Capillary length Created 2026-09-24 Updated 2026-10-14
The capillary length measures when gravity and surface tension are comparably important in shaping a liquid interface. For a liquid of uniform mass density , beneath a gas whose mass density is negligible, with uniform gravitational acceleration and constant surface tension ,
A deformation of height and horizontal length scale has hydrostatic pressure variation of order and small-slope capillary pressure of order . Equating these gives : surface tension smooths small features, whereas gravity matters for broad ones. For two resting fluids, replace by their positive mass density difference in this static balance. This change alone does not give the two-fluid wave dynamics, because both fluids can have inertia. [ref]
With the stipulated illustrative parameters , , and , the capillary length is . These parameters define the ideal calculations below; they are not a measurement of a particular sample.
Figure 1.
The gravity-capillary wave crossover occurs at wavelength , where phase speed is smallest
. Calculated phase velocity and group velocity magnitudes, and the ratio of the surface tension and gravity terms in the deep-water dispersion relation, for the stipulated , and . The capillary length is , while the equality wavelength is . Both panels show ideal theory, without experimental data. Details.
For a sinusoid with wavenumber , the relevant horizontal scale is , while its wavelength is . Thus the Bond number for this scale and the reciprocal restoring-term ratio are
Equality is at , hence for these parameters. Using instead produces a different numerical Bond number; state the length convention. The capillary length itself is not the equality wavelength. This distinction helps choose whether a measured ripple should be modeled as a surface gravity wave, a nearly pure capillary wave, or a gravity-capillary wave. [ref]