How is equilibrium constant formed? How can an such an arbitrary expression have souch meaning?
Although several answers give the equilibrium constant in terms of the Gibbs energy,
ΔG°=-RTln(K
eq)
there is a bit more to the story. I will do this without discussing activities. Consider the generic equation,
2A + B
3C
Where A, B and C are chemical species. We can find these on tables that give us the Standard Gibbs Energies of formation, which we can call, ΔG°
A, ΔG°
B, ΔG°
C. Recall that these are pressure (or in solution concentration) dependent and the relationships are,
ΔG
A =ΔG°
A –RT lnP
AΔG
B =ΔG°
B –RT lnP
BΔG
C =ΔG°
C –RT lnP
CLet us now write down the change in Gibbs energy for the reaction:
ΔG
Rx= 3ΔG
C - 2ΔG
A- ΔG
B = 3ΔG°
C - 2ΔG°
A- ΔG°
B + 3RT lnP
C - 2RT lnP
A - RT lnP
BΔG
Rx= ΔG°
Rx+ RT lnP
C3- RTlnP
A2 - RT lnP
B= ΔG°
Rx+ RT ln[P
C3/(P
A2P
B)]=
ΔG
Rx= ΔG°
Rx+ RT ln[Q]
Where Q is the quotient product: it has the same form as the equilibrium constant but the pressures are not the equilibrium pressures, but just the pressures that happen to be present,
Q= P
C3/(P
A2P
B)
K
eq as pressures become their equilibrium values.
You should easily be able to see that the ΔG
Rx gets more or less negative as those pressures change in the quotient product, thereby showing that Le Chatelier’s principle raises or lowers the Gibbs energy, shifting the equilibrium one way or the other.
It also becomes the equilibrium constant when the pressures are their equilibrium pressures. However at equilibrium there is no change and the ΔG
Rx is zero, hence
ΔG
Rx= ΔG°
Rx+RT ln[Q]
0= ΔG°
Rx+ RT ln[K
eq]
or
ΔG°
Rx=- RT ln[K
eq]
In this you can see where the form of the equilibrium constant comes from.