The Minimum-dissipation theorem for Stokes flow compares fields with fixed boundary velocities. Introducing a freely moving rigid inclusion can reduce velocity and total power at fixed applied force while increasing the resistance at fixed velocity. Extending the inclusion's rigid velocity through its interior adds zero viscous dissipation and gives a trial field in the domain without that inclusion, proving the fixed-velocity comparison.
Write and take to be the dynamic viscosity. The Papkovich–Neuber representation of a homogeneous Stokes flow uses a harmonic vector potential and harmonic scalar potential :
These formulas give incompressibility because , and give , the Stokes equation away from forcing.
For a point force represented by a Dirac delta distribution, rotational covariance and the Linearity of Stokes flow suggest a vector monopole proportional to : is a harmonic function outside the origin, and its slow decay gives the required nonzero resultant force. Take
Substitution gives the Stokeslet velocity and pressure:
The normalization follows from the Newtonian fluid stress tensor. Differentiating the velocity gives the rate of strain and vorticity of a Stokeslet:
Here . Thus . On a sphere enclosing the origin, its outward traction integrates to , so in the distributional sense. All displayed fields away from the point force have .
For a sphere in a uniform straining Stokes flow, centre the sphere at the origin and write the ambient velocity as , with and . Faxén's first law and Faxén's rotational law give zero translation and rotation. To impose the no-slip boundary condition, use the decaying harmonic dipole and quadrupole potentials
Trace freedom makes harmonic, and each component of is harmonic. The Papkovich–Neuber representation gives
At , the coefficient of must give , while the extra radial term must vanish. Hence and , giving the complete disturbance
The total velocity vanishes on the sphere and tends to the imposed strain at infinity. This field has no Stokeslet or rotlet contribution, consistent with a force-free, torque-free sphere. Its leading far field is the radial stresslet .
Now put the first sphere at and the second at , where , and let . The first sphere's leading disturbance is its Stokeslet. The rate-of-strain tensor and vorticity incident on the second sphere are
The second sphere translates with the local flow and rotates with half its local vorticity. Its force-free and torque-free conditions therefore remove any reflected force or torque monopole. The incident strain produces the stresslet just obtained. Since
its velocity at the first centre, using the relative vector , is
Faxén's first law then gives the self-mobility correction from a distant force-free sphere:
Finite-size terms and further reflections are beyond the leading order retained in this method of reflections for Stokes flow.
Only the imposed force does work, so the viscous dissipation is . With , define and . At fixed ,
so the leading change is negative when . The direction is held fixed in taking .
The fixed-force comparison of minimum viscous dissipation distinguishes the prescribed force from prescribed boundary velocity. Indeed,
and hence
At the actual reduced velocity, adding the second sphere increases the dissipation relative to an isolated translating sphere at that same velocity, exactly as required by the Minimum-dissipation theorem for Stokes flow. One can extend the two-sphere velocity rigidly into the second sphere, adding zero strain and producing an admissible trial field in the domain without it. The reflected angular velocity of the first sphere contributes only a higher-order squared rotational power to this comparison.
Finally hold the second sphere's angular velocity at zero. Faxén's rotational law requires the applied couple
The resulting rotlet adds at the first centre
This is the additional rotational constraint correction to sphere mobility. Including the strain reflection, the total leading change relative to the isolated velocity is
For motion parallel to the line of centres the constraint adds nothing at this order; for transverse motion it supplies an extra resisting correction.
Let be the Stokes flow and let be any other admissible incompressible flow with the same no-slip boundary condition on the sphere and the same decay at infinity. Put
Then and on the sphere. The viscous dissipation satisfies
For the Stokes stress
incompressibility of gives
The divergence theorem, the homogeneous boundary data, decay at infinity, and give
Therefore
This proves the Minimum-dissipation theorem for Stokes flow.