Thermoelasticity of Fe$^{3+}$- and Al-bearing bridgmanite
Gaurav Shukla, Matteo Cococcioni, Renata M. Wentzcovitch

TL;DR
This study uses ab initio calculations to explore how Fe$^{3+}$ and Al substitutions affect the thermoelastic properties of bridgmanite, revealing spin transition effects and implications for Earth's mantle elasticity.
Contribution
It provides detailed insights into the thermoelastic behavior of Fe$^{3+}$- and Al-bearing bridgmanite under mantle conditions, including spin crossover effects and substitution impacts.
Findings
Spin crossover causes elastic anomalies in Fe$^{3+}$-bearing bridgmanite.
Aluminum presence suppresses elastic anomalies associated with Fe$^{3+}$ spin transition.
Elastic properties of Fe$^{3+}$ and Al co-substituted bridgmanite resemble those of (Mg,Fe$^{2+}$)SiO$_3$ under mantle conditions.
Abstract
We report \textit{ab initio} (LDA + U) calculations of thermoelastic properties of ferric iron (Fe)- and aluminum (Al)-bearing bridgmanite (MgSiO perovskite), the main Earth forming phase, at relevant pressure and temperature conditions and compositions. Three coupled substitutions, namely, [Al]-[Al], [Fe]-[Fe], and [Fe]-[Al] have been investigated. Aggregate elastic moduli and sound velocities are successfully compared with limited experimental data available. In the case of the [Fe]-[Fe] substitution, the high-spin (S=5/2) to low-spin (S=1/2) crossover in [Fe] induces a volume collapse and elastic anomalies across the transition region. However, the associated anomalies should disappear in the presence of aluminum in the most favorable substitution, i.e.,…
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Taxonomy
TopicsHigh-pressure geophysics and materials · Thermal Expansion and Ionic Conductivity · Intermetallics and Advanced Alloy Properties
