Cubic calcite and its structural phase transitions

IF 1.2 4区 地球科学 Q4 MATERIALS SCIENCE, MULTIDISCIPLINARY Physics and Chemistry of Minerals Pub Date : 2025-02-14 DOI:10.1007/s00269-024-01306-4
Yang Yang, Yixin Lin, Xiangdong Ding, Christopher J. Howard, Ekhard K. H. Salje
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Abstract

Calcite, CaCO3, has been reported to exist in as many as seven different structural forms. The structure at room temperature and pressure (space group R\(\overline{3 }\)c, ‘Phase I’) was established by Bragg many years ago. A phase transition to a higher temperature phase (space group R\(\overline{3 }\)m, ‘Phase V’) was noted to occur at around 1240 K—this may proceed via an intermediate phase (space group again R\(\overline{3 }\)c, referred to as ‘Phase IV’). These phases differ primarily in the disposition of the CO3 groups. Additional phases are found at higher pressures. We report a para-phase (parent phase, virtual prototype, aristotype) which assists in understanding the different phases, the phase transitions, and especially the domain structures and twin wall boundaries associated with these transitions. Molecular dynamics methods were used to study the temperature evolution of an isothermal-isobaric (NPT) ensemble of some 384,000 atoms. These computations reproduced the features of the known structures in R\(\overline{3 }\)c and R\(\overline{3 }\)m and then, at higher temperature, revealed a structure of the sodium chloride type (space group Fm\(\overline{3 }\)m) in which the entities were the Ca2+ cation and the CO32− anion, this latter with effectively spherical symmetry. On this basis we have upon cooling a necessarily first order ferroelastic transition from cubic Fm\(\overline{3 }\)m to rhombohedral R\(\overline{3 }\)m, computed to occur at a simulated temperature of 1900 K, and a possibly continuous transition from the R\(\overline{3 }\)m to rhombohedral (on a doubled cell) R\(\overline{3 }\)c computed to occur at about 1525 K. The computations also allowed us to follow the domain structure and twin walls as a function of temperature, during both heating and cooling. The structure just below the R\(\overline{3 }\)m to R\(\overline{3 }\)c transition shows strong disorder in the orientation of the CO3 groups, and this may be what is sometimes referred to as Phase IV. The domain structure just below the cubic to rhombohedral transition shows twinning of typical ferroelastic character. The doubling of the cell below the R\(\overline{3 }\)m to rhombohedral (on a doubled cell) R\(\overline{3 }\)c leads to a more complicated twin pattern. Indeed, the different structures can be identified from patterns of twinning. Differences between domain structures obtained on heating and cooling indicate extensive thermal metastabilities.

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来源期刊
Physics and Chemistry of Minerals
Physics and Chemistry of Minerals 地学-材料科学:综合
CiteScore
2.90
自引率
14.30%
发文量
43
审稿时长
3 months
期刊介绍: Physics and Chemistry of Minerals is an international journal devoted to publishing articles and short communications of physical or chemical studies on minerals or solids related to minerals. The aim of the journal is to support competent interdisciplinary work in mineralogy and physics or chemistry. Particular emphasis is placed on applications of modern techniques or new theories and models to interpret atomic structures and physical or chemical properties of minerals. Some subjects of interest are: -Relationships between atomic structure and crystalline state (structures of various states, crystal energies, crystal growth, thermodynamic studies, phase transformations, solid solution, exsolution phenomena, etc.) -General solid state spectroscopy (ultraviolet, visible, infrared, Raman, ESCA, luminescence, X-ray, electron paramagnetic resonance, nuclear magnetic resonance, gamma ray resonance, etc.) -Experimental and theoretical analysis of chemical bonding in minerals (application of crystal field, molecular orbital, band theories, etc.) -Physical properties (magnetic, mechanical, electric, optical, thermodynamic, etc.) -Relations between thermal expansion, compressibility, elastic constants, and fundamental properties of atomic structure, particularly as applied to geophysical problems -Electron microscopy in support of physical and chemical studies -Computational methods in the study of the structure and properties of minerals -Mineral surfaces (experimental methods, structure and properties)
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