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by philipkglass
3392 days ago
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Accelerated silicate weathering seems like the best bet. Naturally occurring silicate compounds of magnesium and calcium react with ambient CO2 in the presence of water to form stable carbonates and silicon dioxide: CaSiO3 + CO2 -> CaCaO3 + SiO2 The thermodynamics are much more favorable than "combustion-in-reverse" (trying to reform hydrocarbons from CO2). The products are stable and the process can deal with point CO2 sources, distributed sources, atmospheric CO2, and ocean acidification -- the whole shebang. But the natural kinetics of silicate weathering are very slow. Kinetics can be improved by orders of magnitude if you grind the silicate minerals to dust; it's a surface area limited reaction. Kinetics get better yet if you apply the mafic rock dust to e.g. acid sulfate soils used for agriculture in the tropics. Those soils already need a pH boost to avoid crop stunting by soluble aluminum. Doing the adjustment with silicates instead of limestone means a two-for-one benefit (crop productivity plus drawing down CO2). But I think that to see widespread adoption there will have to be some targeted donor aid to poorer countries; ground limestone is cheaper than ground silicates if you don't care about CO2 abatement, and the rich world's farmers don't have a lot of acid sulfate soils in need of treatment within their home countries. |
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