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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Detalles Bibliográficos
Autores principales: Hsieh, Wen-Pin, Goncharov, Alexander F., Labrosse, Stéphane, Holtgrewe, Nicholas, Lobanov, Sergey S., Chuvashova, Irina, Deschamps, Frédéric, Lin, Jung-Fu
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7335046/
https://www.ncbi.nlm.nih.gov/pubmed/32620830
http://dx.doi.org/10.1038/s41467-020-17106-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7335046/
https://www.ncbi.nlm.nih.gov/pubmed/32620830
http://dx.doi.org/10.1038/s41467-020-17106-7

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