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)