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.
 
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