Aplanarity of CO3 groups: a theoretical ­investigation

Density functional theory‐based calculations have been used to demonstrate that the aplanarity of CO groups in some carbonates such as dolomite, CaMg(CO), aragonite, CaCO, and norsethite, BaMg(CO), is a ground‐state property. This distortion stabilizes dolomite by ∼500 J mol. Up to at least 6 GPa, t...

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Veröffentlicht in:Acta crystallographica. Section B, Structural science Structural science, 2000-08, Vol.56 (4), p.648-653
Hauptverfasser: Winkler, Björn, Zemann, Josef, Milman, Victor
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Zemann, Josef
Milman, Victor
description Density functional theory‐based calculations have been used to demonstrate that the aplanarity of CO groups in some carbonates such as dolomite, CaMg(CO), aragonite, CaCO, and norsethite, BaMg(CO), is a ground‐state property. This distortion stabilizes dolomite by ∼500 J mol. Up to at least 6 GPa, the aplanarity of CO groups in dolomite is independent of pressure. In aragonite the aplanarity increases slightly on increasing pressure, while a significant tilting of the CO groups occurs. The calculations do not support previous findings of anomalously low values for the pressure derivative of the bulk moduli, , of aragonite and dolomite. Instead, the computed pressure dependences of the unit‐cell volumes correspond to = 5.0 (5) for aragonite and = 4 (1) for dolomite, when fitted with a third‐order Birch–Murnaghan equation‐of‐state.
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source Crystallography Journals Online; Access via Wiley Online Library
subjects Aplanarity
Carbonates
Condensed matter: structure, mechanical and thermal properties
Density functional theory
Earth sciences
Earth, ocean, space
Exact sciences and technology
High-pressure and shock-wave effects in solids and liquids
Mechanical and acoustical properties of condensed matter
Mineralogy
Non silicates
Physics
title Aplanarity of CO3 groups: a theoretical ­investigation
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