So i understand all of Le Chatelier's principles etc. etc. but why is it that when you go deeper into the ocean, i.e. to a higher pressure, the solubility of CaCO3 (s) increases?
My understanding thus far is:
[CO2(aq)] will increase which means the [H+] and [HCO3-] will increase, but surely they increase by the same proportion so for the dissociation of HCO3- to H+ and CO3^2- the equilibrium will shift to the right, increasing the [CO3^2-] which would shift the equilibrium of CaCO3 to its dissolved form back to CaCO3?
I'll try and attach the equilibriums