Cargando…
The effect of iron spin transition on electrical conductivity of (Mg,Fe)O magnesiowüstite
We measured the electrical conductivity of Mg(0.81)Fe(0.19)O magnesiowüstite, one of the important minerals comprising Earth’s lower mantle, at high pressures up to 135 GPa and 300 K in a diamond-anvil cell (DAC). The results demonstrate that the electrical conductivity increases with increasing pre...
Autores principales: | Ohta, Kenji, Hirose, Kei, Onoda, Suzue, Shimizu, Katsuya |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
The Japan Academy
2007
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3756880/ https://www.ncbi.nlm.nih.gov/pubmed/24019587 |
Ejemplares similares
-
Subduction-related oxidation of the sublithospheric mantle evidenced by ferropericlase and magnesiowüstite diamond inclusions
por: Kiseeva, Ekaterina S., et al.
Publicado: (2022) -
Structural transition and re-emergence of iron's total electron spin in (Mg,Fe)O at ultrahigh pressure
por: Hsu, Han, et al.
Publicado: (2022) -
Symmetry broken spin reorientation transition in epitaxial MgO/Fe/MgO layers with competing anisotropies
por: Martínez, Isidoro, et al.
Publicado: (2018) -
The thermal conductivity of the Earth's core and implications for its thermal and compositional evolution
por: Ohta, Kenji, et al.
Publicado: (2020) -
Electric control of spin transitions at the atomic scale
por: Kot, Piotr, et al.
Publicado: (2023)