Many climate models include the removal of between 5 and 10 gigatons of carbon dioxide per year through the end of the century. Christopher Reinhard and colleagues used a large number of Earth system model simulations to create a complex representation of the physical and chemical response of the atmosphere and sea to enhanced rock weathering.
Enhanced rock weathering is the practice of processing rock materials in such a way as to encourage chemical reactions between rock and atmospheric carbon, forming substances like bicarbonate, which then keep carbon out of the atmosphere.
Bicarbonate can be added to the ocean and stored for up to 10,000 years before the hydrological cycle eventually transports it back into the atmosphere. There has been concern, however, that some fraction of the bicarbonate added to seawater will break down almost immediately, rapidly leaking carbon back into the atmosphere.
The models predict that the oceanic storage of carbon is 90 percent effective and "leakage" on decadal timescales is minimal. Carbon will leave the ocean as atmospheric levels come down, simply because carbon concentrations seek equilibrium across the skin of the sea, but this flux will not be significantly augmented by leakage from enhanced rock weathering, according to the authors.
Research Report:New estimates of the storage permanence and ocean co-benefits of enhanced rock weathering
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