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a USDA-ARS, P.O. Box E, Fort Collins, CO 80522
b USDA-ARS, 119 Keim Hall, East Campus, Univ. Nebraska, Lincoln, NE 68583
c USDA-ARS, retired, 226 E. Circle Dr., Canon City, CO 81212
* Corresponding author (adhalvor{at}lamar.colostate.ed)
Received for publication January 26, 2001. Spring wheat (Triticum aestivum L.) is generally produced in the northern Great Plains using tillage and a cropfallow system. This study evaluated the influence of tillage system [conventional-till (CT), minimum-till (MT), and no-till (NT)] and N fertilizer rate (0, 22, and 45 kg N ha-1) on grain N, grain N removal from cropping system, and changes in residual postharvest soil NO3N during six rotation cycles of a dryland spring wheatfallow (SWF) cropping system. Grain N concentration increased with increasing N rate and was higher with CT (33.3 g kg-1) than with NT (32.3 g kg-1) at 45 kg ha-1 N rate. Grain N removal per crop was greater with CT (70 kg N ha-1) and MT (68 kg N ha-1) than with NT (66 kg N ha-1) and tended to increase with increasing N rate, but varied with rotation cycle. Total grain N removal in six rotation cycles was in the order: CT > MT > NT. Total grain N removal by six SW crops was increased by N fertilization, with only 21 and 17% of the applied N removed in the grain for the 22 and 45 kg ha-1 N rates, respectively. Postharvest soil NO3N levels in the 150-cm profile varied with N rate and rotation cycle, with residual NO3N increasing during consecutive dry crop cycles. In contrast, some leaching of NO3N below the SW root zone may have occurred during wetter crop cycles. Soil profile NO3N levels tended to be greater with CT and MT than with NT. Variation in precipitation during rotation cycles and N fertilization impacted grain N removal and residual soil NO3N levels more than tillage system within this SWF cropping system.
Abbreviations: CT, conventional-till F, fallow MT, minimum-till NT, no-till SW, spring wheat
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