Tillage systems need to be compared over an extended period of time to
determine their transitional and long-term impacts on crop growth and
soil properties. A 15-yr experiment established in 1976 compared redu
ced tillage systems with conventional fall moldboard plowing for produ
ction of continuous corn (Zea mays L.) on a Maryhill silt loam soil (T
ypic Hapludalf). Corn plant growth and yield and soil properties were
compared for rive tillage systems: fall plow (fall mold-board plow + s
pring secondary tillage), fall chisel plow (fall chisel plow + spring
secondary), spring plow, spring plow/secondary (spring plow + secondar
y), and no-till. No-till consistently resulted in slower plant growth
than most or all of the other tillage systems. The fall plow and sprin
g plow/secondary treatments resulted in grain yields averaging 5% more
than fall chisel plow, 9% more than spring plow, and 16% more than no
-till yields. From 1976 to 1983, no-till yields tended to increase rel
ative to fall plow; from 1988 to 1990, however, no-till yields were mu
ch less than fall plow. No-till resulted in the lowest proportion of a
ggregates <5 mm in diameter, highest bulk density, and greatest penetr
ometer resistance. Penetrometer resistance of the spring plow plots in
creased at a slower rate with depth than the fall chisel plow system.
Among soil properties measured, the proportion of aggregates <5 mm in
diameter was most often significantly correlated with yield.