Papers Published
Abstract:
Perturbation methods are applied to study an
initial-boundary value problem for Richards' equation
describing vertical infiltration of
water into a finite layer of soil. This problem for the
degenerate diffusion equation with convection and
Dirichlet/Robin boundary conditions exhibits several
different regimes of behavior. Boundary layer analysis and
short-time asymptotics are used to describe the structure
of similarity solutions, traveling waves, and other solution
states and the transitions connecting these different
intermediate asymptotic states.