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Atmospheric CO2 (g) is in equilibrium with dissolved CO, (aq), CO2(g) CO2 (aq) CO: (aq) then can react with water to become H
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CQ (8) T Wcaq) co (aq) + HOU) - 12003 (aq) Overall rom co, (g) + Holl) - 140₂ (aq) 2. 2 (9) T W cag) Kelto, ca9] = 1.44810- 43. According to le chatteleer prmaple of we we add more reactant then more and more product will formed in the reaction moves

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