Many models for soil water retention have been proposed. However, most
of these models are curve-fitting equations and do not emphasize the
physical significance of their empirical parameters. A new retention m
odel that exhibits increased flexibility was developed by applying thr
ee-parameter lognormal distribution laws to the pore radius distributi
on function f(r) and to the water capacity function, which was taken t
o be the pore capillary pressure distribution function f(psi). This mo
del contains three parameters that are closely related to the statisti
cs of f(psi): the bubbling pressure psi(c), the mode psi0 of f(psi), a
nd the standard deviation sigma of transformed f(psi). By comparison o
f this model with three existing models (the van Genuchten model, the
Brooks-Corey model, and the modified Tani model), it was shown that ps
i(c), psi0, and sigma are all essential for a general retention model.