Impact of Long-Term Tillage Systems for Continuous Corn on Nitrate Leaching to Tile Drainage

Information is lacking on the long-term of tillage systems on NO 3 losses to surface and groundwater. An 11-yr (1982-1992) study was conducted to assess NO 3 losses to subsurface, tile drainage for corn (Zea mays L.) grown with continuous conventional tillage (CT) and no tillage (NT) on a poorly drained Webster clay loam soil (fine-loamy, mixed, mesic Typic Haplaquoll) at Waseca, MN. Nitrogen was applied at an annual application rate of 200 kg ha -1 . Mean annual subsurface drain flow during the 11-yr period was 35 mm higher for NT (315 mm) compared with CT (280 mm). Flow-weighted nitrate-nitrogen (NO 3 -N) concentrations increased dramaticaly in the wet years (NO 3 -N) concentrations increased dramatically in the wet years (1990 and 1991) following the dry period of 1987 to 1989. Flow-weighted NO 3 -N concentrations during the 11-yr period averaged 13.4 and 12.3 mg L -1 for CT and NT, respectively. Although subsurface drain flow was 12% higher with NT, NO 3 -N losses were about 5% higher with CT mainly due to higher NO 3 -N concentrations with CT in the last 2 yr. Corn grain yields and N removal were significantly higher in 6 out of 11 yr with CT compared with NT with no difference between tillage systems in the other 5 yr. Grain yields averaged 8.63 Mg ha -1 wich CT and 7.3 Mg ha -1 with NT during the 11-yr period. Multiple regression equations showed that annual flow-weighted NO 3 -N concentration is best predicted from residual soil NO 3 in the 0- to 1.2-m profile and spring rainfall while NO 3 -N flux can be predicted well from May and June rainfall. Results from this long-term study indicate that on this poorly drained soil, CT has a positive effect on corn grain yield and N removal compared with NT, but tillage systems had minimal impact of NO 3 losses to subsurface drain flow. Higher drain flow with NT does not necessarily result in higher NO 3 -N fluxes lost via subsurface drainage