2023
DOI: 10.1016/j.epsl.2023.118449
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Partitioning of silicon and sulfur between solid and liquid iron under core pressures: Constraints on Earth's core composition

Fumiya Sakai,
Kei Hirose,
Guillaume Morard
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Cited by 4 publications
(3 citation statements)
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“…Seismic velocities of the inner core could provide additional constraints to our composition model, but awaiting future studies on the velocity of Fe-S-Si-H alloys under inner core conditions. It should be noted that our composition model assumes that the partition coefficients of various light elements are independent from each other for the composition range relevant to the core, however, pair interactions between light elements in Fe-alloys have been observed for S-Si 53,54 , S-C 55 , C-H 56 , etc. Specifically, recent solid/ liquid partition experiments 54 on the Fe-Si-S system up to 189 GPa have demonstrated that D S decreases considerably with increasing Si content, whereas D Si increases with increasing S content.…”
Section: The Composition Of the Earth's Corementioning
confidence: 99%
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“…Seismic velocities of the inner core could provide additional constraints to our composition model, but awaiting future studies on the velocity of Fe-S-Si-H alloys under inner core conditions. It should be noted that our composition model assumes that the partition coefficients of various light elements are independent from each other for the composition range relevant to the core, however, pair interactions between light elements in Fe-alloys have been observed for S-Si 53,54 , S-C 55 , C-H 56 , etc. Specifically, recent solid/ liquid partition experiments 54 on the Fe-Si-S system up to 189 GPa have demonstrated that D S decreases considerably with increasing Si content, whereas D Si increases with increasing S content.…”
Section: The Composition Of the Earth's Corementioning
confidence: 99%
“…It should be noted that our composition model assumes that the partition coefficients of various light elements are independent from each other for the composition range relevant to the core, however, pair interactions between light elements in Fe-alloys have been observed for S-Si 53,54 , S-C 55 , C-H 56 , etc. Specifically, recent solid/ liquid partition experiments 54 on the Fe-Si-S system up to 189 GPa have demonstrated that D S decreases considerably with increasing Si content, whereas D Si increases with increasing S content. We conducted an additional global search of core compositions by using D Si = 1.1 and Ds = 0.2 extrapolated from ref.…”
Section: The Composition Of the Earth's Corementioning
confidence: 99%
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