In: Chemistry
Explain how the pH of water can be affected by the ionic strength of the water
The ionic strength (I) of a solution is calculated from all the
ions `i` in the solution and as follow:
I = ½ . ∑ [i] . z2
This equation states that ionic strength is calculated as the squared sum of the valence and concentration of all ions in the solution.
The concentration metric used is usually the molar concentration (mol/L), but the most accurate is actually to use the molal concentration (mol/kg). In most cases it is easier to use molarities and in most cases the difference is not that important.
Ionic strength is used to correct equations used in e.g. pH calculations and to get more accurate estimates of concentrations of ions and compounds in equilibriums.
The relationship between the concentration [H+] and
activity of e.g. the hydrogen ion {H+} is:
fH+. [H+] =
{H+}
In this equation fH+ is the individual activity of the H+ ion and [H+] the concentration of the hydrogen ion and {H+} the activity of H+.
The calculation of fH+ is relatively straightforward. It is however not entirely clear which formula should be used for the calculation of fH+, ionic strength etc. in solutions that are far from ideal, since there is no consensus about which equations are true under which circumstances.
So if you are working with wastewater, or any biological system, you will have some trouble finding the right equation to use, and arhiing why you’ve picked any equation for your calculations.
For this example I'll assume that the Güntelberg equation for
calculating individual ion activities can be used to describe the
relationship between [H+] and {H+}.
The Güntelberg equation states that:
log10 fH+ =
-0.51.z2.(√I / (1 + √I))
Let us in this example consider a 0.1 M solution of MgSO4 with a pH of 7, meaning that the activity of the H+ion or {H+} is 10-7 . We start by writing down the concentration of ions in the solution:
Ion mol/L |
Mg2+ = 0.1 M |
SO42+ = 0.1 M |
H+ = 10-7 M |
By using the equation for calculating ionic strength we get that I ≈ 0.40. In these types of calculations the concentration of [H+] in itself is often discarded as it only accounts for a fraction of the total ionic strength.
If 0.40 is entered into the Güntelberg equation and the
necessary rearrangements are done, fH+ is
calculated to approx 0.634 or a fH+ of
10-6.80.
This value is used to calculate [H+] from
{H+}.
Still the pH value is 7 as {H+} is 10-7 as measured with a pH-meter. However, if the concentration of some compound in a equilibrium is calculated a value of [H+] of 10-6.80 should be used.