GET > Agenda > Computational modelling of equilibrium Iron isotope fractionation in solid and molten FeS metal alloys

Computational modelling of equilibrium Iron isotope fractionation in solid and molten FeS metal alloys

Séminaire le 05 déc 2019 de 11h00 à 12h00
Salle Pyrénées Salle Pyrénées
Carlos Pinilla

Professeur, Universidad del Norte, Barranquilla, Colombie

Iron is one of the most abundant non-volatile elements in the solar system and plays a major role in planetary formation and differentiation. Information about these processes can be gained by studying the Fe isotope fractionation. In particular, recent attention has been paid to 56Fe/54Fe equilibrium isotope fractionation at conditions relevant to Earth’s core formation and the influence that light elements (O, H, C, Ni, Si and S) have had in this process. Most of these experiments have relied on the study of Fe fractionation from quenched phases (silicate glasses and molten iron alloys). In addition, because of the difficulty of performing these experiments at high pressure, crystalline iron is often used as a proxy form of molten iron at deep conditions. In this work, we use ab-initio computational methods to perform a systematic study of the 56Fe/54Fe equilibrium isotope fractionation in molten and solid FexS(1-x) alloys at conditions of the core formation. These data allow us to discuss the effects of using isotope fractionation data from solid metals as proxy for molten alloys at these conditions. Additionally, we comment on the effects of S concentration on Fe isotope fractionation in liquid systems. Finally, we discuss our findings on view of latest results on 56Fe/54Fe equilibrium isotope fractionation and their relevance for the formation of the Earth’s core.

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