Carbonate Species vs. pH (Closed System)
Given is a 10-3 molar carbonate solution (closed system with 1 mM DIC). What is the species distribution in the pH range between 1 and 13?
One of the most celebrated diagrams in hydrochemistry is undoubtedly the carbonate species distribution vs. pH (something as shown below). The carbonate speciation is the outcome of a set of equations for the pure CO2-H2O system.1
However: For a given value of DIC, say 1 mM, the pH is fixed to 4.68 in a pure CO2 solution at 25 and there is no chance to alter the pH unless the pure system is extended by an additional degree of freedom. This can be done – as everybody knows – by addition of NaOH (to increase pH) or HCl (to decrease pH).
To cover the desired pH range from 1 to 13 a series of options are available (infinitely many). Here are only three:
Option 1. Start with the pure CO2 solution and add successively HCl until pH 1 is reached. Then, take again the pure CO2 solution and add successively NaOH until pH 13.
Option 2. Prepare an initial solution with pH 13 (by addition of 137.2 mM NaOH). Then add to this solution successively HCl until pH 1 is reached.
Option 3. Prepare an initial solution with pH 1 (by addition of 122.4 mM HCl). Then add to this solution successively NaOH until pH 13 is reached.
[Note: The titration curves for each option differ from another, at least slightly. This is caused by two things: (i) different ionic strengths and (ii) Na forms aqueous complexes such like NaHCO3 and NaCO3-, whereas Cl does not.]
Titration Calculations for Option 1
There are two ways to perform the titration calculation for Option 1:2
Way 1. Choose the amount of HCl/NaOH and calculate the pH.
Start with pure water (button H2O) and use the reaction module (button Reac). Then enter two reactants:
- 1 mM CO2 (which is equivalent to 1 mM DIC)
- either HCl or NaOH (and repeat it with variable amount)
Way 2. Choose the pH and calculate the amount of HCl/NaOH.
Start with pure water (button H2O) and switch to molar units (checkbox Mol). Enter 1 mM DIC, the desired pH value, say pH = 3, and set an arbitrary start value for chloride (to mimic HCl addition), say 1 mM Cl.
Click on Start and force charge-balance adjustment with parameter “Cl”. The program promptly outputs the correct amount of Cl (which is identical to the molar amount of HCl). The output tables (including table Ions) display the complete speciation. Some of these data are replicated in the table below.
For pH > 4.68, use Na instead of Cl (in order to simulate NaOH addition). In this way, you are able to calculate any titration point you wish. The table below gives you some idea. (Completion of this table is going faster than expected.)
What you finally achieve by Way 1 or Way 2 is something like this:3
Results and Discussion
The pure 1 mM CO2 system is marked by light-red color.
Mass Conservation (Mole Balance). It’s easy to confirm that the sum of all carbonate species (in each table row) equals the total amount of dissolved inorganic carbon:
|(1)||DIC = CO2 + HCO3- + CO3-2 + NaHCO3 + NaCO3- = 1 mM|
This equation can be rearranged into a sum of three terms
|(2)||DIC = CO2 + [HCO3-]T + [CO3-2]T|
where the sum of bicarbonates and the sum of carbonates are specified as separate entities:
|(3a)||[HCO3-]T||= HCO3- + NaHCO3|
|(3b)||[CO3-2]T||= CO3-2 + NaCO3-|
Diagrams. The first diagram displays the pH dependence of five carbonate species; the second diagram plots the pH dependence of CO2, [HCO3-]T, and [CO3-2]T. Thereby, ion HCO3- is merged with NaHCO3 to total bicarbonate, and ion CO3-2 is merged with NaCO3- to total carbonate.
The second diagram exhibits some kind of symmetry about pH = 8.2 which is known as the equivalence point of a pure NaHCO3 solution. Hydrogen carbonate (blue curve) dominates the pH range between 6 and 10; this range almost coincides with the realm of natural waters (pH 6 to 8).
The plots can also be converted into a stacked-area chart. In this form it demonstrates the strict mass conservation in a closed system, where all carbonate species add up to 1 mM DIC – as demanded by Eq.(1):
Footnotes & Remarks
With the program, the CO2-H2O system is generated by addition of CO2 or H2CO3 (and nothing else) to pure water H2O. ↩
There are more ways to perform such calculations, including the automatic generation of “titration plots” (as part of the reaction module). The advantage of Way 1 or Way 2 over an automatic generation is that we select the individual points of reactant or pH just the way we like it. ↩
Formally, the calculations can be extended to pH 14 (as shown here), but this requires 1745 mM NaOH, which results in a too high ionic strength (just above the validation range of our activity models). ↩