High-temperature behavior of axinite-(Mn), kornerupine and leucosphenite

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Abstract

In situ high-temperature powder X-ray diffraction (HTPXRD) and differential scanning calorimetry (DSC) of three natural borosilicates have been performed in the temperature range of 25—1200 °С. Axinite-(Mn) melts incongruently at 900 °С forming anorthite and bustamite. Leucosphenite decomposes at 850 °С to fresnoite and cristobalite. According to DSC data, kornerupine decomposes at 1177 °С and sapphirine, indialite, and spinel were observed as the products of kornerupine heating. The calculation and orientation of thermal expansion tensor have been performed using HTPXRD data. The study showed that the borosilicates expand weakly and almost isotropically. The average volumetric thermal expansion coefficients are 21.3, 22.7, and 32.9 ∙ 10–6 °C–1 for axinite-(Mn), kornerupine, and leucosphenite, respectively. Leucosphenite has a maximum volumetric expansion most likely due to the pronounced layered character of the crystal structure. The least symmetric structure of axinite-(Mn) has the maximal anisotropy of thermal expansion in the temperature range of 600—900 °C. 

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About the authors

Maria G. Krzhizhanovskaya

Saint-Petersburg State University

Author for correspondence.
Email: mariya.krzhizhanovskaya@spbu.ru
ORCID iD: 0000-0002-1380-7458
Scopus Author ID: 6602302951
ResearcherId: K-7045-2013

Assistant Professor of Crystallography Department, Institute of Earth Sciences

Russian Federation, 199034, St. Petersburg, University Emb., 7/9

Vera A. Firsova

Institute of Silicate Chemistry of Russian Academy of Sciences

Email: va_firsova@mail.ru

Senior Scientist

Russian Federation, 199034, St.Petersburg, Makarova Emb, 2

Rimma S. Bubnova

Institute of Silicate Chemistry of Russian Academy of Sciences

Email: rimma_bubnova@mail.ru

Head of Structural Chemistry Lab.

Russian Federation, 199034, St.Petersburg, Makarova Emb, 2

Sergei N. Britvin

Saint-Petersburg State University

Email: sergei.britvin@spbu.ru

Professor, Crystallography Department, Institute of Earth Sciences

Russian Federation, 199034, St. Petersburg, University Emb., 7/9

Olga G. Bubnova

Saint-Petersburg State University

Email: olga.bubnova@spbu.ru

Leading Researcher of XRD center

Russian Federation, 199034, St. Petersburg, University Emb., 7/9

Igor V. Pekov

Moscow State University

Email: igorpekov@mail.ru

Professor, Mineralogy Department, Geological Feculty

Russian Federation, 119991, Москва, Воробьевы горы

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Supplementary files

Supplementary Files
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2. Fig. 1. Thermal behavior of axinite-(Mn): a — HTXRD, б — DSC and TG (for details see text).

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3. Fig. 2. 3D-plot of XRD pattern of leucosphenite depending on temperature.

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4. Fig. 3. Thermal behavior of kornerupine: a — HTXRD, б — DSC and TG (for details see text).

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5. Fig. 4. Temperature dependences of the unit cell parameters of axinite-(Mn) (a), isolated borosilicate anion (б), and the pole figure of thermal expansion coefficients compared to the crystal structure of axinite-(Mn) (в).

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6. Fig. 5. Temperature dependences of the unit cell parameters of leucosphenite (a) and the pole figure of thermal expansion coefficients compared to the ac projection of the crystal structure (б).

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7. Fig. 6. Temperature dependences of the unit cell parameters of kornerupine (a) and the pole figure of thermal expansion coefficients compared to the ab projection of the crystal structure (б).

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