Reduced tillage and no-tillage cropping systems have periods of time l
asting several months or years between tillage operations. If erosion
is to be predicted for these systems, then there is a need to characte
rize the effects of such extended time since tillage on rill erodibili
ty. Most erosion studies have been conducted on freshly tilled or dist
urbed soils which may respond differently to erosive forces than undis
turbed soils. The objective of this study was to evaluate the effects
of extended time since tillage on critical shear stress and rill erodi
bility for a Heiden vertisol under corn production. Rainfall simulatio
n studies were conducted in March and August, before corn planting and
after corn harvest, over a period of two years with time since tillag
e ranging from 7 to 624 days. Tests were replicated four times across
a slope of 4 to 6%. The resulting data expands erosion information on
one site included in the 1987 national tour under the Water Erosion Pr
ediction Project (WEPP) studies. As time since tillage increased, the
flow width in rills increased, and the hydraulic radius and hydraulic
shear converged to more stable values. Three soil strength measurement
s, cumulative rainfall, or cumulative rainfall energy were not consist
ently correlated to rill erosion parameters and did not seem to be pot
entially useful for future predictions. Different approaches may be ne
eded to relate repetitive wetting and drying cycles to measured soil p
roperties and erodibility. Critical shear stress ranged from 0.3 to 2.
47 Pa which indicated that rill erosion started at lower flow velociti
es or shallower flow depths than characterized by the 1987 WEPP data.
Rill erodibility was found to be highly variable (0.73 - 16.31 x 10(3)
s/m) on freshly tilled treatments, but variability decreased signific
antly for 89 days or more time since tillage, stabilizing in the range
of 2 - 5 x 10(3) s/m. Erosion should be more accurately predictable o
n sites with extended time since tillage, for the soil in this study.