Capillary currents and viscous droplet spreading
David Darrow, Lucas Warwaruk, John W. M. Bush
TL;DR
This study addresses the spreading of viscous, shallow droplets on rough substrates and demonstrates that large droplets spread via capillary currents driven by edge forces, while a Darcy precursor film propagates ahead due to substrate roughness. The authors combine experiments with a capillary-current theory that enforces a quasi-equilibrium balance between hydrostatic and curvature pressures and includes bulk and edge dissipation, recovering the classical small-droplet laws ($R_1\sim V^{3/10} t^{1/10}$) and ($R_1\sim V^{3/8} t^{1/8}$) for large drops, and predicting $R_2$ scaling with a logarithmic correction ($R_2\sim t^{3/8}/\sqrt{\log t}$). The work also explains the Darcy precursor film dynamics observed ahead of droplets on rough substrates and demonstrates dynamic similarity across fluids, while extending the framework to partial wetting and smooth substrates. Overall, the capillary-current perspective unifies droplet-spreading mechanisms across scales and substrate types, with implications for coating, microfluidics, and porous-media wetting.
Abstract
We present the results of a combined experimental and theoretical study of the spreading of viscous droplets over rigid substrates. First, we experimentally investigate the wetting of a roughened glass surface by a viscous droplet of silicone oil, wide and shallow relative to the capillary length $\ell_c$. The horizontal radius of the droplet grows according to an $R_\mathrm{drop}\sim t^{1/8}$ scaling reminiscent of viscous gravity currents (Lopez et al. 1976). The droplet is preceded by a mesoscopic fluid film that percolates through the rough substrate, its radius increasing according to $R_\mathrm{film}\sim t^{3/8}/(\log t)^{1/2}$. To rationalize these observed scalings, we develop a new 'capillary current' model for the spreading of shallow droplets with arbitrary radius on rough surfaces. Furthermore, on the basis of established similarities between droplet spreading over wetted rough and smooth substrates (Cazabat & Cohen Stuart 1986), we argue its relevance to a broader class of spreading problems. We propose that, throughout their evolution, shallow droplets maintain a quasi-equilibrium balance between hydrostatic and curvature pressure, perturbed only by unbalanced contact line forces arising along the droplet's edge. For drops with horizontal radii small with respect to $\ell_c$, our model converges to the original description of Hervet & de Gennes (1984) and thereby recovers the classic spreading laws of Hoffman (1975), Voinov (1976), and Tanner (1979). For drops wide with respect to $\ell_c$, it rationalizes why millimetric, surface-tension-driven capillary currents exhibit the same spreading behavior as relatively large-scale viscous gravity currents.
