Pressure dependence of metal–silicate partitioning explains the mantle phosphorus abundance
Abstract Previous experiments performed below 20 GPa suggested that the metal/silicate partition coefficient of phosphorus (P), D P, extrapolated to typical high-pressure and -temperature conditions of the Earth’s core formation gives too high P concentration in the core unless a large amount of sil...
| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2024-01-01
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| Series: | Scientific Reports |
| Online Access: | https://doi.org/10.1038/s41598-024-51662-y |