A localized amount of insoluble surfactant spreads over a planar film of depth scale . Neglect gravity, capillarity and diffusion. Then and Marangoni stress drives , giving . The thin-film equations with insoluble surfactant admit a similarity solution in which the film height and concentration depend on , conserving total surfactant and fluid volume relative to the undisturbed layer.
When the smoothing width exceeds the capillary length, gravity dominates capillarity. Balancing hydrostatic flux against the Marangoni stress flux gives . The condition is in physical units. The smoothing region catches up with the spreading pool at and , after which the sharp-front outer similarity solution ceases to apply.
After gravity smoothing of a Marangoni front reaches the whole spreading pool, the film approaches uniform depth while surface transport continues. A small height gradient creates a hydrostatic pressure return flow that almost cancels the net Marangoni stress flux. Setting in the thin-film equations with insoluble surfactant gives and fractional depth variation . The depressed region under the surfactant therefore becomes progressively shallower.
The height jump in linear similarity profiles for surfactant spreading is smoothed by surface tension. If through a region of width , the Marangoni stress flux is and the capillary flux is . Their balance gives . This estimate assumes gravity is negligible and the smoothing region remains narrow compared with the pool.
For symmetric finite-mass Marangoni spreading on a liquid film, the leading outer profiles are and inside , where . Outside, and . The similarity solution follows from , , and . The film reaches height immediately behind the front, leaving an outer height jump that gravity or surface tension must smooth. These are ideal leading outer profiles, not a description of the microscopic central dry region or the smoothed edge.

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