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Proc Natl Acad Sci U S A. 2014 Jul 22;111(29):10468-72. doi: 10.1073/pnas.1322427111. Epub 2014 Jul 7.

Spin crossover in ferropericlase and velocity heterogeneities in the lower mantle.

Author information

  • 1Laboratory of Seismology and Physics of Earth's Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, People's Republic of China; and wuzq10@ustc.edu.cn wentz002@umn.edu.
  • 2Department of Chemical Engineering and Materials Science andMinnesota Supercomputing Institute, University of Minnesota, Minneapolis, MN 55455 wuzq10@ustc.edu.cn wentz002@umn.edu.

Abstract

Deciphering the origin of seismic velocity heterogeneities in the mantle is crucial to understanding internal structures and processes at work in the Earth. The spin crossover in iron in ferropericlase (Fp), the second most abundant phase in the lower mantle, introduces unfamiliar effects on seismic velocities. First-principles calculations indicate that anticorrelation between shear velocity (VS) and bulk sound velocity (VĪ†) in the mantle, usually interpreted as compositional heterogeneity, can also be produced in homogeneous aggregates containing Fp. The spin crossover also suppresses thermally induced heterogeneity in longitudinal velocity (VP) at certain depths but not in VS. This effect is observed in tomography models at conditions where the spin crossover in Fp is expected in the lower mantle. In addition, the one-of-a-kind signature of this spin crossover in the RS/P (∂ ln VS/∂ ln VP) heterogeneity ratio might be a useful fingerprint to detect the presence of Fp in the lower mantle.

KEYWORDS:

density functional theory; elastic modulus; lateral heterogeneity; mantle plume; seismic tomography

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