A force-driven rigid particle with surface has a leading translating sphere in Stokes flow with . Expanding the no-slip boundary condition gives the first-order surface velocity , where . The first-order resultant force and torque vanish when the applied load is fixed. The Lorentz reciprocal theorem for Stokes flow, using the uniform surface traction in translating-sphere Stokes flow, therefore gives . For with symmetric traceless , the isotropic fourth moment gives . A rotating-sphere test similarly gives , which vanishes for an inversion-symmetric deformation.
Write the supplied velocity in the radial form
At , and , giving the no-slip boundary condition . At infinity and the supplied gauge-fixed pressure tends to zero. These are the laboratory-frame conditions for a sphere translating through otherwise quiescent fluid.
The exterior Stokes equations can also be checked directly:
and
To compute surface traction in translating-sphere Stokes flow, let point from the sphere into the fluid. At the surface, , and . Hence
Substitute into the Newtonian fluid stress tensor. Its viscous contribution to the surface traction is , so the normal part cancels the pressure contribution:
The vector is constant over the entire sphere in the stated pressure gauge. Integrating it gives the fluid's drag force on the sphere,
This is Stokes's law. On an exterior fluid domain the outward domain normal at its inner boundary is ; that distinction will matter in the reciprocal calculation.
Work in the frame in which the distant fluid is stationary, and take the pressure at infinity as zero. In the Unscaled Papkovich–Neuber representation, choose the harmonic potentials
Both are harmonic away from the sphere's centre: is harmonic there and . Substitution into , , gives the translating sphere in Stokes flow:
Here . At the coefficients of sum to one and those of sum to zero, so the no-slip boundary condition is satisfied. The field decays at infinity. The Papkovich–Neuber representation enforces the Stokes equation and incompressibility, and Uniqueness of Stokes flow identifies the physical solution.
Differentiate radially at fixed direction :
On the surface, multiplying the specified Newtonian fluid stress tensor by the outward normal from the solid gives
Thus the surface traction in translating-sphere Stokes flow is uniform and the fluid's force on the sphere is
This is the Stokes drag law; an external force of the opposite sign maintains the motion.
Stokes's law Created 2026-10-14 Updated 2026-10-20
For an isolated rigid sphere of radius moving at velocity relative to a distant uniform Newtonian fluid, the drag force exerted by the fluid is
The assumptions are steady incompressible flow, constant dynamic viscosity , an unbounded surrounding fluid, the no-slip boundary condition, and a small diameter-based particle Reynolds number, . Integrating the surface traction in translating-sphere Stokes flow gives the factor : the disturbance pressure contributes to the drag magnitude and the viscous shear stress contributes . See Richard Fitzpatrick, Axisymmetric Stokes Flow Around a Solid Sphere, equations 10.120–10.129.
The result is linear drag: doubling doubles the drag force, and doubling at fixed also doubles it. The required power is , all supplied to viscous dissipation. Density enters the check of the particle Reynolds number, although it does not appear in the leading drag formula.
Nearby walls or other particles change the hydrodynamic resistance matrix and invalidate the isolated-sphere coefficient, even at very small Reynolds number. Finite Reynolds number introduces inertia corrections; the Oseen approximation resolves the distant region where the leading Stokes flow approximation ceases to be uniform. A clean gas bubble has tangential slip and instead obeys clean-bubble Stokes drag, with coefficient in its spherical, negligible-internal-viscosity limit. See H. K. Moffatt, Six Lectures on General Fluid Dynamics, section 3.4 for the sphere solution and its small-Reynolds number limitation. The continuum mechanics and boundary assumptions must also remain valid as the particle becomes very small.
Balancing this Stokes drag law against gravity and buoyancy gives the Stokes settling velocity of an isolated rigid sphere.