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.
Science , year = 2014, month = jun, volume = 344, pages =
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Multi-technique observations constrain the configuration of the ξ Tau system, detecting orbital oscillations on multiple timescales and suggesting component C is itself a binary.
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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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Configuration of the $\xi$ Tau system constrained by multi-technique observations
Multi-technique observations constrain the configuration of the ξ Tau system, detecting orbital oscillations on multiple timescales and suggesting component C is itself a binary.