210 12 Integral Formulae and Distribution Functions
in the ordered and the isotropic state is
sa=−kB
∫
fln(f/f 0 )d^2 u=−kB〈ln(f/f 0 )〉. (12.36)
Use off=f 0 ( 1 +Φ),cf.(12.16) yields
sa=−kB〈( 1 +Φ)ln( 1 +Φ)〉 0. (12.37)
With the help of the power series expansion
( 1 +x)ln( 1 +x)=x+
∑∞
n= 2
(− 1 )n
1
n(n− 1 )
xn,
and due to〈Φ〉 0 =0, the entropy (12.37) is equivalent to
sa=−kB
∑∞
n= 2
(− 1 )n
1
n(n− 1 )
〈Φn〉 0. (12.38)
The first few terms in this series are
sa=−kB
(
1
2
〈Φ^2 〉 0 −
1
6
〈Φ^3 〉 0 +
1
12
〈Φ^4 〉 0 ±...
)
. (12.39)
In lowest order inΦ, the orthogonality and the normalization (12.15) of the expansion
tensors imply
sa=−kB
(
1
2
∑∞
= 1
aμ 1 μ 2 ···μaμ 1 μ 2 ···μ±...
)
. (12.40)
The dots stand for terms associated with third and higher powers inΦ. Examples for
the role of higher order terms are discussed in the Exercise15.1.
12.2.7 Fokker-Planck Equation for the Orientational
Distribution
In the absence of any orientating torque and for a spatially homogeneous system, the
distribution function for the orientation of (effectively) uniaxial particles immersed
in a fluid obeys the dynamic equation, frequently called orientationalFokker-Planck
equation,
∂f(u)
∂t
−ν 0 LμLμf(u)= 0. (12.41)