Next: Turbulence in eddy space
Up: The Kolmogorov turbulence theory
Previous: Introduction
In 1938, von Kármán and Howarth proposed an equation governing
homogeneous isotropic turbulence whose original form is written
as[3]
 |
(1) |
In this equation
and
are
instantaneous velocity fluctuation at
and
, respectively,
overbar (
) denotes the conventional (ensemble) average and
denotes the Navier-Stokes equation written in terms of the instantaneous fluid quantities
 |
(3) |
where
and
are the average velocity and pressure,
respectively,
is the kinematic viscosity, and
denotes
nabla vector. Likewise
is defined by Eq.(2) in
which (
) is replaced with (
).
Eq.(1) is an equation in 6-D physical space and time, namely, has seven
independent variables (
).
The classical theory[3] chose to discuss homogeneous and
isotropic turbulence to
reduce independent variables to (
). We can
show, however,
that the equation can be renovated to be available for
inhomogeneous turbulence as well by introducing separation of
variables, together with a closure condition which seems
plausible intuitively.
The actual derivation proceeds as follows: Eq.(1) in which
is decomposed into average and fluctuating parts using (3),reads
 |
(4) |
where
 |
(5) |
together with
defined as in Eq.(1). Upon
substituting Eq.(5) into Eq.(4) we see that the equation consists of
terms of double and triple fluctuation correlations,
which we will decompose as
where
is the wave number,
is the characteristic length of flow
geometry, R.P. denotes taking real part, and subscript
runs 1
through 4. A supplementary definition
 |
(8) |
stands for the pressure fluctuation.
It is more convenient for later use to employ the following alternative
expressions:
It is to be noted that there is no a priori reason why the double and
triple correlations are to be expressed in terms of the same
. At this point it is simply invoked as the closure condition to
truncate the chain of equations at the level of Eq.(4). This closure can
be justified only through the quality of outcome as to whether it fits
with physical reality of turbulence.
With these preliminaries, Eq.(4) with assumption (6',7') substituted
into, leads to the form typical of separation of variables, here into
(
,t) and (
,t), respectively;
![\begin{displaymath}
\int_{-\infty}^{\infty}
d\mbox{\boldmath {$k$}}g_j\hat{g}_...
...(\widehat{\mbox{ns}})_l^{(0)}}_{\displaystyle =\;-i\omega}]=0
\end{displaymath}](img38.png) |
(9) |
where
is the separation parameter having the dimension of the
frequency, and
stands for
, and
is defined by
 |
(10) |
with
Imaginary factor
as appearing in Eq.(9) reflects the statistical symmetry of the tensor
, which is met under the following additional condition
![\begin{displaymath}
g_l(\hat{\mbox{\boldmath {$x$}}},-\mbox{\boldmath {$k$}})=[g_l(\hat{\mbox{\boldmath {$x$}}},\mbox{\boldmath {$k$}})]^*
\end{displaymath}](img47.png) |
(11) |
In fact, then, the two terms inside[ ] of integral (9) are
commutable to each other through taking complex conjugate(*), if
is purely imaginary. Thus we are led to the assertion that
the only equation that need to be solved is
 |
(12) |
To go further
from this point on, we need to have relationship between
frequency
introduced as the separation parameter and wave number
by which the solution is constructed in the form of bilinear
integral. Physically they are related to each other by the dispersion
relation
. Or, instead, we may introduce phase velocity
by
 |
(13) |
with no loss of generality. In fact, its constancy does not mean the
turbulent eddies being assumed as nondispersive. For the
unsteady term in the equation
is
responsible for the dispersive part, if any.
Owing to the convolution form of integral (10) periodic factor drops off
from Eq.(12) despite its nonlinear structure by putting
 |
(14) |
thereby we have the following equation governing its amplitude
,
 |
(15) |
where
with
 |
(17) |
It is readily checked that expressions defined by (15) and (10) are related to each other by
Several remarks are in order with regards to physical implications of
variables having appeared in this section: Amplitude function
as
obeying Eq.(14) is essentially complex and is not an
observable. It is related to the observable quantity of fluctuation
correlation through
 |
(18) |
as is confirmed by (6'),(11)and (13). Its complex variable structure has its
origin in Eq.(9)
where the imaginary unit
is introduced from the symmetry postulate
of statistical mechanics[2] for correlation tensor (18). We may
note some coincidental parallelism to Schroedinger's wave equation where
the imaginary factor secures the corresponding tensor to be Hermitean as
it should.
The most crucial on which this paper rests is the soundness of the basis
of Eq.(1). Originally it was a product of intuition by Theodore von
Kármán without any `first principle' ground shown in the
paper[3]. In fact, then, any linear combinations of
would be claimed as equally qualified. Firm basis is provided by nonequilibrium statistical mechanics[4] to justify that the linear combination only of the form (1) is consistent with Liouville's equation, namely, the equation of continuity in the phase space of Hamiltonian mechanics. .
Next: Turbulence in eddy space
Up: The Kolmogorov turbulence theory
Previous: Introduction