A planar freezing front can push a spherical particle steadily when repulsive sphere-plane dispersion force balances lubrication resistance. The thin parabolic gap gives hydraulic drag , and balancing it against gives the displayed speed. This balance assumes a nonretarded interaction, small gap and negligible inertial and other particle forces.
For a sphere partially below a planar melting isotherm, write and depth . Local premelting gives film thickness . Conservation in the thin spherical film gives flux and pressure . Integrating vertical repulsive and hydraulic stresses over the wetted cap yields the displayed speed. The unknown thermodynamic constant cancels, but a narrow rim where the film ceases to be thin is excluded from the leading approximation.

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