Environmental Engineering Reference
In-Depth Information
The pair of equations (3.3.14) will be the starting point for our applica-
tion of linear response theory.
According to the definition (3.2.10) of K BA ( t ), and eqn (3.2.12),
K BA ( ω )=2 BA ( ω )=
2 iG BA ( ω ) .
We may write
i
π
i
h
[ B ( t ) , A ]
χ BA ( ω ) e −iωt =
(3 . 3 . 15)
−∞
and, setting t = 0, we obtain the following sum rule :
h
π
[ B, A ]
χ BA ( ω ) =
,
(3 . 3 . 16)
−∞
which may be compared with the value obtained for the equal-time corre-
lation function
B A
B
A
, (3.3.7). The Green function in (3 . 3 . 14 a )
must satisfy this sum rule, and we note that the thermal averages in
(3 . 3 . 14 a ) and (3.3.16) are the same. Equation (3.3.16) is only the first
of a whole series of sum rules.
The n th time-derivative of B ( t ) may be written
dt n B ( t )= i
n
d n
n B ( t )
B ( t )
, B ( t )] .
L
L
H
ith
[
h
Taking the n th derivative on both sides of eqn (3.3.15), we get
) n χ BA ( ω ) e −iωt = i
n +1
i
π
n B ( t ) , A ]
(
[
L
.
h
−∞
Next we introduce the normalized spectral weight function
χ BA ( ω )
ω
1
χ BA (0)
1
π
F BA ( ω ) =1 .
(3 . 3 . 17 a )
The normalization of F BA ( ω ) is a simple consequence of the Kramers-
Kronig relation (3 . 2 . 11 d ). The n th order moment of ω , with respect to
the spectral weight function F BA ( ω ), is then defined as
F BA ( ω )=
,
where
−∞
BA =
−∞
ω n
ω n F BA ( ω ) dω,
(3 . 3 . 17 b )
which allows the relation between the n th derivatives at t =0tobe
written
χ BA (0)
( ) n +1
1) n
n B, A ]
BA =(
[
L
.
(3 . 3 . 18 a )
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