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-infinite aquifer is an analytic curve, to which a steady 2-D plane or axisymmetric Darcian flow converges

are shallow cones, spherical, spheroidal, and paraboloidal caps. An instantaneous seepage flow rate, Q

An explicit analytical solution is obtained to an old problem of a potential steady-state 2-D

of a model for 2-D seepage flow with a capillary fringe. The boundary of the obstacle appears to show a

of a model for 2-D seepage flow with a capillary fringe. The boundary of the obstacle appears to show a

-D seepage into horizontal drains and axisymmetric flow into cavities are examined and generalized

-capillarity driven flow in an unsaturated medium with parabolic inclusion. Flow kinematic characteristics are studied

-D seepage into horizontal drains and axisymmetric flow into cavities are examined and generalized

Limiting analytical solutions for complex saturated and unsaturated transport problems

. HYDRUS-2D computations for flows in saturated and unsaturated soils match well the analytical solutions

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