234 Lectures on Dynamics of Stochastic Systems
The corresponding steady-state probability distribution has the form
P(x, y) = C exp
−
λ
D
H(x, y)
, H(x, y) =
y
2
2
+ U(x). (9.20)
9.2.3 Systems of Hydrodynamic Type
In Sect. 1.1.3, page 10, we considered the general dynamics of simplest
hydrodynamic-type systems (HTS). Now, we consider these systems in terms of the
statistical description.
Hydrodynamic-type systems with linear friction are described by the dynamic
equations
d
dt
v
i
(t) = F
i
(v) − λ
(i)
v
i
(t) (i = 1, . . . , N), (9.21)
where λ
(i)
is the friction coefficient of the i-th component of the N-dimensional vector
v
1
and F
i
(v) is the function quadratic in v and having the following properties:
(a) v
i
F
i
(v) = 0,
energy conservation holds at λ
(i)
= 0:
d
dt
E(t) = 0, E(t) =
v
2
i
(t)
2
;
(b)
∂
∂v
i
F
i
(v) = 0,
conditions of the Liouville theorem are satisfied at λ
(i)
= 0, and this equality
is the equation of incompressibility in the phase space.
Equilibrium Thermal Fluctuations in the Hydrodynamic-Type Systems
Here, we dwell on a class of phenomena closely related to the Brownian motion;
namely, we dwell on equilibrium thermal fluctuations in solids.
Microscopic equations describe the behavior of physical systems only in terms of
spatial scales large in comparison with the molecule free path in the medium and tem-
poral scales great in comparison with the time intervals between molecule collisions.
This means that macroscopic equations adequately describe the behavior of systems
only on average. However, in view of molecule thermal motion, macroscopic vari-
ables are in general terms stochastic variables, and a complete macroscopic theory
must describe not only system behavior on average, but also the fluctuations about the
average.
1
In the general case, the dissipative term in Eq. (9.21) has the form λ
ik
v
k
. However, we can always choose
the coordinate system in which two positively defined quadratic forms – energy E = v
2
i
/2 and dissipation
λ
ik
v
i
v
k
– have the diagonal representation. The form of Eq. (9.21) assumes the use of namely such a
coordinate system.