Alternative Farming System Effects on Profile Nitrogen Concentrations on Two Iowa Farms

There is a general lack of quantitative data to assess alternate farming systems. Our objectives were to quantify long‐term (20‐yr) effects of conventional and alternative farming practices on soil NH 4 ‐N, NO 3 ‐N, and total‐N concentrations. Contiguous soil map units of Clarion loam (fine‐loamy, mixed, mesic Typic Hapludoll), Nicollet loam (fine‐loamy, mixed, mesic Aquic Hapludoll), Canisteo silty clay loam (fine‐loamy, mixed [calcareous], mesic Typic Haplaquoll), and Webster silty clay loam (fine‐loamy, mixed, mesic Typic Haplaquoll) were identified and used to compare long‐term farming system effects. Sixty‐four soil profile cores averaging 4.5 m in depth were collected from a 16‐ha conventional field and from a 16‐ha alternative field in April 1989 following a year in which total precipitation was ≈30% below normal (588 vs. 848 mm). In autumn 1990, 32 cores averaging 3.0 m in depth were collected from each of two other 16‐ha conventional and alternative fields just north of those sampled in 1989. Farming practice significantly affected total‐N, NH 4 ‐N, and NO 3 ‐N concentrations measured at the various sampling depths, but differences were small and inconsistent. Corn ( Zea mays L.) grain yields averaged 9093 kg ha −1 in the conventional field and 8977 kg ha −1 in the alternative field in 1989. Comparing conventional and alternative fields, total aerial N accumulation 6 wk after planting averaged 203 and 123 mg plant −1 , ear leaf N concentration averaged 26.6 and 20.6 g kg −1 , and total N removed by corn grain averaged 91.6 and 85.7 kg ha −1 . All measured differences were generally within the 95% confidence interval, and neither system was consistently better. We conclude that well‐managed conventional and alternative farming systems do not differ in their risk for groundwater N pollution in central Iowa.