Spreading of wetting liquid over a surface by disjoining pressure gradient driven film flow and by capillary pressure gradient driven channel flow is well known. Bacri ( J. Phys. Lett. ( Paris) 46, L467–L473, 1985) reported “anomalously” rapid spreading of wetting liquid during imbibition into a prewet porous medium. We predict quantitatively this phenomenon, called “hyperdispersion,” from viscous flow along pore walls in thin films of thickness h governed by disjoining force and capillarity. Pore radius distribution, pore network topology, and disjoining pressure function Π( h) all determine the magnitude of capillary dispersion. At high capillary pressures, we find that capillary pressure P c , wetting phase relative permeability k rw , and capillary dispersion coefficient D c can obey power laws in saturation S, which is the sum of the thin-film and pendular-structure inventories: S = S film + S ps . If Π ∝ h − m so that S film ∝ P −1/ m c , if S ps ∝ P − b c , and if thin films control flow, two sets of power law behavior exist. In the case 1/ m < b, P c ∝ S − m , k rw ∝ S 3, and D c ∝ S 2− m . In the case 1/ m > b, P c ∝ S −1/ b , k rw ∝ S 3/ mb, and D c ∝ S(3− m− mb)/ mb. The exponents m and b dictate the behavior of D c as the saturation of the wetting phase approaches zero. More complex function Π( h) can lead to nonmonotonic D c ( S). Bacri measured D c values two or three orders of magnitude higher than we predict, implying a distribution of wetting liquid different from any we consider.
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