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Electronic Transitions in Perovskite: Possible Nonconvecting Layers in the Lower Mantle

Badro, James, Rueff, Jean-Pascal, Vankó, György, Monaco, Giulio, Fiquet, Guillaume, Guyot, François·2004·Science

Abstract

We measured the spin state of iron in magnesium silicate perovskite (Mg 0.9 ,Fe 0.1 )SiO 3 at high pressure and found two electronic transitions occurring at 70 gigapascals and at 120 gigapascals, corresponding to partial and full electron pairing in iron, respectively. The proportion of iron in the low spin state thus grows with depth, increasing the transparency of the mantle in the infrared region, with a maximum at pressures consistent with the D″ layer above the core-mantle boundary. The resulting increase in radiative thermal conductivity suggests the existence of nonconvecting layers in the lowermost mantle.

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Metadata

Authors
Badro, J., Rueff, J.-P., Vankó, G., Monaco, G., Fiquet, G., & Guyot, F.
Venue
Science
Published
2004-07-16
Volume
305
Issue
5682
Pages
383-386
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2039235095
Cited by
373
References
0
FWCI
27.59
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Electronic Transitions in Perovskite: Possible Nonconvecting Layers in the Lower Mantle. https://app.cochat.ai/papers/10.1126/science.1098840
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Badro, J., Rueff, J.-P., Vankó, G., Monaco, G., Fiquet, G., & Guyot, F. (2004). Electronic Transitions in Perovskite: Possible Nonconvecting Layers in the Lower Mantle. Science. https://doi.org/10.1126/science.1098840

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Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.