The leading disturbance in sphere Stokes flow has size . Consequently viscous diffusion has size , background advection has size , and their ratio is . Even if the sphere Reynolds number is small, this ratio becomes order one at . Thus the Stokes approximation is nonuniform at distances of order . At that outer distance the disturbance itself is small relative to , so self-convection is smaller than background advection and the Oseen approximation is appropriate:
Write . It is sufficient outside the origin to impose and : these give zero divergence, and substitution into momentum gives . With , differentiation yields
A decaying radial choice is . Therefore
The exponent is nonpositive, so this scalar decays at infinity, including as directly downstream. In the overlap ,
Choosing cancels the first term's gradient in . The remaining leading velocity is
Matching fixes . Thus the potential-source and wake decomposition of sphere Oseen flow is
Its pressure is , the sign appropriate to a fixed sphere in an incident flow. The velocity decays in every direction and matches the requested leading inner disturbance; the sphere's potential-dipole term enters a higher matching order.
The scalar potential is a point source: , so integration over a centred sphere gives
To see the fluid wake, take downstream along and transverse radius . For , , giving
The fluid wake is concentrated within . Its integrated mass deficit is , balancing the outward potential-source mass flux. The corresponding momentum deficit is
which equals the leading sphere drag. The Gaussian integral used here is .
The PDF labels as the mass-source strength, but this has dimensions of force. The actual mass-source strength is ; is the momentum deficit or drag. The decomposition above supplies both quantities and identifies the printed normalization error.

Articles by others on the same topic (0)

There are currently no matching articles.