474 VII Steady Oseen Fl ow in Exterior Domains
fundamental solution. In particular, taking into account the properties of this
solution, every q-weak solution exhibits a paraboloidal wake region in the
direction of the positive x
1
-axis; see Remark VII.3.1.
Some interesting consequences of Theorem VII.6.2 are l eft to the reader
in the following exercises.
Exercise VII.6.1 Let v satisfy the assumption of Theorem VII.6.2. Show that, for
all sufficiently large R,
Z
∂B
R
`
v
2
+ ∇v : ∇v
´
≤ c
1
R
−(n−1)/2
Z
∂B
R
|p − p
0
|
2
≤ c
1
R
−(n−1)
.
Hint: Use Theorem VII.6.2 together with Exercise VII.3.1 and Exercise VII.3.4.
Exercise VII.6.2 The following result generalizes uniqueness Theorem VII.1.2.
Let v, p be a q-generalized solution to the Oseen problem (VII.0.3), (VII.0.2) in an
exterior domain Ω of class C
2
. Show that if f ≡ v
∗
≡ 0 then v ≡ 0, p ≡const.
Under these latter assumptions on the data, show that if v, p is a corresponding
smooth solution with v = o(1) as |x| → ∞, then v ≡ 0, p ≡ const.
Exercise VII.6.3 Show that the remainder σ in (VII.6.18)
1
has the following
summability properties:
σ ∈ L
q
(Ω
R
), for all q > n/(n − 1)
σ ∈ L
q
(Ω
R
), for all q > (n + 1)/n, if Φ ≡
R
∂Ω
v
∗
· n = 0
R > δ(Ω
c
).
Hint: As |x| → ∞, it is σ(x) = O(e(x)) if Φ 6= 0, and O( ∇E(x)) if Φ = 0 . Then use
the summability prop erties of e and ∇E.
Exercise VII.6.4 Let v, p be a smooth solution to the Oseen problem in an exterior
domain Ω ⊆ R
n
, n = 2, 3, with v = 0 at ∂Ω. Show that if v 6≡ 0, necessarily
kv − v
∞
k
2,Ω
= ∞, for any choice of v
∞
∈ R
n
.
4
Hint: Recall that E 6∈ L
2
(Ω
R
).
Exercise VII.6.5 (Olmstead & Gautesen 1968) Show the following “drag paradox”
for the Oseen approximation. Let B be a (smooth) body moving in a viscous liquid
that fills the whole space, with no spin and translational velocity λe
1
. Set Ω :=
R
3
− B, and denote by D(e
1
) := e
1
R
∂Ω
n · T , the drag exerted by the liquid on B
in t he Oseen approximation, where n i s the inner unit normal to ∂Ω (≡ ∂B). Prove
that t he drag is the same if the direction of the translational velocity is reversed,
namely, D(e
1
) = −D(−e
1
). Hi nt: Use (appropriately!) (VII.6.1) on the domain Ω
R
,
then let R → ∞ and employ the asymptotic properties of Theorem VII.6.2.
The representation formula (VII.6.1 6) allows us to obtain an interesting
asymptotic estimate for the vortici ty field ω = ∇×v in three dimensions. To
this end, we observe that, setting
4
If n ≥ 4 this statement no longer holds since E ∈ L
2
(Ω
R
).