When carbon dioxide "dissolves" in water, essentially all of it
reacts to form carbonic acid, H2CO3:
The carbonic acid can then dissociate into H* and bicarbonate ions,
(The table at the back of this book gives thermodynamic data for both of these
reactions.) Consider a body of otherwise pure water (or perhaps a raindrop) that
is in equilibrium with the atmosphere near sea level, where the partial pressure of
carbon dioxide is 3.4 x 10-4 bar (or 340 parts per million). Calculate the molality
of carbonic acid and of bicarbonate ions in the water, and determine the pH of the
solution. Note that even "natural" precipitation is somewhat acidic.