A formal statistical discussion of the origins of the random walk and
its relation to the classic advection-dispersion equation is given. At
issue is the common use of Gaussian distributed steps in producing th
e desired dispersive effects. Shown are alternative solutions to the b
asic Langevin equation describing mass displacements based on non-Gaus
sian, white increments. In particular, the results reveal that uniform
or symmetric-triangular steps can be employed without loss of general
ity in accuracy of the solution (over all Peclet numbers) and may yiel
d significant savings in the computational generation of the random de
viates required in the Monte Carlo procedures of the random walk metho
d.