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.
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Mantle partial melting buffers magma-ocean differentiation more on Earth than Mars due to stronger convection, explaining the presence of a basal dense layer only on Mars.
citing papers explorer
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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.
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Earth and Mars interior structures set by re-melting of the first solid mantle
Mantle partial melting buffers magma-ocean differentiation more on Earth than Mars due to stronger convection, explaining the presence of a basal dense layer only on Mars.