Encyclopedia of Astrobiology

2011 Edition
| Editors: Muriel Gargaud, Ricardo Amils, José Cernicharo Quintanilla, Henderson James (Jim) CleavesII, William M. Irvine, Daniele L. Pinti, Michel Viso

Siderophile Elements

  • Francis AlbaredeEmail author
Reference work entry
DOI: https://doi.org/10.1007/978-3-642-11274-4_1445

Definition

In the Berzelius–Goldschmidt classification, siderophile elements alloy with metallic iron (sideros), most notably in planetary cores. Transition elements such as Ni, Co, Mn, Mo, Au, and the Platinum-Group Elements (Os, Pd, Pt, Re, Rh, Ru) are highly siderophilic. Under reducing conditions, carbon, silicon, and phosphorus become moderately siderophilic. Likewise, under high pressure, some  lithophile elements tend to fractionate into the core and become siderophilic. The question of which elements behave in this way is hotly debated for K, Pb, and Nb for the implication it has on the evolution of planetary interiors.

See also

Copyright information

© Springer-Verlag Berlin Heidelberg 2011

Authors and Affiliations

  1. 1.Ecole Normale Supérieure de LyonLyon Cedex 7France