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Melting of Fe and Fe0.9375Si0.0625 at Earth's core pressures studied using ab initio molecular dynamics

Belonoshko, Anatoly B. (author)
KTH,Kondenserade materiens teori,Tillämpad materialfysik
Rosengren, Anders (author)
KTH,Kondenserade materiens teori
Burakovsky, Leonid (author)
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Preston, Dean L. (author)
Johansson, Börje (author)
Uppsala universitet,KTH,Tillämpad materialfysik,Fysiska institutionen,Condensed Matter Theory Grp
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 (creator_code:org_t)
2009
2009
English.
In: Physical Review B. Condensed Matter and Materials Physics. - 1098-0121 .- 1550-235X. ; 79:22
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • The issue of melting of pure iron and iron alloyed with lighter elements at high pressure is critical to the physics of the Earth. The iron melting curve in the relevant pressure range between 3 and 4 Mbar is reasonably well established from the theoretical point of view. However, so far no one attempted a direct atomistic simulation of iron alloyed with light elements. We investigate here the impact of alloying the body-centered cubic (bcc) Fe with Si. We simulate melting of the bcc Fe and Fe0.9375Si0.0625 alloy by ab initio molecular dynamics. The addition of light elements to the hexagonal-close-packed (hcp) iron is known to depress its melting temperature (T-m). We obtain, in marked contrast, that alloying of bcc Fe with Si does not lead to T-m depression; on the contrary, the T-m slightly increases. This suggests that if Si is a typical impurity in the Earth's inner core, then the stable phase in the core is bcc rather than hcp.

Subject headings

NATURVETENSKAP  -- Fysik (hsv//swe)
NATURAL SCIENCES  -- Physical Sciences (hsv//eng)

Keyword

ab initio calculations
Earth core
high-pressure effects
iron
iron
alloys
melting
molecular dynamics method
silicon alloys
centered-cubic phase
inner-core
in-situ
iron
anisotropy
temperature
transitions
equation
physics
state
Physics

Publication and Content Type

ref (subject category)
art (subject category)

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