Approximations in Chemical Equilibrium (add a weak acid HA into pure water)

  • #1
SilverSoldier
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Suppose we add a weak acid HA into pure water, so that upon addition its initial concentration is c. The following equilibria should establish in the system. $$\text{HA}+\text{H}_2\text{O}\rightleftharpoons\text{H}_3\text{O}^++\text{A}^-$$ $$2\text{H}_2\text{O}\rightleftharpoons\text{H}_3\text{O}^++\text{OH}^−$$ Let ##K_a## and ##K_w## respectively be the equilibrium constants for these processes. We can express the composition of the system before and after equilibrium as follows. Let ##a## be the concentration of ##\text{H}_3\text{O}^+## and ##\text{OH}^−## already present in the system due to the autoionization of water initially; i.e., ##a=\sqrt{K_w}##.

##\text{HA}##​
##\text{H}_3\text{O}^+##​
##\text{A}^-##​
Initial concentration
##c##​
##a##​
-​
Change in concentration
##-p##​
##+p##​
##+p##​
Equilibrium concentration
##c-p##​
##a+p+q##​
##p##​

##\text{H}_2\text{O}##​
##\text{H}_3\text{O}^+##​
##\text{OH}^−##​
Initial concentration
-​
##a##​
##a##​
Change in concentration
-​
##+q##​
##+q##​
Equilibrium concentration
-​
##a+p+q##​
##a+q##​

Thus, we can obtain the following expressions at equilibrium. $$K_w=\left(a+p+q\right)\left(a+q\right)$$ $$K_a=\dfrac{\left(a+p+q\right)\left(p\right)}{c-p}$$ Taking ##r=a+q##, we obtain the following cubic equations in ##p## and ##r##. $$p^3K_a+p^2\left(K_a^2−K_w−cK_a\right)−2pcK_a^2+c^2K_a^2=0$$ $$r^3K_a+r^2\left(cK_a+K_w\right)−rK_aK_w−K_w^2=0$$ Now, as the acid begins to dissociate, because there is ##\text{H}_3\text{O}^+## already present in the system, the reverse "association" process should start off faster, so it should take lesser time for its rate to increase up to a significant value bringing the system to equilibrium, allowing time only for fewer molecules of the acid to dissociate.

At the same time, because ##\text{H}_3\text{O}^+## is being "removed" by the reverse autoionization process as it forms, the system should be trying to keep the ##\text{H}_3\text{O}^+## concentration below whatever value it would otherwise have risen to in the absence of autoionization.

The fact that the reverse autoionization process is triggered as the reaction proceeds should mean that ##\text{OH}^-## ions in the system should be being consumed, so by the time equilibrium is attained, its concentration must be lesser than the initial value. This means that ##r## in the equation above must be less than ##a##, so if ##a## can be considered small, then ##r^3## must be even smaller, and the effect of the ##r^3## term in the equation should be negligible. It should therefore be possible the reduce it to $$r^2\left(cK_a+K_w\right)−rK_aK_w−K_w^2=0$$ The following is a plot I made of the above equations with the ##x## axis representing ##c## and ##y## axis representing ##r##. The ##r^3## term is neglected in the orange curve, and not neglected in the black curve (##K_a=5## and ##K_w=0.5## here).

geogebra-export.png

The orange curve greatly deviates from the black curve for small concentrations. Is this possible, because ##r## must always be less than ##a## for all concentrations? Have I made an error somewhere? Is it wrong to neglect the ##r^3## term?

By the way, I have not seen calculations being made taking the ##\text{H}_3\text{O}^+## and ##\text{OH}^-## concentrations already present in the system initially into consideration. Where the autoionization of water is not neglected it is always assumed that there are no ##\text{H}_3\text{O}^+## and ##\text{OH}^-## ions present in the system before equilibrium. Why is this? Is there anything wrong with saying it is already present?
 
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  • #2
In general when systematically finding equilibrium nobody cares about initial concentrations of anything. Total (analytical) concentrations and mass balances are all that matters (apart from Ka/Kb and charge balance).

For nitpickers one of the mass balances should be that of water itself, but it makes the calculations a bit more difficult, as it forces the solver into mass balances of elements, not of substances. The most general equilibirum programs do that, those specialized for pH calculations don't, as it is enough to add Kw to make sure autoionization of water is part of the system.

While you approach - starting with ICE tables - should in principle produce the same results, I have never seen it used that way. The general approach is actually simpler and easier to use.
 
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Likes BillTre and berkeman
  • #3
Borek said:
In general when systematically finding equilibrium nobody cares about initial concentrations of anything. Total (analytical) concentrations and mass balances are all that matters (apart from Ka/Kb and charge balance).

For nitpickers one of the mass balances should be that of water itself, but it makes the calculations a bit more difficult, as it forces the solver into mass balances of elements, not of substances. The most general equilibirum programs do that, those specialized for pH calculations don't, as it is enough to add Kw to make sure autoionization of water is part of the system.

While you approach - starting with ICE tables - should in principle produce the same results, I have never seen it used that way. The general approach is actually simpler and easier to use.
How are we able to simplify the above cubics to simpler equations that can be solved? How do we, for example, simplify the cubic in ##p## to obtain the usual result that ##p=\sqrt{cK_a}##?
 
  • #4
Look here for a review of methods used: https://www.chembuddy.com/?left=pH-calculation&right=toc

Broadly speaking the main idea is the "5% rule" - if in a sum x+y one component (say y) is less than 5% of the other we try to ignore it and assume x+y≈x. That typically decreases the degree of the resulting polynomial.
 

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