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New journal of chemistry, 2019, Vol.43 (44), p.1743-1747
Ort / Verlag
Cambridge: Royal Society of Chemistry
Erscheinungsjahr
2019
Quelle
Alma/SFX Local Collection
Beschreibungen/Notizen
Magnesium (Mg) and iron (Fe) are almost immiscible under ambient conditions; this makes Mg an unusual candidate to be considered as a main light element in the earth's core; on the other hand, recent studies have shown that a significant amount of Mg can be dissolved in Fe to form Fe-Mg compounds under high pressure as high pressure can sufficiently improve the solubility of Mg in Fe. However, the formation mechanism and structures of the Fe-Mg compounds are still unknown to date. Herein, we proposed a series of unexpected Fe-Mg compounds (FeMg
4
, FeMg
3
, FeMg
2
, Fe
2
Mg
3
, FeMg and Fe
2
Mg) using the CALYPSO structure search method in conjunction with first-principles calculations. The results show that valence electrons of the Mg atoms transfer to the Fe atoms under high pressure, leading to the formation of these Fe-Mg compounds. This study represents a significant step forward in the understanding of binary Fe-Mg compounds.
A dynamically and thermodynamically stable Fe-rich compound, Fe
2
Mg, reveals that Mg may be a light element candidate in the earth's inner core.