Intermediate spin state and the B1-B2 transition in ferropericlase
Ferropericlase (fp), (Mg_{1−x}Fe_{x})O, the second most abundant mineral in the Earth's lower mantle, is expected to be an essential component of the mantles of super-Earths. Here, we present an ab initio investigation of the structure and magnetic ground state of fp up to ∼3TPa with iron conce...
| Prif Awduron: | , , |
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| Fformat: | Erthygl |
| Iaith: | English |
| Cyhoeddwyd: |
American Physical Society
2022-04-01
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| Cyfres: | Physical Review Research |
| Mynediad Ar-lein: | http://doi.org/10.1103/PhysRevResearch.4.023078 |