Nn. Ranells et Mg. Wagger, WINTER ANNUAL GRASS-LEGUME BICULTURES FOR EFFICIENT NITROGEN MANAGEMENT IN NO-TILL CORN, Agriculture, ecosystems & environment, 65(1), 1997, pp. 23-32
Winter annual cover crops may be an effective tool for managing inorga
nic N in the sandy soils of the Atlantic Coastal Plain when summer dro
ughts can result in relatively high residual fertilizer N levels. A fi
eld experiment was conducted from 1992 to 1994 on a Norfolk loamy sand
to determine the effect of (1) previous corn fertilizer N rate (150 o
r 300 kg ha(-1)) on dry matter (DM) and N accumulation in rye, crimson
clover, and hairy vetch monocultures and respective rye-legume bicult
ures; (2) the respective cover crops on residual soil inorganic N leve
ls; and (3) cover crops on corn grain yield. Compared to the preplant
corn N rate of 150 kg ha(-1), the 300 kg N ha(-1) rate resulted in gre
ater profile soil inorganic N contents on subsequent sampling dates in
both years. Concomitant with these greater residual soil N levels wer
e increases in cover crop DM and N accumulation compared with low resi
dual soil N levels. Averaged over 2 year, cover crop DM accumulation b
y April was in the order of rye > rye-vetch = rye-crimson clover > hai
ry vetch > crimson clover. The corresponding cover crop N content rank
ing was hairy vetch > rye-hairy vetch > crimson clover = rye-crimson c
lover > rye. Before corn planting in Apr, rye monoculture reduced soil
inorganic N content an average of 62% in 1993 and 37% in 1994 compare
d to legume monocultures. Soil inorganic N content under the rye-legum
e bicultures was reduced an average of 44% and 15% for the same dates.
Inadequate rainfall during both corn growing seasons resulted in poor
corn yields (1.18 to 2.50 Mg ha(-1)) that were generally unaffected b
y cover crop or prior N rate. The results from this study demonstrated
the ability of rye and rye-legume bicultures to scavenge residual soi
l inorganic N following a summer corn crop, thereby minimizing the lea
ching of N from the plant resting zone. (C) 1997 Elsevier Science B.V.