A method is presented for predicting the advective-dispersive transpor
t of a contaminant towards a well in a confined aquifer. Due to (macro
-)dispersion, particles carry out random walks through the porous form
ation, Using perturbation techniques analytical approximations are der
ived for the fraction of the particles that reach the well and for the
mean and variance of the arrival time. In particular, approximations
for the breakthrough curve at the well are provided. The asymptotic ap
proximations are shown to be in good agreement with results of random-
walk simulations. The method may be applied to any 2D-flow pattern.