Corn (Zea mays L.) and soybean [Glycine mar (L.) Merr.], the backbone
of Midwestern crop production, respond to rotation, but how growing co
nditions affect this is not well documented. Our objectives were to de
termine the effect of various corn and soybean cropping patterns on yi
elds and to evaluate environmental effects on the rotation effect. The
study began in 1981 at Lamberton, MN, on a Webster clay loam (fine-lo
amy, mixed, mesic Typic Endoaquoll), in 1982 at Waseca, MN, on a Nicol
let clay loam (fine-loamy, mixed, mesic Aquic Hapludoll), and in 1983
at Arlington, WI, on a Piano silt loam (fine-silty, mixed, mesic Typic
Argiudoll). Cropping sequences were (i) continuous monoculture of eac
h crop; (ii) annual rotation of the two crops; and (iii) 1, 2, 3, 4 an
d 5 yr of each crop following 5 yr of the other crop. Results are base
d on 11 yr Of data at Lamberton, 8 yr (soybean) or 9 yr (corn) at Wase
ca, and 9 yr at Arlington. Corn rotated annually with soybean yielded
13% more, and 1st-yr corn following multiple years of soybean yielded
15% more than continuous corn. Soybean annually rotated with corn yiel
ded 10% more, and 1st-yr soybean following multiple years of corn yiel
ded 18% more than continuous soybean. The crops differed in response t
o increasing years of consecutive planting: 2nd-yr to 5th-yr corn yiel
ds were no different from continuous corn yields; 2nd-yr soybean yield
ed 8% more than continuous soybean, 3rd-yr soybean yielded 3% more, an
d 4th- and 5th-yr soybean yielded the same as continuous soybean. Rela
tive increase in yields of both crops in annual rotation compared with
monoculture was approximately twofold greater in low-yielding than in
high-yielding environments. In low-yielding environments, the yield a
dvantage of an annual rotation of corn and soybean compared with monoc
ulture was frequently greater than 25%. The commonly practiced annual
rotation of corn and soybean maximized corn yields, but not soybean yi
elds, relative to the other sequences studied.