Reduced lattice thermal conductivity of Fe-bearing bridgmanite in Earth's deep mantle

Wen Pin Hsieh, Frédéric Deschamps, Takuo Okuchi, Jung Fu Lin

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

Complex seismic, thermal, and chemical features have been reported in Earth's lowermost mantle. In particular, possible iron enrichments in the large low shear-wave velocity provinces (LLSVPs) could influence thermal transport properties of the constituting minerals in this region, altering the lower mantle dynamics and heat flux across core-mantle boundary (CMB). Thermal conductivity of bridgmanite is expected to partially control the thermal evolution and dynamics of Earth's lower mantle. Importantly, the pressure-induced lattice distortion and iron spin and valence states in bridgmanite could affect its lattice thermal conductivity, but these effects remain largely unknown. Here we precisely measured the lattice thermal conductivity of Fe-bearing bridgmanite to 120 GPa using optical pump-probe spectroscopy. The conductivity of Fe-bearing bridgmanite increases monotonically with pressure but drops significantly around 45 GPa due to pressure-induced lattice distortion on iron sites. Our findings indicate that lattice thermal conductivity at lowermost mantle conditions is twice smaller than previously thought. The decrease in the thermal conductivity of bridgmanite in mid-lower mantle and below would promote mantle flow against a potential viscosity barrier, facilitating slabs crossing over the 1000 km depth. Modeling of our results applied to LLSVPs shows that variations in iron and bridgmanite fractions induce a significant thermal conductivity decrease, which would enhance internal convective flow. Our CMB heat flux modeling indicates that while heat flux variations are dominated by thermal effects, variations in thermal conductivity also play a significant role. The CMB heat flux map we obtained is substantially different from those assumed so far, which may influence our understanding of the geodynamo.

Original languageEnglish
JournalJournal of Geophysical Research: Solid Earth
DOIs
Publication statusAccepted/In press - 2017

Fingerprint

Bearings (structural)
thermal conductivity
Thermal conductivity
Earth mantle
Earth (planet)
mantle
heat
core-mantle boundary
heat flux
Heat flux
lower mantle
Iron
iron
Shear waves
S waves
wave velocity
S-wave
shear stress
geodynamo
convective flow

Keywords

  • Bridgmanite
  • Geodynamics
  • Thermal conductivity

ASJC Scopus subject areas

  • Geophysics
  • Oceanography
  • Forestry
  • Ecology
  • Aquatic Science
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology

Cite this

Reduced lattice thermal conductivity of Fe-bearing bridgmanite in Earth's deep mantle. / Hsieh, Wen Pin; Deschamps, Frédéric; Okuchi, Takuo; Lin, Jung Fu.

In: Journal of Geophysical Research: Solid Earth, 2017.

Research output: Contribution to journalArticle

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