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Biryukov YP, Zinnatullin AL, Levashova IO, Shablinskii AP, Bubnova RS, Vagizov FG, Ugolkov VL, Filatov SK, Pekov IV. Crystal structure refinement, low- and high-temperature X-ray diffraction and Mössbauer spectroscopy study of the oxoborate ludwigite from the Iten'yurginskoe deposit. ACTA CRYSTALLOGRAPHICA SECTION B, STRUCTURAL SCIENCE, CRYSTAL ENGINEERING AND MATERIALS 2023; 79:368-379. [PMID: 37669151 DOI: 10.1107/s2052520623006455] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/15/2023] [Accepted: 07/25/2023] [Indexed: 09/07/2023]
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.
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Affiliation(s)
- Yaroslav P Biryukov
- Institute of Silicate Chemistry of the Russian Academy of Sciences (ISC RAS), Makarova Emb., 2, Saint Petersburg, 199034, Russian Federation
| | - Almaz L Zinnatullin
- Institute of Physics, Kazan Federal University, Kremlyovskaya Str., 18, Kazan, 420008, Russian Federation
| | - Irina O Levashova
- Institute of Silicate Chemistry of the Russian Academy of Sciences (ISC RAS), Makarova Emb., 2, Saint Petersburg, 199034, Russian Federation
| | - Andrey P Shablinskii
- Institute of Silicate Chemistry of the Russian Academy of Sciences (ISC RAS), Makarova Emb., 2, Saint Petersburg, 199034, Russian Federation
| | - Rimma S Bubnova
- Institute of Silicate Chemistry of the Russian Academy of Sciences (ISC RAS), Makarova Emb., 2, Saint Petersburg, 199034, Russian Federation
| | - Farit G Vagizov
- Institute of Physics, Kazan Federal University, Kremlyovskaya Str., 18, Kazan, 420008, Russian Federation
| | - Valery L Ugolkov
- Institute of Silicate Chemistry of the Russian Academy of Sciences (ISC RAS), Makarova Emb., 2, Saint Petersburg, 199034, Russian Federation
| | - Stanislav K Filatov
- Institute of Earth Sciences, Department of Crystallography, Saint Petersburg State University, Universitetskaya Emb., 7/9, Saint Petersburg, 199034, Russian Federation
| | - Igor V Pekov
- Faculty of Geology, Moscow State University, Leninskie Gory, 1, Moscow, 119991, Russian Federation
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Sofronova S, Nazarenko I. Ludwigites: From natural mineral to modern solid solutions. CRYSTAL RESEARCH AND TECHNOLOGY 2017. [DOI: 10.1002/crat.201600338] [Citation(s) in RCA: 12] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/11/2022]
Affiliation(s)
- S. Sofronova
- L.V. Kirensky Institute of Physics; Siberian Branch of Russian Academy of Science; 660036 Krasnoyarsk Russia
| | - I. Nazarenko
- L.V. Kirensky Institute of Physics; Siberian Branch of Russian Academy of Science; 660036 Krasnoyarsk Russia
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