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- W47100108 abstract "Liquid iron silicate (Fe2SiO4) is an important component of natural silicate liquids appearing in Earth’s interior. The effect of iron in the properties of these melts is a crucial issue, as it displays a high-spin to low-spin transition at high pressures which is accompanied by volume reduction and changes in the optical absorption spectrum. This phenomenon has a major influence on properties like the buoyancy or the thermal conductivity of the melt, and ultimately on the chemical and thermal evolution of our planet. Computer simulations using ab initio methods have proven to be a powerful approach to the study of liquid silicate systems[1,2], although not yet including Fe." @default.
- W47100108 created "2016-06-24" @default.
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- W47100108 date "2010-05-01" @default.
- W47100108 modified "2023-09-26" @default.
- W47100108 title "Spin-polarized Molecular Dynamics simulations of liquid iron silicate at high pressures." @default.
- W47100108 hasPublicationYear "2010" @default.
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