How does CO2 dissolve in seawater and what is the effect on ocean pH?

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Multiple Choice

How does CO2 dissolve in seawater and what is the effect on ocean pH?

Explanation:
CO2 dissolving in seawater engages the carbonate chemistry of the ocean. When CO2 enters, it reacts with water to form carbonic acid (CO2 + H2O ⇌ H2CO3). This carbonic acid then dissociates, releasing hydrogen ions and forming bicarbonate (H2CO3 ⇌ H+ + HCO3−), with further dissociation to carbonate (HCO3− ⇌ H+ + CO3^2−). The additional hydrogen ions raise the acidity of seawater, lowering its pH. While some bicarbonate and carbonate are produced, the overall effect of adding CO2 is an increase in H+ and a decrease in pH—ocean acidification. The other statements ignore or misstate this chemistry: CO2 does not dissolve without reacting and increasing pH, nor is there no pH effect.

CO2 dissolving in seawater engages the carbonate chemistry of the ocean. When CO2 enters, it reacts with water to form carbonic acid (CO2 + H2O ⇌ H2CO3). This carbonic acid then dissociates, releasing hydrogen ions and forming bicarbonate (H2CO3 ⇌ H+ + HCO3−), with further dissociation to carbonate (HCO3− ⇌ H+ + CO3^2−). The additional hydrogen ions raise the acidity of seawater, lowering its pH. While some bicarbonate and carbonate are produced, the overall effect of adding CO2 is an increase in H+ and a decrease in pH—ocean acidification. The other statements ignore or misstate this chemistry: CO2 does not dissolve without reacting and increasing pH, nor is there no pH effect.

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