Long-Term Agroecosystem Research in the Central Mississippi River Basin: Dissolved Nitrogen and Phosphorus Transport in a High-Runoff-Potential Watershed

Abstract

© American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America. Long-term monitoring data from agricultural watersheds are needed to determine if efforts to reduce nutrient transport from crop and pasture land have been effective. Goodwater Creek Experimental Watershed (GCEW), located in northeastern Missouri, is a high-runoff-potential watershed dominated by claypan soils. The objectives of this study were to: (i) summarize dissolved NH 4 -N, NO 3 -N, and PO 4 -P flow-weighted concentrations (FWC), daily loads, and yields (unit area loads) in GCEW from 1992 to 2010; (ii) assess time trends and relationships between precipitation, land use, and fertilizer inputs and nutrient transport; and (iii) provide context to the GCEW data by comparisons with other Corn Belt watersheds. Significant declines in annual and quarterly FWCs and yields occurred for all three nutrient species during the study, and the decreases were most evident for NO 3 -N. Substantial decreases in first- and fourthquarter NO 3 -N FWCs and daily loads and modest decreases in first-quarter PO 4 -P daily loads were observed. Declines in NO 3 -N and PO 4 -P transport were attributed to decreased winter wheat (Triticum aestivum L.) and increased corn (Zea mays L.) production that shifted fertilizer application from fall to spring as well as to improved management, such as increased use of incorporation. Regression models and correlation analyses indicated that precipitation, land use, and fertilizer inputs were critical factors controlling transport. Within the Mississippi River Basin, NO 3 -N yields in GCEW were much lower than in tile-drained areas, but PO 4 -P yields were among the highest in the basin. Overall, results demonstrated that reductions in fall-applied fertilizer and improved fertilizer management reduced N and P transport in GCEW.