3 ms·
The reaction between carbon dioxide and alkaline earth silicates is thermodynamically spontaneous in the presence of water, but kinetically hindered. It's a rea
by philipkglass 6y ago
The reaction between carbon dioxide and alkaline earth silicates is thermodynamically spontaneous in the presence of water, but kinetically hindered. It's a reaction with slow diffusion of reactants through the product layer, limited by surface area. So crush rocks rich in alkaline earth silicates and distribute them in near-shore environments. It's an artificially accelerated version of the geological carbon cycle. It still requires vast-in-absolute-terms amounts of energy to crush billions of tons of rock, but it's not running uphill against thermodynamics.
Olivine:
Mg2SiO4 + 2CO2 → 2MgCO3 + SiO2: ΔH -89 kJ mol/CO2
Serpentine:
Mg3Si2O5(OH)4 + 3 CO2 → 3MgCO3 + 2SiO2 + 2H2O: ΔH -64 kJ mol/CO2
Wollastonite:
CaSiO3 + CO2 → CaCO3 + SiO2: ΔH -90 kJ mol/CO2
https://www.ipcc.ch/site/assets/uploads/2018/03/srccs_chapter7-1.pdf https://www.ipcc.ch/site/assets/uploads/2018/03/srccs_chapte... (Section 7.2.2 "Chemistry of mineral carbonation")
- CyanBird 6y agoWe already have catalytic convertors on cars, can we add co2 capture to them as well? Add a little box with powdered olivine and some extra chemical bits to capture a higher % of co2 than absolute 0? Catalytic convertors already use finely coated incredibly expensive platinum to break down complex molecules, and it is certainly easier to capture co2 near the source than when dissipated in the atmosphere
- dodobirdlord 6y agoNo. The reaction happens in water, it’s fairly slow, the mixture needs to be agitated, and it would require similar quantities of silicates to the among of hydrocarbons being burned. Better to ignore capture at the source and instead prioritize mass-capture in places that are energy efficient. Shallow coastal areas near major deposits.
- sunstone 6y agoA couple of H-bombs in the Himalayas might do the trick quite quickly.