The Role of Redox on Bridgmanite Crystal Chemistry and Calcium Speciation in the Lower Mantle
Abstract
Abstract The amount of ferric iron Fe 3+ in the lower mantle is largely unknown and may be influenced by the disproportionation reaction of ferrous iron Fe 2+ into metallic Fe and Fe 3+ triggered by the formation of bridgmanite. Recent work has shown that Fe 3+ has a strong effect on the density and seismic wave speeds of bridgmanite and the incorporation of impurities such as aluminum. In order to further investigate the effects of ferric iron on mineral behavior at lower mantle conditions, we conducted laser‐heated diamond‐anvil cell (LHDAC) experiments on two sets of samples nearly identical in composition (an aluminum‐rich pyroxenite glass) except for the Fe 3+ content; with one sample with more Fe 3+ (“oxidized”: Fe 3+ /ΣFe ~ 55%) and the other with less Fe 3+ (“reduced”: Fe 3+ /ΣFe ~ 11%). We heated the samples to lower mantle conditions, and the resulting assemblages were drastically different between the two sets of samples. For the reduced composition, we observed a multiphase assemblage dominated by bridgmanite and calcium perovskite. In contrast, the oxidized material yielded a single phase of Ca‐bearing bridgmanite. These Al‐rich pyroxenite samples show a difference in density and seismic velocities for these two redox states, where themore »
- Authors:
-
- Yale Univ., New Haven, CT (United States); Colorado School of Mines, Golden, CO (United States)
- Yale Univ., New Haven, CT (United States)
- Yale Univ., New Haven, CT (United States); Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
- Publication Date:
- Research Org.:
- Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
- Sponsoring Org.:
- USDOE National Nuclear Security Administration (NNSA)
- OSTI Identifier:
- 1775041
- Alternate Identifier(s):
- OSTI ID: 1786776
- Report Number(s):
- LLNL-JRNL-806201
Journal ID: ISSN 2169-9313; 1009919
- Grant/Contract Number:
- AC52-07NA27344; DE‐FG02‐94ER14466
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Geophysical Research. Solid Earth
- Additional Journal Information:
- Journal Volume: 125; Journal Issue: 10; Journal ID: ISSN 2169-9313
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; 37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY
Citation Formats
Creasy, Neala, Girard, Jennifer, Eckert, James O., and Lee, Kanani M. The Role of Redox on Bridgmanite Crystal Chemistry and Calcium Speciation in the Lower Mantle. United States: N. p., 2020.
Web. doi:10.1029/2020jb020783.
Creasy, Neala, Girard, Jennifer, Eckert, James O., & Lee, Kanani M. The Role of Redox on Bridgmanite Crystal Chemistry and Calcium Speciation in the Lower Mantle. United States. https://doi.org/10.1029/2020jb020783
Creasy, Neala, Girard, Jennifer, Eckert, James O., and Lee, Kanani M. Wed .
"The Role of Redox on Bridgmanite Crystal Chemistry and Calcium Speciation in the Lower Mantle". United States. https://doi.org/10.1029/2020jb020783. https://www.osti.gov/servlets/purl/1775041.
@article{osti_1775041,
title = {The Role of Redox on Bridgmanite Crystal Chemistry and Calcium Speciation in the Lower Mantle},
author = {Creasy, Neala and Girard, Jennifer and Eckert, James O. and Lee, Kanani M.},
abstractNote = {Abstract The amount of ferric iron Fe 3+ in the lower mantle is largely unknown and may be influenced by the disproportionation reaction of ferrous iron Fe 2+ into metallic Fe and Fe 3+ triggered by the formation of bridgmanite. Recent work has shown that Fe 3+ has a strong effect on the density and seismic wave speeds of bridgmanite and the incorporation of impurities such as aluminum. In order to further investigate the effects of ferric iron on mineral behavior at lower mantle conditions, we conducted laser‐heated diamond‐anvil cell (LHDAC) experiments on two sets of samples nearly identical in composition (an aluminum‐rich pyroxenite glass) except for the Fe 3+ content; with one sample with more Fe 3+ (“oxidized”: Fe 3+ /ΣFe ~ 55%) and the other with less Fe 3+ (“reduced”: Fe 3+ /ΣFe ~ 11%). We heated the samples to lower mantle conditions, and the resulting assemblages were drastically different between the two sets of samples. For the reduced composition, we observed a multiphase assemblage dominated by bridgmanite and calcium perovskite. In contrast, the oxidized material yielded a single phase of Ca‐bearing bridgmanite. These Al‐rich pyroxenite samples show a difference in density and seismic velocities for these two redox states, where the reduced assemblage is denser than the oxidized assemblage by ~1.5% at the bottom of the lower mantle and slower (bulk sound speed) by ~2%. Thus, heterogeneities of Fe 3+ content may lead to density and seismic wave speed heterogeneities in Earth's lower mantle.},
doi = {10.1029/2020jb020783},
journal = {Journal of Geophysical Research. Solid Earth},
number = 10,
volume = 125,
place = {United States},
year = {Wed Sep 30 00:00:00 EDT 2020},
month = {Wed Sep 30 00:00:00 EDT 2020}
}
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