Abnormal Elasticity of Fe-Bearing Bridgmanite in the Earth's Lower Mantle
Abstract
We measured the effect of pressure on the compressional and shear wave velocity (VP, VS) as well as density of Fe-bearing bridgmanite, Mg0.96(1)Fe2+0.036(5)Fe3+0.014(5)Si0.99(1)O3, using impulsive stimulated light scattering, Brillouin light scattering, and X-ray diffraction, respectively, in diamond anvil cells up to 70 GPa at 300 K. A drastic softening of VP by ~6(±1)% is observed between 42.6 and 58 GPa, while VS increases continuously with increasing pressure. A significant reduction in Poisson's ratio from 0.24 to 0.16 occurs at ~42.6–58 GPa, while VS increases by ~3(±1)% above ~40 GPa compared to MgSiO3-bridgmanite. Thermoelastic modeling of the experimental results shows that the observed elastic anomaly of Fe-bearing bridgmanite is consistent with a spin transition of octahedrally coordinated Fe3+ in bridgmanite. These results challenge traditional views that Fe enrichment will reduce seismic velocities, suggesting that seismic heterogeneities in the mid-lower mantle may be due to a spin transition of Fe in Fe-bearing bridgmanite.
- Authors:
-
- Univ. of Texas, Austin, TX (United States)
- Okayama Univ., Misasa (Japan)
- Univ. of Bayreuth (Germany)
- Seoul National Univ. (Korea, Republic of)
- Publication Date:
- Research Org.:
- Argonne National Lab. (ANL), Argonne, IL (United States). Advanced Photon Source (APS)
- Sponsoring Org.:
- USDOE Office of Science (SC), Basic Energy Sciences (BES); National Science Foundation (NSF)
- OSTI Identifier:
- 1459956
- Grant/Contract Number:
- AC02‐06CH11357; FG02‐94ER14466
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Geophysical Research Letters
- Additional Journal Information:
- Journal Volume: 45; Journal Issue: 10; Journal ID: ISSN 0094-8276
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- ENGLISH
- Subject:
- 58 GEOSCIENCES; bridgmanite; elasticity; spin transition; lower mantle
Citation Formats
Fu, Suyu, Yang, Jing, Zhang, Yanyao, Okuchi, Takuo, McCammon, Catherine, Kim, Hyo-Im, Lee, Sung Keun, and Lin, Jung-Fu. Abnormal Elasticity of Fe-Bearing Bridgmanite in the Earth's Lower Mantle. United States: N. p., 2018.
Web. doi:10.1029/2018GL077764.
Fu, Suyu, Yang, Jing, Zhang, Yanyao, Okuchi, Takuo, McCammon, Catherine, Kim, Hyo-Im, Lee, Sung Keun, & Lin, Jung-Fu. Abnormal Elasticity of Fe-Bearing Bridgmanite in the Earth's Lower Mantle. United States. https://doi.org/10.1029/2018GL077764
Fu, Suyu, Yang, Jing, Zhang, Yanyao, Okuchi, Takuo, McCammon, Catherine, Kim, Hyo-Im, Lee, Sung Keun, and Lin, Jung-Fu. Tue .
"Abnormal Elasticity of Fe-Bearing Bridgmanite in the Earth's Lower Mantle". United States. https://doi.org/10.1029/2018GL077764. https://www.osti.gov/servlets/purl/1459956.
@article{osti_1459956,
title = {Abnormal Elasticity of Fe-Bearing Bridgmanite in the Earth's Lower Mantle},
author = {Fu, Suyu and Yang, Jing and Zhang, Yanyao and Okuchi, Takuo and McCammon, Catherine and Kim, Hyo-Im and Lee, Sung Keun and Lin, Jung-Fu},
abstractNote = {We measured the effect of pressure on the compressional and shear wave velocity (VP, VS) as well as density of Fe-bearing bridgmanite, Mg0.96(1)Fe2+0.036(5)Fe3+0.014(5)Si0.99(1)O3, using impulsive stimulated light scattering, Brillouin light scattering, and X-ray diffraction, respectively, in diamond anvil cells up to 70 GPa at 300 K. A drastic softening of VP by ~6(±1)% is observed between 42.6 and 58 GPa, while VS increases continuously with increasing pressure. A significant reduction in Poisson's ratio from 0.24 to 0.16 occurs at ~42.6–58 GPa, while VS increases by ~3(±1)% above ~40 GPa compared to MgSiO3-bridgmanite. Thermoelastic modeling of the experimental results shows that the observed elastic anomaly of Fe-bearing bridgmanite is consistent with a spin transition of octahedrally coordinated Fe3+ in bridgmanite. These results challenge traditional views that Fe enrichment will reduce seismic velocities, suggesting that seismic heterogeneities in the mid-lower mantle may be due to a spin transition of Fe in Fe-bearing bridgmanite.},
doi = {10.1029/2018GL077764},
journal = {Geophysical Research Letters},
number = 10,
volume = 45,
place = {United States},
year = {Tue May 08 00:00:00 EDT 2018},
month = {Tue May 08 00:00:00 EDT 2018}
}
Web of Science
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