An estimate of the sorptivity that requires only the knowledge of simp
le integrals of the soil-water diffusivity weighted by a power of the
water content is present. The result is checked systematically for dif
fusivity functions with very different behaviour: power law, exponenti
al and the two Fujita diffusivities. In all cases the error is always
less than 1% regardless of whether or not the diffusivity increases ra
pidly with water content.