边形间隙中形成了[BO3]3-三角形的骨架。在所研究的温度范围内没有发现磁性有序的迹象。Fe2+→ Fe3+氧化发生在600以上 K、 并伴随着晶胞参数的降低和随后的不完全固相分解,形成赤铁矿、沃里克石和磁铁矿。这种矿物在1582以上的温度下熔化 K.菱铁矿的热膨胀是轻微的各向异性,这可以通过[MO6]n-八面体的致密堆积以及氧中心双链彼此几乎垂直的取向来解释。在室温下,最大膨胀沿c轴(αc=9.1×10-6 K-1),最小膨胀在ab平面(αa=8.6×10-6,αb=7.6×10-6 K-1),这是由于[BO3]3-三角形的优选取向。提供了三种硼镁石族的氧代硼酸盐的热行为的比较,即丙戊酸(Mg,Fe2+)2(Fe3+,Ti,Mg,Al)O2(BO3)、钒酸盐(Fe2+,Mg)2(Fe 3+,Mn2+,Sn,Al。
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来源期刊
Acta crystallographica Section B, Structural science, crystal engineering and materials
Acta crystallographica Section B, Structural science, crystal engineering and materials CHEMISTRY, MULTIDISCIPLINARYCRYSTALLOGRAPH-CRYSTALLOGRAPHY
CiteScore
3.60
自引率
5.30%
发文量
0
期刊介绍: Acta Crystallographica Section B: Structural Science, Crystal Engineering and Materials publishes scientific articles related to the structural science of compounds and materials in the widest sense. Knowledge of the arrangements of atoms, including their temporal variations and dependencies on temperature and pressure, is often the key to understanding physical and chemical phenomena and is crucial for the design of new materials and supramolecular devices. Acta Crystallographica B is the forum for the publication of such contributions. Scientific developments based on experimental studies as well as those based on theoretical approaches, including crystal-structure prediction, structure-property relations and the use of databases of crystal structures, are published.
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