8.
Bibliographical
notes
333
Given such an estimate, the Cauchy problem (7.1) can be solved by a standard
limiting process. Indeed by Theorem 2.1 the sequences
{
f)
}
-Un
,
f)xi
nEN
i =
1,2,
...
,N,
are locally equibounded and equi-HOlder continuous in
RN
x (0, Tr). This gives
the existence
of
a unique solution in ET
r
•
The
largest time
of
existence can be
calculated from
(7.8) by letting r
-+
00.
In particular the solution to (7.1) is global
in time
if
. j uo(x)
lim
sup
>./(
-2)
dx =
O.
f'-OO()
p>r P P
Kp
8. Bibliographical notes
Theorem 2.1 is taken from [41]. A weaker version
of
(2.2) in
I-space
dimension
is due to Kalashnikov [58]. It is remarkable that in
(2.4) one can also control the
behaviour
of
the space-gradient IDul as Ixl-+
00.
Since IDul
2
is a non-negative
subsolution
of
a porous
medium-type
equation (see (1.8)
of
Chap. IX) the same
techniques yield a version
of
(2.2) for such degenerate p.d.e. The analog
of
(2.2)
for the porous medium equation is due to
Benilan-Crandall-Pierre
[10] in the
context
of
an existence theorem. A rather general version is in [4]. Perhaps the
most relevant estimate
of
Theorem 2.1 is the integral gradient bound (2.3) proved
in [41]. A version
of
such a local bound, for the porous medium equation is in [4]
and reads
jlDuml
dxdr
~
-yt
1
/"p1+w!=r
"lu"I!;.:~l,
K.
=
N(m
- 1) + 2,
Kp
where -y=-y(N, m) and
- j u(x,t)
IIIulllr,T-E =
sup
sup
,./(m-l)
dx.
O<tST~p>r
p
Kp
The estimate holds for
small
time intervals and for general non-linearities.
We
refer to [4] for details. There is no analog
of
(2.4) for the porous medium equation.
Theorems 4.1 is taken from [41]. The analog for the porous medium equations is
in [6] and for general non-linearities [4]. It would
be
desirable to have a version
of
the uniqueness Theorem 6.1 for initial data measures. This would parallel the
analogous theory for the heat equation.