Coupled (H+,M3+) substitutions in forsterite

Feiwu Zhang, Kate Wright

Research output: Contribution to journalArticle

14 Citations (Scopus)

Abstract

Coupled substitutions involving hydrogen plus trivalent elements (Al, Eu, Fe, Ga, Gd, Lu, Mn, Nd, Pu, Sc, Y and Yb) in forsterite (Mg2SiO4) are studied using atomistic simulation methods. Incorporation of hydrogen is energetically favourable when included in the forsterite lattice as hydroxyl groups (OH-) at O3 sites while the trivalent cations replace either magnesium or silicon. Our calculations show a strong dependence on the ionic radius of the impurity species and some variation with pressure. There are also significant structural distortions around the impurity defects. At low pressure (0GPa), the smaller trivalent cations, (e.g. Al, Fe, Mn and Ga) substitute into forsterite by replacing Si as: MSi '+OHO3 The larger trivalent cations (e.g. Eu, Gd, Lu, Nd, Pu, Y and Yb) however, replace Mg at the M2 site coupled with an Mg1 vacancy as described by VMg1 +MMg2 +OHO3 At 12GPa, the large cations are more stable at Mg1 relative to Mg2, but both are predicted to be less stable than configurations associated with Si vacancies. The trivalent ionic radius has a significant effect on the H incorporation mechanism, however, the high formation energy of Si vacancies suggests that the presence of H in forsterite could inhibit incorporation of these elements, particularly at high pressure.

Original languageEnglish
Pages (from-to)5958-5965
Number of pages8
JournalGeochimica et Cosmochimica Acta
Volume74
Issue number20
DOIs
Publication statusPublished - 1 Oct 2010
Externally publishedYes

Fingerprint Dive into the research topics of 'Coupled (H<sup>+</sup>,M<sup>3+</sup>) substitutions in forsterite'. Together they form a unique fingerprint.

Cite this