376 15. Nonlinear Parabolic Equations
Both the PDE and the boundary conditions may have t-dependent coefficients.
For example, the PDE might be
(6.99) u
t
D A.t/u
xx
:
Some studies of these problems can be found in Chap. 8 of [Fr1]andin[KMP],
where particular attention is paid to the nature of the dependence of the solution
on the coefficient A.t/,assumedtobe>0.
There are also two-phase Stefan problems, where the ice is not assumed to be
at temperature 0, but rather at a temperature u
i
.t; x/ 0, to be determined as
part of the problem. Furthermore, these problems are most interesting in higher-
dimensional space. More material on this can be found in [Fr2].
Exercises
1. If v solves (6.3)–(6.4), show that
d
dt
s
v.t/
2
L
2
D
2
s
v
x
.t/
2
L
2
I
hence
s.t/kv.t/k
2
L
2
C 2
Z
t
0
s./
1
v
x
./
2
L
2
d Dkf k
2
L
2
:
2. If u satisfies (6.1)–(6.2), show that
(6.100) s.t/
2
D 1 C 2a
Z
1
0
xf .x / d x 2a
Z
s.t/
0
xu.t; x/ dx:
Compare the upper bound on s.t/ this gives with (6.68).
Show that, conversely, (6.1)and(6.100)imply(6.1)–(6.2). This result, or rather its ana-
logue in the more general context of the nonhomogeneous boundary condition (6.97),
played a role in the analysis in [CH].
7. Quasi-linear parabolic equations I
In this section we begin to study the initial-value problem
(7.1)
@u
@t
D
X
j;k
A
jk
.t;x;D
1
x
u/@
j
@
k
u C B.t; x; D
1
x
u/; u.0/ D f:
Here, u takes values in R
K
, and each A
jk
can be a symmetric K K matrix;
we assume A
jk
and B are smooth in their arguments. We assume for simplicity
that x 2 M D T
n
,then-dimensional torus. Modifications for a more general,