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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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Bibliografiske detaljer
Udgivet i:Nat Commun
Main Authors: Hsieh, Wen-Pin, Goncharov, Alexander F., Labrosse, Stéphane, Holtgrewe, Nicholas, Lobanov, Sergey S., Chuvashova, Irina, Deschamps, Frédéric, Lin, Jung-Fu
Format: Artigo
Sprog:Inglês
Udgivet: Nature Publishing Group UK 2020
Fag:
Online adgang: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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