TY  - JOUR
A1  - Wang, Lin
A1  - Liu, Zhaodong
A1  - Koizumi, Sanae
A1  - Ballaran, Tiziana Boffa
A1  - Katsura, Tomoo
T1  - Aluminum Components in Bridgmanite Coexisting With Corundum and the CF‐Phase With Temperature
Y1  - 2023-01-22
VL  - 128
IS  - 1
JF  - Journal of Geophysical Research: Solid Earth
DO  - 10.1029/2022JB025739
PB  - 
N2  - Abstract Phase relations in the MgSiO<sub>3</sub>–MgAl<sub>2</sub>O<sub>4</sub>–Al<sub>2</sub>O<sub>3</sub> system are investigated at 27 GPa and 2000–2600 K using a multi‐anvil apparatus. The AlAlO<sub>3</sub> content in the bridgmanite increases from 8.6 to 20.0 mol% with increasing temperature from 2000 to 2600 K, while the MgAlO<sub>2.5</sub> content remains nearly constant, that is, 3–4 mol% at these temperatures. Therefore, the presence of an additional Al‐bearing phase suppresses the oxygen vacancy substitution for Al<sup>3+</sup> in bridgmanite. Conversely, significant amounts of the Al<sub>8/3</sub>O<sub>4</sub> component can be dissolved into the calcium‐ferrite type MgAl<sub>2</sub>O<sub>4</sub>–Mg<sub>2</sub>SiO<sub>4</sub>–Al<sub>8/3</sub>O<sub>4</sub> phase (CF‐phase), implying that the CF‐phase likely contains some amount of vacancies. Therefore, the CF‐phase could also be a candidate mineral for transporting volatiles into the lower mantle. Our results, combined with previous studies on Al‐bearing bridgmanite, indicate that, once the Al per formula unit exceeds 0.12 in bridgmanite, the MgAlO<sub>2.5</sub> content remains nearly constant and the AlAlO<sub>3</sub> component becomes dominant.
N2  - Plain Language Summary: Bridgmanite, the most abundant mineral in the Earth's mantle, can contain Al<sup>3+</sup> in the forms of MgAlO<sub>2.5</sub> and AlAlO<sub>3</sub>. To constrain the substitution mechanism of Al<sup>3+</sup> in bridgmanite, we investigate the MgAlO<sub>2.5</sub> and AlAlO<sub>3</sub> contents in bridgmanite coexisting with a calcium‐ferrite type phase and corundum at different temperatures. Our results demonstrate that the MgAlO<sub>2.5</sub> content reaches saturation (3–4 mol%) when an additional Al‐bearing phase exists in the system.
N2  - Key Points: The MgAlO<sub>2.5</sub> content in bridgmanite remains constant with temperature when bridgmanite coexists with corundum and the CF‐phase. The MgAlO<sub>2.5</sub> content in bridgmanite reaches a solubility of 3–4 mol% when bridgmanite coexists with an additional Al‐bearing phase. A significant amount of the Al<sub>8/3</sub>O<sub>4</sub> component can be dissolved into the CF‐phase.
UR  - http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/11126
ER  -