IX.4 Existence and Uniqueness with Nonhomogeneous Boundary Data 607
kvk
C
1
≤ ckfk
C
with c = c(n, Ω).
The example shown previously rules out the general validity of EC, but, on
the other side, it also suggests that condition (IX.4.7) can possibl y b e replaced
by the weaker one:
m+1
X
i=1
|Φ
i
| < cν, (IX.4.12)
for some positive constant c. In fact, this is indeed the case. Specifically, follow-
ing the work of Galdi (1991), by suitably modifying the Leray-Hopf extension
(IX.4.5), we shall prove existence of solutio ns under the sole condition that the
fluxes Φ
i
of v
∗
through each component Γ
i
of ∂Ω satisfy condition (IX.4. 12),
with a computable constant c that depends only on Ω and n.
3
However, if
∂Ω has more than one connected component, existence of solutions satisfying
merely (IX.4.6) with no restriction on the size of t he fluxes Φ
i
remains open.
4
To show our ma in result we need some preparatory steps.
Lemma IX.4.1 Let Ω be a bounded locally Lipschitz domain in R
n
, n = 2, 3 .
Denote by ω
i
, i = 1, . . . , m, the (bounded) connected components of R
n
− Ω
and set
ω ≡
m
[
i=1
ω
i
.
5
Then, given a ∈ W
1/2,2
(∂Ω) verifying the condition
Z
Γ
i
a · n = 0, i = 1, 2, . . . , m + 1, (IX.4.13)
where n is the outer normal to ∂Ω and
Γ
i
≡ ∂ω
i
, for i = 1, . . ., m, Γ
m+1
≡ ∂(Ω ∪ ω),
3
We wish to emphasize that, clearly, the condition on the “smallness” of Φ
i
does
not imply a priori “smallness” of v
∗
. On the other hand, if we assume that the
trace norm of v
∗
at the boundary is small with respect to ν, then existence with
nonzero small fluxes Φ
i
is proved in a direct elementary way.
4
For another approach t o existence with nonhomogeneous data, again due to Leray,
we refer the reader to the Notes for this Chapter. In that context, we shall also
give other existence results due to Amick (1984), Morimoto (1992) and Morimoto
and Ukai (1996), where the restriction (IX.4.7) can be removed.
5
Clearly, the number m is finite since ∂Ω i s compact and, furthermore,
min
i=1,...,m
dist (ω
i
, ∂(Ω ∪ ω)) > 0,
(cf. also Griesinger 1990a).