Chemistry and mineralogy of earth's mantle. the spin state of iron in Fe³⁺-bearing Mg-perovskite and its crystal chemistry at high pressure

Valence, spin states, and crystallographic sites of Fe in (Mg,Fe)SiO₃perovskite were investigated using energy-domain ⁵⁷Fe-synchrotron Mössbauer spectroscopy and powder X-ray diffraction up to 86 GPa. The volumes of Fe³⁺-bearing perovskite in this study are slightly smaller than those of Mg endmember perovskite. Our Mössbauer data suggest that Fe³⁺prefers A sites coupled with Mg vacancies, which is consistent with previous data at ambient conditions. Fe³⁺in the A site remains in a high-spin state up to 86 GPa, and some fraction of the A site is occupied by Fe²⁺at pressures above 30 GPa. Fe²⁺in the A sites is also in a high-spin state up to 86 GPa. The coupled substitution from Mg²⁺to a highspin state of Fe³⁺and Mg²⁺vacancy would make the volume of perovskite smaller than that of Mg end-member perovskite. If the lower mantle is saturated in silica, perovskite containing high-spin Fe³⁺in A site has a higher density. Such silica oversaturated regions could sink by the density difference.