Authors
Guillaume Morard, C Sanloup, B Guillot, G Fiquet, M Mezouar, JP Perrillat, G Garbarino, K Mibe, T Komabayashi, K Funakoshi
Publication date
2008/10
Journal
Journal of Geophysical Research: Solid Earth
Volume
113
Issue
B10
Description
Fe‐S‐Si immiscibility has been investigated using in situ X‐ray methods at high pressure and high temperature. An in situ X‐ray diffraction study of immiscible liquids for P∼5 GPa and T/Tm∼1.1 has been performed, showing differences in structural properties between S‐rich and Si‐rich coexisting liquid phases. Moreover, the respective role of S and Si on Fe alloys has been quantitatively investigated in Fe‐X liquids (X = S, Si) with 20%wt of light elements. The transition from immiscible to miscible textures has been observed in the ternary mixture by in situ X‐ray radiography for the Fe‐18wt%S‐8.5wt%Si (Fe‐28.8at%Si‐11.9at%S) sample composition between 12 and 16 GPa. Closure of the miscibility gap occurs in the same pressure range as the Fe‐S eutectic liquid evolves toward a compact structure. By working within the framework of the hard sphere (HS) fluid commonly used in liquid state theory, we show …
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