Understanding the Effects of CO2 on Seawater
As CO2 concentration in the atmosphere rises, more CO2 is absorbed by the oceans. This leads to the formation of carbonic acid, which dissociates into bicarbonate ions (HCO3-) and hydrogen ions (H+). The increased concentration of hydrogen ions causes the seawater pH to decrease (acidification).
Option (B): This is correct because the rise in CO2 leads to a decrease in seawater pH due to increased acidity, and the concentration of bicarbonate ions increases as a result of CO2 dissolving into the seawater.
Option (C): This is correct because the rise in CO2 leads to warming of surface ocean water, which can further exacerbate ocean acidification. The increased CO2 reduces the concentration of carbonate ions, which are essential for marine organisms to form calcium carbonate shells.
Option (A): This is incorrect because seawater pH actually decreases, not increases, with the rise in CO2.
Option (D): This is incorrect because while seawater pH decreases, the concentration of bicarbonate ions actually increases, not decreases, with the absorption of CO2 by the oceans.