Environmental Engineering Reference
In-Depth Information
Case (1): H n = 0
Define G 0 as the Green's function of the center part without
anharmonic interactions. When the center part is decoupled with
thermal leads, itsGreen's function g satisfies the equation
g r [ ω ] = ( ω + i δ ) 2 I D CC 1 . (3.31)
The influence of thermal leads is projected into the center part
in the form of self energy . Each thermal lead contributes a self
energy term
= L + R
(3.32)
The self energy of thermal leads is written as
α = D C α g αα D α C ( α = L, R), (3.33)
where the surface Green's function g αα is the Green's function of
isolated semi-infinitethermal lead. Itsatisfies
g r
) 2 I D αα 1 ( α = L, R). (3.34)
The surface Green's function can be calculated by a simple
iteration method [10] or by a more e cient decimation approach
[11].
Applying the Dysonequation, G 0 can becalculated from g :
G 0 [ ω ] =
[ ω ] = (
ω + i δ
αα
r [ ω ] 1
= ( ω + i δ ) 2 I D CC
( g r [ ω ]) 1
r [ ω ] 1
(3.35)
G 0 [ ω ] = G 0 [ ω ] ( g r [ ω ] ) 1 g < [ ω ] ( g a [ ω ] ) 1 G 0 [ ω ]
+ G 0 [ ω ] < [ ω ] G 0 [ ω ] (3.36)
For equilibrium states, fluctuation-dissipation theorem is satis-
fied and Eq. 3.36 can befurther simplified into
G 0 [
G 0 [
< [
] G 0 [
ω
=
ω
ω
ω
]
]
].
(3.37)
Case (2): H n =
0
Define G as the Green's function of the center part with anharmonic
interactions. The anharmonic interaction H n gives rise to a many-
bodyselfenergyterm n . G can beobtainedfrom G usingtheDyson
equation.
G 0 [ ω ] 1
n [ ω ] 1
G r [ ω ] =
= (
] 1
) 2 I
r [
r
ω +
i
δ
D CC
ω
]
n [
ω
(3.38)
 
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