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Low thermal conductivity of iron-silicon alloys at Earth’s core conditions with implications for the geodynamo
Earth’s core is composed of iron (Fe) alloyed with light elements, e.g., silicon (Si). Its thermal conductivity critically affects Earth’s thermal structure, evolution, and dynamics, as it controls the magnitude of thermal and compositional sources required to sustain a geodynamo over Earth’s histor...
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| Vydáno v: | Nat Commun |
|---|---|
| Hlavní autoři: | , , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2020
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7335046/ https://ncbi.nlm.nih.gov/pubmed/32620830 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-020-17106-7 |
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