The dispersion of a passive tracer in fluid flowing between a source a
nd a sink in a Hele-Shaw geometry, characteristic of field scale flows
in a layer or fracture, is considered. A combination of analytic and
numerical techniques and complementary experimental measurements are e
mployed, leading to a consistent picture. This dispersion process is f
ound to be characterized by a power-law decay in time of the tracer co
ncentration, with an exponential cutoff at very long times, in strong
contrast to the Gaussian behavior associated with the widely used quas
i-one-dimensional (1-D) models.