FIRST PRINCIPLES CALCULATIONS ON THE HIGH-PRESSURE BEHAVIOR OF MAGNESITE

dc.contributor.authorVočadlo L.
dc.date.accessioned2021-01-14T11:13:45Z
dc.date.available2021-01-14T11:13:45Z
dc.date.issued1999
dc.description.abstractThe 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.identifierhttps://elibrary.ru/item.asp?id=31236184
dc.identifier.citationAmerican Mineralogist, 1999, 84, 10, 1627-1631
dc.identifier.issn0003-004X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/23076
dc.titleFIRST PRINCIPLES CALCULATIONS ON THE HIGH-PRESSURE BEHAVIOR OF MAGNESITE
dc.typeСтатья

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