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Title: Elasticity of ferropericlase across the spin crossover in the Earth’s lower mantle

Journal Article · · Scientific Reports
DOI:https://doi.org/10.1038/srep17188· OSTI ID:1240833
 [1];  [1];  [2];  [3];  [3]
  1. Univ. of Texas, Austin, TX (United States). Department of Geological Sciences, Jackson School of Geosciences
  2. Univ. of Texas, Austin, TX (United States). Department of Geological Sciences, Jackson School of Geosciences; Center for High Pressure Science and Technology Advanced Research, (China)
  3. Institute for Study of the Earth's Interior, Misasa, Tottori (Japan)

The effects of the spin transition on the physics and chemistry of the lower-mantle ferropericlase and perovskite have been suggested to have significant consequences on the seismology and geochemistry. Knowing the elasticity of ferropericlase across the spin transition can help explain seismic and mineralogical models of the lower-mantle including the origin of seismic heterogeneities in the middle to lowermost parts of the lower mantle. However, full elastic tensors of ferropericlase within the spin transition and in the low-spin state remains experimentally controversial due to technical challenges in directly measuring sound velocities under lower-mantle conditions. Here we have reliably measured both VP and VS of a single-crystal ferropericlase ((Mg0.92,Fe0.08)O) using complementary Brillouin Light Scattering and Impulsive Stimulated Light Scattering coupled with diamond anvil cell (DAC) up to 96 GPa. The derived elastic tensors show drastically softened C11 and C12 within the spin transition at 40-60 GPa while C44 is not affected. Based on thermoelastic modelling along an expected geotherm, the spin crossover in ferropericlase can contribute to elastic abnormalities at mid lower-mantle conditions. Furthermore, our results imply the middle to lowermost parts of the lower mantle would exhibit enhanced seismic heterogeneities due to the occurrence of the mixed-spin and low-spin ferropericlase.

Research Organization:
Univ. of Chicago, Argonne, IL (United States); Carnegie Institution of Washington, Washington, D.C. (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Basic Energy Sciences (BES); USDOE National Nuclear Security Administration (NNSA)
Grant/Contract Number:
AC02-06CH11357; NA0002006
OSTI ID:
1240833
Alternate ID(s):
OSTI ID: 1335494
Journal Information:
Scientific Reports, Vol. 5; ISSN 2045-2322
Publisher:
Nature Publishing GroupCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 42 works
Citation information provided by
Web of Science

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Cited By (6)

Abnormal Elasticity of Fe-Bearing Bridgmanite in the Earth's Lower Mantle journal May 2018
Elastic Softening of (Mg 0.8 Fe 0.2 )O Ferropericlase Across the Iron Spin Crossover Measured at Seismic Frequencies journal July 2018
The extreme acoustic anisotropy and fast sound velocities of cubic high-pressure ice polymorphs at Mbar pressure journal May 2019
Effects of iron on the lattice thermal conductivity of Earth’s deep mantle and implications for mantle dynamics journal April 2018
Abnormal Elasticity of Single-Crystal Magnesiosiderite across the Spin Transition in Earth’s Lower Mantle journal January 2017
Effects of iron spin transition on the electronic structure, thermal expansivity and lattice thermal conductivity of ferropericlase: a first principles study journal March 2019

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