Conservation Reserve Program (CRP) areas that are returned to crop pro
duction will initially be much less erodible than fields which were fa
rmed using conventional practices. In this study, a rainfall simulator
was used to measure runoff and erosion from former CRP areas in Missi
ssippi, Nebraska and South Dakota over approximately a two year period
. Soil loss rates measured immediately following tillage on each of th
e three sites were similar to values obtained on the undisturbed CRP t
reatments. However when left in a fallow condition, the erosion-reduci
ng effectiveness of the sod appeared to have lasted less than one year
The rapid increase in soil erodibility following tillage was attribut
ed to a reduction in surface cover and organic material. The WEPP and
RUSLE models are currently used extensively in conservation planning a
nd assessment. The experimental data collected in this study were used
to derive selected parameter values for use in these models.