A control volume model of solute transport through a single fracture i
n a porous matrix is developed. Application to problems of contaminant
transport through fractured clay demonstrates several strong features
of the method. The control volume approach inherently conserves mass
and treats dispersivity at interfaces in a physically correct manner.
By employing an upstream weighting scheme, based on the exact solution
to the one-dimensional steady state advection-dispersion equation, th
e model proves to be more efficient than previous single-fracture mode
ls. The significance of matrix diffusion in the direction parallel to
the fracture axis is investigated. For the transport of a nonreactive
tracer through a 20-micrometer-wide fracture in clay material, analyti
cal solutions based on one-dimensional matrix diffusion are erroneous
for flow velocities of less than 1 m/day. The influence of boundary co
nditions on two-dimensional matrix diffusion is considered, and the cl
ean-up of a contaminated fracture is simulated.