“…In some cases, NO 3 − ‐rich water from adjacent agricultural fields may flow to the stream by paths that are too deep to allow interaction with riparian vegetation, a situation termed ‘riparian bypass’ (Jacks and Norrstrom, 2004; Wilcox et al , 2006; McCarty et al , 2008; Mills et al , 2008). Where NO 3 − bypasses biologically active riparian areas or where buffers do not exist, it may remain at high concentration as it moves through streambed sediments resulting in appreciable nutrient export to streams (Böhlke and Denver, 1995; Denver et al , 2003; Angier et al , 2005). In other cases, however, the streambed substantially reduces NO 3 − concentrations as the NO 3 − ‐rich water discharges to the stream (Lee and Hynes, 1978; Jacobs and Gilliam, 1985; Mills et al , 2008).…”