226 R. Farwig, H. Kozono and H. Sohr
such that g(t),N
∂Ω
=0for a.a. t ∈ (0,T). Then the inhomogeneous Stokes
system (1.4) has a unique very weak solution E satisfying (1.8), i.e.,
E ∈ L
s
(0,T; L
q
(Ω)) ∩ L
4
(0,T; L
4
(Ω)), (5.7)
and the a priori estimate
E
q,s;T
+ E
4,4;T
≤ c (F
0
q,s;T
+ F
0
12
7
,4;T
+g
L
s
(0,T ;W
−
1
q
,q
(∂Ω))
+ g
L
4
(0,T ;W
−
1
4
,4
(∂Ω))
+u
0
J
q,s
σ
+ u
0
J
4,4
σ
)
(5.8)
holds with a constant c = c(q, r, s,Ω) > 0 independent of T .
Proof. We apply Proposition 5.1 with the exponents s, q, r and 4, 4,
12
7
.Sincethe
very weak solution E of (1.4) in [3, 4, 5] is constructed in a finite number of steps
where each of them yields the same result for s, q, r and for 4, 4,
12
7
, it is easily seen
that the unique solution E satisfies (5.7), (5.8).
Remark 5.3. (i) In the case 4 ≤ s ≤ 8, 4 ≤ q ≤ 6andT finite the L
s
(L
q
)-conditions
in (5.6) imply the L
4
(L
4
)-conditions; then (5.6)–(5.8) simplify considerably.
(ii) For the system (1.1) consider data f =divF , F ∈ L
2
(0,T; L
2
(Ω)),
u
0
∈ L
2
(Ω) and boundary data g as in (5.6)
3
satisfying g(t),N
∂Ω
=0fora.a.
t ∈ (0,T). Then solve (1.4) with data f
0
=0,E
0
=0andg to get a (unique) very
weak solution E satisfying (5.7) and the a priori estimate
E
q,s;T
+ E
4,4;T
≤ c
g
L
s
(0,T ;W
−
1
q
,q
(∂Ω))
+ g
L
4
(0,T ;W
−
1
4
,4
(∂Ω))
.
Next, by Theorem 1.3, we find a weak solution v of the perturbed Navier-Stokes
system (1.12) with data f
1
= f =divF , F
1
= F ,andv
0
= u
0
satisfying (1.13),
(1.14). Then u = v + E is a weak solution of (1.1) split into a weak and a very
weak part, v and E. It is an easy exercise to write down a corresponding energy
estimate for u in terms of u
0
, f and g only.
(iii) Assuming more regularity on the boundary data g better properties of
u = v + E can be achieved; we refer to [3, 4] and to the forthcoming paper [6] for
such results.
In the second part of this Section we consider the assumption (1.15) and
Corollary 1.5. Assume that the bounded domain Ω ⊂ R
3
with ∂Ω=
L
∪
j=0
Γ
j
∈ C
1,1
has boundary components Γ
0
,...,Γ
L
with Γ
0
being the “outer” boundary of Ω
and Γ
j
, 1 ≤ j ≤ L, being the boundary of “holes” Ω
j
. Further, let the boundary
data g with g(t) ∈ W
1
2
,2
(∂Ω) for a.a. t ∈ (0,T) satisfy the restricted flux condition
Γ
j
g(t) · Ndo =0, 0 ≤ j ≤ L. (5.9)
Then, due to a construction in [14], there exists a solenoidal extension E = E
ε
∈
W
1,2
(Ω) of g for a.a. t ∈ (0,T) satisfying (1.16) (for arbitrary but fixed ε>0and