A theorem is presented which gives the perturbation stream function \ ilde
Ψ(
r,θ) when a sphere (
r=
a) is introduced into an unlimited viscous fluid in axisymmetric motion obeying the Stokes equation, of which the stream function is
Ψ(
r,θ), where (
r,θ,\varphi) are the polar coordinates.
\ ilde
Ψ(
r,θ) is given by
\ ilde
Ψ(
r,θ)=\ ilde
Ψ1(
r,θ)+
a2\ ilde
Ψ2(
r,θ),
\ ilde
Ψ1(
r,θ)=\left(
a−\frac
r2a\
ight)\frac∂∂
Rψ
1(
R,θ)−\left(\frac32\frac
ra−\frac12\frac
r3a3\
ight)ψ
1(
R,θ),
\ ilde
Ψ2(
r,θ)=\left(
a−\frac
r2a\
ight)\frac∂∂
Rψ
2(
R,θ)−\left(\frac12\frac
ra+\frac12\frac
r3a3\
ight)ψ
2(
R,θ),
ψ
2(
r,θ)=−\fracsinθ4\sqrt
r∫
0r\sqrt
rω(
r,θ)
dr, ψ
1(
r,θ)=
Ψ(
r,θ)−
r2ψ
2(
r,θ),
where ω is the vorticity, and
R=
a2⁄
r.
This gives the stream sheets directly without recourse to manipulation of spherical harmonics, and is very simple when
Ψ(
r,θ) is irrotational, i.e. ω=ψ
2=0.
As examples of the applications of this theorem, the stream functions for uniform flow, source flow and parabolic flow past a sphere are derived.
View full abstract