
5.9 Onsager’s extremum principle 105
One could just as well invert the kinetic equation, Eq. (5.129), obtaining
X
j
=
k
R
jk
J
k
(5.131)
σ ≡
J
j
X
j
=
j
J
j
k
R
jk
J
k
=
j
k
R
jk
J
j
J
k
. (5.132)
The new kinetic coefficients represent the resistance or friction of the processes whereas
the L coefficients represent their mobilities. The set of R coefficients are directly obtain-
able from the set of L coefficients. If there were no cross coefficients one would simply
get
σ =
(1/L
jj
)J
2
j
. (5.133)
The right-hand side of Eq. (5.132) could have been formulated directly by assuming that
the rate of entropy production is a function of the fluxes and developing that function
in a Taylor series. Evidently, the first term in the series can be omitted because there
can be no entropy production without a flux. The second term can also be omitted in
view of the second law because that term is linear in the fluxes and would make the
entropy production change sign if the direction is reversed, which is not allowed since
the entropy production of spontaneous processes must be positive. The right-hand side
of Eq. (5.132) represents the third term except for a factor
1
/
2
. Onsager thus defined a
function
(J, J ) ≡
1
/
2
j
k
R
jk
J
j
J
k
. (5.134)
He called it dissipation function because 2 is not only equal to the rate of entropy
production, σ . Under isobarothermal conditions 2T actually represents the rate of
Gibbs energy dissipation. Without any physical argument, Onsager then formulated a
new function, = σ − and examined under what conditions its value is maximized.
Forasystem with gradual variations of the local state he found the answer by variation
analysis. We shall avoid this complication by limiting the derivation to a small volume
with approximately uniform conditions or to a system with more than one homogeneous
region.
Comparison of Eq. (5.132) and first part of Eq. (5.134) demonstrate that is equal to
σ/2. However, they represent different functions. This is best understood by multiplying
them with T. According to Eq. (5.53), T d
ip
S is equal to the decrease in Gibbs energy of
the system if it is completely isolated, and −T σ is the time derivative of Gibbs energy,
˙
G. The quantity σ thus represents a rate of change of the state of the system. On the
other hand, T with defined by Eq. (5.134) shows how the Gibbs energy is being
dissipated by friction. The new function is thus defined as
= σ − =
j
X
j
J
j
−
1
/
2
j
k
R
jk
J
j
J
k
. (5.135)
We shall now consider a purely hypothetical case where the fluxes can vary under fixed
forces and the coefficients, if they are not constant, vary with the forces but not with the