06
Chapter
2
side (7.41)
is
to be integrated by parts. 17e are likely to have
from
(7.39)
(7.431
But then having multiplied by
k0
and integrated over
t
we find
from (7.38)
k
I
pods
I
ln[l
+
C
I
a(x,
r)exp
{IluCt)II+
C
I
U,(s)ds}
dt]
5
t
t
t
0
0
0
Using again inequalities (7.32) and (7.34) conclude:
Strengthening inequality (7.29) in the way similar to the previous
case we obtain the required estimate
We emphasize again that inhomogeneous boundary value problems
differ from problem (1.10)
-
(1.12)
in
the proof of estimate of
the form (7.44).
As
soon
as
this evaluation
is
obtained, auxiliary
relations (2.7). (2.111, (2.12)
will
give bounds
from
above and
from below for density and for derivative
ap/dx
in
L,(O,
T;
L2(51))
considered
as
parabolic and boundary conditions can be made homo-
geneous after the corresponding substitution.
As
a
result, in
equations there appear only lower terms, which don’t create any
additional difficulties.
Therefore equations for velocity and temperature can be
8.
STABILIZATION
OP
SOLUTIONS
UNDZR
INFINITE
TIILE
INCREASE
Stabiliza ion of viscous
as
equation solutions has been studied
in
works
156, 59,
69,
1394.
It
should be noted that the model of
barotropic liquid in the case
of
monotonous state equation
P(
P)
has
only been fully investigated. The fact of stabilization in the
Cauchy problem has been proved in [69]. Estimates of convergence
velocity have also been obtained in [56, 1391.
In considering stabilization problems, the proof of
a
priori evalu-