Oceanic uptake of carbon dioxide is thus described: CO2 (g) + H2O ⇔ H2CO3, K = [H2CO3]/PCO2 = 3 x 10-2 M atm-1  H2CO3 ⇔ HCO3- + H+,  K = [HCO3-][H+]/[H2CO3] = 9 x 10-7 moles/L HCO3- ⇔ CO32 - + H+, K = [CO32 -][H+]/[HCO3-] = 7 x 10-10 moles/L Charge balance equation: [H+] = [OH-] + [HCO3-] + 2[CO32 ]  If the CO2 concentration in the atmosphere is 300 ppm, what is the pH of the ocean?

Introduction to General, Organic and Biochemistry
11th Edition
ISBN:9781285869759
Author:Frederick A. Bettelheim, William H. Brown, Mary K. Campbell, Shawn O. Farrell, Omar Torres
Publisher:Frederick A. Bettelheim, William H. Brown, Mary K. Campbell, Shawn O. Farrell, Omar Torres
Chapter6: Solutions And Colloids
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Oceanic uptake of carbon dioxide is thus described:
CO2 (g) + H2O ⇔ H2CO3, K = [H2CO3]/PCO2 = 3 x 10-2 M atm-1 
H2CO3 ⇔ HCO3- + H+,  K = [HCO3-][H+]/[H2CO3] = 9 x 10-7 moles/L
HCO3- ⇔ CO32 - + H+, K = [CO32 -][H+]/[HCO3-] = 7 x 10-10 moles/L
Charge balance equation:
[H+] = [OH-] + [HCO3-] + 2[CO32

If the CO2 concentration in the atmosphere is 300 ppm, what is the pH of the ocean?

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