Environmental Engineering Reference
In-Depth Information
1.
G
>
and
G
<
: they are usually regarded as correlation functions,
and are directly related to observable physical quantities (e.g.,
thermal current, density of states and so on) and dynamic
properties.
2.
G
r
and
G
a
: they have good analytical properties, facilitate
calculations of physical response, and also have simple
relations to observablephysical quantities.
In equilibrium or steady states, the system is time-translation
invariant. The Green's functions depend only on the difference in
time. Then it is more convenient to go from time space to frequency
space through Fourier transformation:
+∞
G
(
t
)
e
i
ω
t
dt
.
ω
=
G
[
]
(3.22)
−∞
In frequency space, there are relations:
G
<
[
G
>
[
]
T
−
ω
=
ω
]
(3.23)
G
<
[
ω
]
†
=−
G
<
[
ω
]
(3.24)
]
∗
G
r
[
G
r
[
−
ω
]
=
ω
(3.25)
G
r
[
ω
]
†
=
G
a
[
ω
]
(3.26)
For steady states, only two Green's functions are linearly inde-
pendent. Thisnumberdecreases to onefor equilibriumstates, since
equilibrium systems satisfy the fluctuation-dissipation theorem,
whichgivesrisetoanadditionalrelationbetweenGreen'sfunctions.
G
<
[
)(
G
r
[
G
a
[
ω
]
=
f
(
ω
ω
]
−
ω
]),
(3.27)
where
f
is the Bose-Einstein distribution function. The correlation
function
G
<
contains information of fluctuation, while
G
r
−
G
a
describes dissipation of the system. The fluctuation-dissipation
theorem tells us that fluctuation is proportional to dissipation in
equilibriumstates.