Carbon Dioxide - Carbonic Acid Equilibrium
Carbonic acid is formed when atmospheric CO2 is dissolved in water. The chemical equilibria are
1) Gas dissolution
2) Carbonic acid formation
3) Carbonic acid equilibrium
In an open system, the partial pressure of CO2 (g) is relatively constant at P(CO2) = 0.000355 Atmosphere.
The equilibrium expression is the Henry's Law equation (@ 25 °C)
Using this one may obtain
Click here to learn more about calculating the pH of water in equilibrium with air
Dependent Carbonate Equilibrium
Using carbonate mass balance and acid equilibrium expressions, the fractional amounts of all carbonate species can be found as a function of [H+]
The pH dependent fractions are
Of interest is the total carbonate as a function of pH.
Remember that [H2CO3] is "fixed" by the atmosphere in an open equilibrium system and
Total carbonate increases with pH.
Solubility of Calcium Carbonate
(A Systematic Treatment)
This is obviously a difficult system of equations to solve. Though it could be done, let's look for the approximations (AKA, the easy way out)
Click here to learn more about systematic treatment of chemical equilibrium
Molar Solubility of Calcium Carbonate Approximations
Open system; The trick to solving for carbonate equilibria is to first identify the major species. That is, we should be able to look at all equilibria and determine which carbonate species are in greatest abundance.
The major equilibrium process here is
By examining the alpha plot, we see that HCO3- is a maximum at pH=8.3. This will help. Solving
Closed System: The real trick here, if there is one, is to find the pH. With the pH, we can easily solve any carbonate problem with the fractional amounts. For example, the calcium carbonate solubility is a function of the fractional amount of carbonate as carbonate and the total amount of carbonate. In a closed system at fixed pH
Click here to learn about calcium carbonate solublity as a function of pH.
This page was last updated Tuesday, August 03, 2004