The force-free Stokes flow equations are
Put . Then , so write
Incompressibility requires . Since for harmonic , take
This gives the Papkovich–Neuber representation
For a rotating sphere the boundary data are toroidal, tangent to every concentric sphere, linear in , and decay at infinity. The harmonic vector field
has precisely these symmetries; it is harmonic because its components are derivatives of , and . Hence
The first pressure argument is . Independently, this velocity is harmonic, so the Stokes momentum equation gives ; matching the ambient pressure sets that constant to zero.
At ,
The surface traction is . Its moment gives the standard rotational resistance
At leading order the particle is a sphere. A pure applied couple produces no translation, while torque balance with the rotating sphere in Stokes flow gives
With directed from the particle into the fluid, the exact conditions on the true surface are
Evaluate no slip at and expand about . The order- terms give
The divergence of the Newtonian stress vanishes in the surrounding fluid, and its symmetry makes the divergence of angular-momentum flux vanish as well. The total force and torque may therefore be evaluated on any homologous enclosing surface, in particular the fixed reference sphere. Since the applied force is zero and the applied couple is fixed independently of ,
Using a fixed enclosing sphere is also why no separate terms involving the shape and leading stress appear.
Apply the Lorentz reciprocal theorem for Stokes flow to and the test flow around a sphere rotating with arbitrary . On ,
The reciprocal integral containing vanishes by the first-order torque condition. Since , the first-order boundary velocity is
The translational term integrates to zero. Therefore, for every ,
Now
For , tracelessness of and the stated fourth-moment identity give
It follows that
A centered ellipsoid has inversion symmetry. An applied axial couple is unchanged under inversion, whereas a translational velocity is reversed, so uniqueness of Stokes flow forces
At leading order in the small axial slope, the outer flow is locally the two-dimensional radial incompressible flow
because and the kinematic boundary condition is . This field is harmonic as a vector field away from the axis, so the exterior pressure is spatially constant and may be set to zero. Its radial normal stress at the interface is
Neglecting the tangential corrections, axial curvature, and the small internal viscous normal stress, the Young–Laplace equation with cylindrical curvature gives
Thus
Interpret the stated ansatz as
Multiplying the pressure relation by gives . Equating its constant and sinusoidal parts yields
The volume per wavelength is proportional to the mean of , namely . Hence
Choosing
then gives exactly
For , the disturbance amplitude obeys
so its long-wave linear growth rate is
The minimum radius is , and
Since the trajectory follows the circle toward increasing , it reaches and hence . Thus the nonlinear disturbance narrows monotonically to pinch-off within this approximation.
When internal pressure gradients matter, axial lubrication flow in the low-viscosity interior has volume flux
Conservation of cross-sectional area, , and the normal-stress expression for give
Let . Balancing with gives , so . Balancing either pressure contribution after two axial derivatives with then gives . Define
At fixed , , and
Substitution leaves the parameter-free third-order equation
Thus the similarity exponents are ; boundary and matching conditions would select a particular profile .
Let measure distance normal to the plane. The normal momentum balance and capillary pressure condition give
The downslope lubrication equation is
Apply no slip and zero tangential stress . Integration gives the flux
The thin-film equation is therefore
Long-wave information near a uniform film propagates with the kinematic speed
When , disturbances travel from into the domain, so is an admissible upstream boundary condition. When , information travels toward from the pool, so the same condition cannot independently be imposed there.
For a stationary vertical plane, set , , and . One integration of the steady equation, using and vanishing derivatives far above the pool, gives
Define
Then
Put and linearize to obtain . The two characteristic roots with positive real part are . These are the modes that decay as , so
The oscillations grow as one moves from the uniform film toward the pool.
In a static meniscus, hydrostatic pressure variation balances capillary pressure , giving the capillary length
The small parameter satisfies
It is reasonable to match to a nearly static meniscus because the bulk pool has negligible thin-film viscous resistance, while its local capillary-hydrostatic shape approaches the vertical wall almost tangentially.
Since and , dimensional curvature is
Matching it to gives
The dimensionless equation is . At a crest, , so
The imposed far-field flux is negligible there; the dominant physical balance is between local gravity-driven drainage and the capillary-pressure gradient.
At a trough, , so
Local gravity-driven flux is negligible; the capillary-pressure gradient drives the fixed flux through the trough against viscous resistance. These alternating balances generate the strongly nonlinear capillary waves.
Write . In the final trough, use
The trough equation requires , so . Matching the limiting curvature to requires
Thus
and the final trough is
If as , its slope on the crest side is
Integrating and using gives
The conditions at imply and . Hence
Let the final crest have . The crest balance gives . Matching its terminal slope to the final-trough slope from part (e) gives
Therefore
At the end matching to the penultimate trough,
The trough scaling from part (e) says that a trough matched to curvature has thickness scale . With , the penultimate trough therefore has
up to numerical constants. The exponent is extremely small, so attaining a clean asymptotic separation would require unrealistically tiny . Finite geometry, nonzero outer effects, molecular forces, and eventual rupture can intervene before experiments display many members of the predicted wave hierarchy.

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