Boussinesq equation for an unconfined aquifer
= Boussinesq equation for an unconfined aquifer
For pore fraction $n$, permeability $k$, liquid density $\rho$, viscosity $\mu$, rainfall recharge $R$, and a shallow groundwater thickness $h$,
$$
n h_t=\frac{k\rho g}{\mu}(hh_x)_x+R.
$$
This is a nonlinear diffusion equation with diffusivity proportional to the local thickness.