A chemist or engineer not only want to know the reactivity of chemicals, but also the extend of the reaction. When reactants are put together, how far will the reaction go? How long will it take to reach an equilibrium state? In dealing with these concerns, the concept of equilibrium constant is devised. In order to get a good approximation for the prediction of a system, we use concentrations or activities to evaluate the equilibrium constant.
[C]c [D]d
---------------- = Keq
[A]a [B]b
where [A], [B], [C], and [D] are stoichiometric concentrations of A, B, C,
and D respectively.
However, dilute solutions and concentrated solutions have slight differences, and a more precise method of calculating and defining the equilibrium constant is desirable. For such an approach, the reactivities of A, B, C, and D are used in place of the concentrations in the definition of K. The reactivity of A ({A}) is proportional to [A], and the proportional constant in most text is a gamma, which is called the activity coefficient
The reactivities based on concentrations given above work well for non-electrolytes (or molecular compounds). In dilute solutions, the activity coefficient is unity.
In solutions of electrolytes, the interactions of charges require some special consideration.
The dissociation of an electrolyte MxXm is,
For very concentrated solutions, using concentration based on weight of solvent may offer a better approximation than using concentration based on volume. However, at this level, we are only introducing the concept of ionic strength for the calculation of the activity coefficient.
Example 1
Solution
Using the simple formula for ionic strength I given above, we have
Further exercise
What is the ionic strength for a 1.0 molar CaCl2 solution?
Ans: 3.
Example 2
Solution
For this solution, the concentrations are:
[La3+] = 2.0 M
[SO42-] = 3.0 M
[Ca2+] = 1.0 M
[Cl-] = 2.0 M
Discussion
Note that the sum is taken over all ions.
Example 3
Solution
Using the limiting Debye-Huckel law,
Discussion
When the coefficient 0.90, the activity is 90% of the concentration.
The activity coefficient for Ca2+ under the same condition is
0.63. The activity is much reduced from the higher charge on the ion.
The introduction of activity is to make the equilibrium constant concept (or laws) to be able to be applied to a wider range. By assuming equilibrium constants and other physical properties unchanged, the activity coefficients at different concentrations are aumatically assumed to change. Thus, we can measure the physical property and estimate the activity coefficients at various concentrations.
For example, by measuring the boiling points and freezing points of solutions with various concentrations, we can estimate the apparent activities of a solute at these concentrations. Dividing the activities (such as {A}) by the stoichiometric concentrations (such as [A]) gives the activity coefficients g, since