When CO2 dissolves in water there is no such thing as aqueous CO2 is there? It forms H2CO3 in an equilibrium reaction system as follows:
CO2(g)+ H20(l) <-> H2CO3(aq)
As you wrote - it is an equilibrium. Thus there is CO
2 present in water.
And adding more CO2 to the reaction system will drive it to the right making more H2CO3 which is why the pH drops because you are just increasing the H+ conc. That's right so far isn't it? Why then, do tanks with CO2 injection show greater plant growth than tanks without it? It doesn't make sense. Where do aquatic plants get their CO2 for photosynthesis?
From the equilibrium concentration of CO
2, you forgot about that factor thus your reasoning is partially faullty.
Now if CaCO3 is added as a solid as crushed coral, it would not actually dissolve would it because both the carbonic acid and the calcium carbonate have carbonate ions so no replacement will occur. Correct? Or is water acting as an acid in this case and the lower pH increases its solubility in the water? If so it would kind of act like a buffer wouldn't it because CO32- ions would push the Rx back to the left and CO2 is continually being pumped into the system as well so the forward and backward Rx would be equal until the coral was completely dissolved??? Now I'm just confusing myself... Is anyone able to explain this to me? I am not seeing how the crushed coral can actually act as a buffer to help maintain an acidic pH. To me it looks like it will either have no effect or will just increase pH rather than maintain a constant pH.
Adding CO
2 lowers pH:
CO
2 + H
2O <-> H
+ + HCO
3-(in fact I could write this reaction as two steps, with H
2CO
3 as intermediary, but it will not change a thing). But in the presence of CaCO
3 situation is a little bit more complicated, as what happens is that part of CaCO
3 dissolves:
CaCO
3 + CO
2 + H
2O -> Ca
2+ + 2HCO
3-There are CO
2 (or H
2CO
3) and HCO
3- present in the solution. This is an acid and its conjugate base, thus you have a buffer solution, with pH close to 7. CO
32- concentration is neglectable in this system.
There is no risk of dissolving all coral as the solubility of CaCO
3 and Ca(HCO
3)
2 is rather low and the solubility of CO
2 is not that large too (less then 2g/L in normal presure and 20 deg C).