Anomalous thermodynamic properties in ferropericlase throughout its spin crossover transition
Contribuinte(s) |
UNIVERSIDADE DE SÃO PAULO |
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Data(s) |
17/04/2012
17/04/2012
2009
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Resumo |
The thermodynamics properties of ferropericlase (Mg(1-x)Fe(x)O where x=0.1875) (Fp) throughout its spin crossover were investigated by first principles. Fp was treated as an ideal solid solution of pure high-spin and low-spin states. The Gibbs free energies of the pure states were addressed using the LDA+U method. A vibrational virtual-crystal model was developed to address the vibrational properties of the pure spin cases and used in conjunction with quasiharmonic theory to compute their vibrational free energies. The thermodynamics properties of Fp display significant anomalies that should be typical of spin crossover systems in general. In Fp, in particular, they are fundamental for understanding the state of earth's interior, where the pressure and temperature conditions of the crossover are realized. National Science Foundation NSF[EAR 0635990] National Science Foundation NSF[DMR 0325218] National Science Foundation NSF[ATM 0428774] |
Identificador |
PHYSICAL REVIEW B, v.80, n.1, 2009 1098-0121 http://producao.usp.br/handle/BDPI/14699 10.1103/PhysRevB.80.014409 |
Idioma(s) |
eng |
Publicador |
AMER PHYSICAL SOC |
Relação |
Physical Review B |
Direitos |
restrictedAccess Copyright AMER PHYSICAL SOC |
Palavras-Chave | #ab initio calculations #density functional theory #Earth structure #free energy #magnesium compounds #vibrational modes #EARTHS LOWER MANTLE #THERMOELASTIC PROPERTIES #AB-INITIO #IRON #(MG,FE)O #TEMPERATURE #DIFFRACTION #PEROVSKITE #ALLOYS #MGO #Physics, Condensed Matter |
Tipo |
article original article publishedVersion |