Flow path link characteristics of small-scale surface drainage network
s are examined using 426 links obtained from erosion plot data. Link l
engths and drainage areas varied considerably in the data set. The dis
tribution of link lengths was well represented by a log-normal probabi
lity density function. Regression equations were developed to predict
link drainage area as a function of link length. Flow path networks we
re predicted by combining link characteristics with the topology defin
ed by an infinite topologically random network. Bifurcation, length, a
nd area ratios of these networks are in good agreement with previously
reported observed values. The usefulness of this approach in modeling
soil erosion is illustrated by coupling the network algorithm with so
il detachment and transport relationships.