Linking Nitrogen Management, Seep Chemistry, and Stream Water Quality in Two Agricultural Headwater Watersheds

Riparian seepage zones in headwater agricultural watersheds represent important sources of nitrate‐nitrogen (NO 3 –N) to surface waters, often connecting N‐rich groundwater systems to streams. In this study, we examined how NO 3 –N concentrations in seep and stream water were affected by NO 3 –N processing along seep surface flow paths and by upslope applications of N from fertilizers and manures. The research was conducted in two headwater agricultural watersheds, FD36 (40 ha) and RS (45 ha), which are fed, in part, by a shallow fractured aquifer system possessing high (3–16 mg L −1 ) NO 3 –N concentrations. Data from in‐seep monitoring showed that NO 3 –N concentrations generally decreased downseep (top to bottom), indicating that most seeps retained or removed a fraction of delivered NO 3 –N (16% in FD36 and 1% in RS). Annual mean N applications in upslope fields (as determined by yearly farmer surveys) were highly correlated with seep NO 3 –N concentrations in both watersheds (slope: 0.06; R 2 = 0.79; p < 0.001). Strong positive relationships also existed between seep and stream NO 3 –N concentrations in FD36 (slope: 1.01; R 2 = 0.79; p < 0.001) and in RS (slope: 0.64; R 2 = 0.80; p < 0.001), further indicating that N applications control NO 3 –N concentrations at the watershed scale. Our findings clearly point to NO 3 –N leaching from upslope agricultural fields as the primary driver of NO 3 –N losses from seeps to streams in these watersheds and therefore suggest that appropriate management strategies (cover crops, limiting fall/winter nutrient applications, decision support tools) be targeted in these zones.