The advent of precision farming practices has heightened interest in managi
ng field variability to optimize profitability. The large variation in yiel
ds across many producer fields demonstrated by yield-monitor-equipped combi
nes has generated concern about management-induced causes of spatial variat
ion in soil productivity. Soil translocation from erosion processes may res
ult in variation in soil properties across field landscape positions that p
roduce long-term changes in soil productivity. The objective of this study
was to examine the relationships between soil redistribution caused by till
age and water erosion and the resulting spatial variability of soil product
ivity in a soil catena in eastern South Dakota. An empirical model develope
d to estimate tillage erosion was used to evaluate changes expected in the
soil profile over a 50-year period on a typical toposequence found in easte
rn South Dakota and western Minnesota. Changes in the soil profile due to w
ater erosion over a 50-year period were evaluated using the WEPP hillslope
model. The tillage erosion model and the WEPP hillslope model were run conc
urrently for a 50-year period to evaluate the combined effect of the two pr
ocesses. The resulting changes in soil properties of the root zone were eva
luated for changes in productivity using a productivity index model. Tillag
e erosion resulted in soil loss in the shoulder position, while soil loss f
rom water erosion occurred primarily in the mid to lower backslope position
. The decline in soil productivity was greater when both processes were com
bined compared to either process acting alone. Water erosion contributed to
nearly all the decline in soil productivity in the backslope position when
both tillage and water erosion processes were combined. The net effect of
soil translocation from the combined effects of tillage and water erosion i
s an increase in spatial variability of crop yields and a likely decline in
overall soil productivity. (C) 1999 Elsevier Science B.V. All rights reser
ved.