FIRST PRINCIPLES CALCULATIONS ON THE HIGH-PRESSURE BEHAVIOR OF MAGNESITE

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dc.contributor.author Vočadlo L.
dc.date.accessioned 2021-01-14T11:13:45Z
dc.date.available 2021-01-14T11:13:45Z
dc.date.issued 1999
dc.identifier https://elibrary.ru/item.asp?id=31236184
dc.identifier.citation American Mineralogist, 1999, 84, 10, 1627-1631
dc.identifier.issn 0003-004X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/23076
dc.description.abstract The equation of state and high pressure (>200 GPa) behavior of magnesite were investigated using first principles pseudopotential calculations based upon density functional theory within the generalized gradient approximation. Using a third-order Birch-Murnahan equation, the calculations predict a bulk modulus K T (0) = 99.0(5) GPa with a delta K/delta P = 4.28(1); with a fixed delta K/delta P = 4, the K T (0) is 111(1) GPa. The results show very good agreement with recent experimental data. The simulations also confirm experimental studies which show that the CO 3 groups are rigid incompressible units while the Mg-O bond length undergoes significant compression. The fully relaxed calculations show no phase transition within this pressure range, and therefore magnesite may be stable throughout the lower mantle subject to temperature destabilization.
dc.title FIRST PRINCIPLES CALCULATIONS ON THE HIGH-PRESSURE BEHAVIOR OF MAGNESITE
dc.type Статья


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