The interaction between carbon dioxide and water results in formation of carbonic acid, H2CO3, which lowers the pH of water through the reactions
H2CO3(aq)+H2O(l) <---> HCO3-(aq) + H3O+(aq) Ka1= 4.3*10^-7
HCO3-(aq) +H2O(l) <---> CO3 2- (aq) + H3O+ (aq) Ka2=5.6*10^-11
This dissocociation causes "normal" rainwater to have a pH of approximately 5.7. However, H3O+(aq) can also come from other sources, particularly from acids resulting from interactions of water with industrial pollutants.
Scientists studying a particular lake found that its pH was 4.8, and the total carbonate concentration (that of H2CO3, HCO-, and CO3 2-) was 4.5*10^-3M. Determine the concentration of each individual carbonate species.
The pH of the solution is 4.8; we define pH as pH = -log [H+]; therefore, [H+] = antilog(-pH) = 10-4.8 = 1.5849*10-5 M.
Find out the fraction of species as
f(H2CO3) = [H+]2/D where D = [H+]2 + Ka1*[H+] + Ka1*Ka2 = (1.5849*10-5)2 + (4.3*10-7)*(1.5849*10-5) + (4.3*10-7)*(5.6*10-11) = 2.5800*10-10.
Therefore, f(H2CO3) = (1.5849*10-5)2/(2.5800*10-10) = 0.9736.
f(HCO3-) = Ka1*[H+]/D = (4.3*10-7)*(1.5849*10-5)/(2.5800*10-10) = 0.0264.
f(CO32-) = Ka1*Ka2/D = (4.3*10-7)*(5.6*10-11)/(2.5800*10-10) = 9.3333*10-7.
[H2CO3] = f(H2CO3)*(total carbonate concentration) = 0.9736*(4.5*10-3 M) = 4.3812*10-3 M (ans).
[HCO3-] = f(HCO3-)*(total carbonate concentration) = 0.0264*(4.5*10-3 M) = 1.188*10-4 M (ans).
[CO32-] = f(CO32-)*(total carbonate concentration) = 9.3333*10-7*(4.5*10-3 M) = 4.199985*10-9 M ≈ 4.20*10-9 M (ans).
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