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Field-scale nitrogen balances associated with long-term continuous corn production

Excessive residual soil NO3-N indicates economic inefficiency for producers and increases the potential for nonpoint leaching of N to water resources. Our objective was to construct an approximate field-scale N budget for continuous corn (Zea mays L.) grown on deep loess soils in four 30- to 60-ha f...

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Bibliographic Details
Published in:Agronomy journal 1998-09, Vol.90 (5), p.644-650
Main Authors: Karlen, D.L. (USDA, ARS, Natl. Soil Tilth Lab., Ames, IA.), Kramer, L.A, Logsdon, S.D
Format: Article
Language:English
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Summary:Excessive residual soil NO3-N indicates economic inefficiency for producers and increases the potential for nonpoint leaching of N to water resources. Our objective was to construct an approximate field-scale N budget for continuous corn (Zea mays L.) grown on deep loess soils in four 30- to 60-ha field-scale watersheds in western Iowa. Preplant and postemergence soil NO3-N levels were determined for the 0- to 30-cm, 30- to 60-cm and 60- to 90-cm depths in April before N fertilizer was applied and again at the V6 growth stage. A simple root-zone water balance and N removal by corn grain were determined. The 4-yr average showed approximately 100 kg ha(-1) of NO3-N in the upper 90 cm of the root zone before an average of 168 kg of fertilizer N ha(-1) was applied. Grain removal accounted for 30 to 70% of the fertilizer N. There were significant differences in grain yield and N removal among the four watersheds. Factors contributing to those differences included different fertilizer rates, tillage and application times. During the four study years, an average of 50% of the applied N was available for leaching, denitrification, and/or NH3 volatilization. High levels of residual soil NO3-N following continuous corn production coupled with steady percolation of precipitation that infiltrated but was not used by the corn crop appear to be the two major factors supplying NO3-N to groundwater baseflow that enters streams during the watersheds. Based on the seasonal water balance, the most successful N management strategies will be those that minimize the amount of residual NO3-N remaining in the soil profile at the end of the growing season
ISSN:0002-1962
1435-0645
DOI:10.2134/agronj1998.00021962009000050013x