Metal saturation from iron disproportionation redistributes hydrogen from subducted water, decreasing mantle silicate water storage capacity by 64-96% to 0.1-0.8 ocean masses and creating a wet shallow-dry deep mantle contrast.
Title resolution pending
1 Pith paper cite this work. Polarity classification is still indexing.
1
Pith paper citing it
citation-role summary
background 1
citation-polarity summary
fields
physics.geo-ph 1years
2026 1verdicts
UNVERDICTED 1roles
background 1polarities
background 1representative citing papers
citing papers explorer
-
Metal Saturation and the Redistribution of Hydrogen in Earth's Mantle
Metal saturation from iron disproportionation redistributes hydrogen from subducted water, decreasing mantle silicate water storage capacity by 64-96% to 0.1-0.8 ocean masses and creating a wet shallow-dry deep mantle contrast.