skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Spin Transition of Iron in the Earth's Lower Mantle

Journal Article · · Physics of the Earth and Planetary Interiors
OSTI ID:964106

Electronic spin-pairing transitions of iron and associated effects on the physical properties of host phases have been reported in lower-mantle minerals including ferropericlase, silicate perovskite, and possibly in post-perovskite at lower-mantle pressures. Here we evaluate current understanding of the spin and valence states of iron in the lower-mantle phases, emphasizing the effects of the spin transitions on the density, sound velocities, chemical behavior, and transport properties of the lower-mantle phases. The spin transition of iron in ferropericlase occurs at approximately 50 GPa but likely turns into a wide spin crossover under lower-mantle temperatures. Current experimental results indicate a continuous nature of the spin crossover in silicate perovskite at high pressures, but which valence state of iron undergoes the spin crossover and what is its associated crystallographic site remain uncertain. The spin transition of iron results in enhanced density, incompressibility, and sound velocities, and reduced radiative thermal conductivity in the low-spin ferropericlase, which should be considered in future geophysical and geodynamic modeling of the Earth's lower mantle. Our evaluation of the experimental and theoretical pressure-volume results shows that the spin crossover of iron results in a density increase of 3-4% in ferropericlase containing 17-19% FeO. Here we have modeled the density and bulk modulus profiles of ferropericlase across the spin crossover under lower-mantle pressure-temperature conditions and showed how the ratio of the spin states of iron affects our understanding of the state of the Earth's lower mantle.

Research Organization:
Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Sponsoring Organization:
USDOE
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
964106
Report Number(s):
UCRL-JRNL-231256; PEPIAM; TRN: US200922%%100
Journal Information:
Physics of the Earth and Planetary Interiors, Vol. 170, Issue 3-4; ISSN 0031-9201
Country of Publication:
United States
Language:
English

Similar Records

Electronic Spin Crossover of Iron in Ferroperclase in Earth?s Lower Mantle
Journal Article · Thu Jan 25 00:00:00 EST 2007 · Science · OSTI ID:964106

Electronic spin state of iron in lower mantle perovskite
Journal Article · Tue Nov 16 00:00:00 EST 2010 · Proc. Natl. Acad. Sci. USA · OSTI ID:964106

Texture and Strength of Lower Mantle Ferropericlase Across the Spin Transition
Journal Article · Thu Jan 01 00:00:00 EST 2009 · Physics and Chemistry of Minerals · OSTI ID:964106