Urea-N is linked to harmful algal blooms in lakes and estuaries, and urea-N-based fertilizers have been implicated as a source. However, the export of urea-N-based fertilizers appears unlikely, as high concentrations of urea-N are most commonly found in surface waters outside periods of fertilization. To evaluate possible autochthonous production of urea-N, we monitored urea-N released from drainage ditch sediments using mesocosms. Sediments from a cleaned (recently dredged) drainage ditch, uncleaned ditch, forested ditch, riparian wetland, and an autoclaved sand control were isolated in mesocosms and flooded for 72 h to quantify urea-N, NH 4 + -N, and NO 3 --N in the floodwater. Sediments were flooded with different N-amended-N) and incubated at three water temperatures (16, 21, and 27°C). Urea-N concentrations in mesocosms representing uncleaned and cleaned drainage ditches were significantly greater than nonagricultural sediments and controls. While flooding sediments with N-enriched solution had no clear effect on urea-N, warmer (27°C) temperatures resulted in significantly higher urea-N. Data collected from field ditches that were flooded by a summer rainstorm showed increases in urea-N that mirrored the mesocosm experiment. We postulate that concentrations of urea-N in ditches that greatly exceed environmental thresholds are mediated by biological production in sediments and release to stagnant surface water. Storm-driven urea-N export from ditches could elevate the risk of harmful algal blooms downstream in receiving waters despite the dilution effect. (Glibert et al., 2004). This phenomenon has drawn attention to sources of urea-N to surface water, and elevated urea-N concentrations issuing from agricultural watersheds have led some researchers to suggest a link to the land application of manures and urea-N synthetic fertilizers (Glibert et al., 2001(Glibert et al., , 2005(Glibert et al., , 2006Lomas et al., 2002;Thorén et al., 2003). Indeed, global urea-N fertilizer consumption ballooned 100-fold from the 1960s to the 2000s (Glibert et al., 2006), part of a trend of dramatically increasing fertilizer N use since the mid-twentieth century. Due in part to restrictions on inorganic fertilizers because of security concerns, urea-N comprises perhaps 60% of global N fertilizer use on an annual basis, and this proportion is expected to grow (Glibert et al., 2014). However, although small losses of agriculturally applied urea-N could be biologically important in receiving waters (Glibert et al., 2006), the export of untransformed urea-N fertilizer is likely minor. The rapid hydrolysis of urea-N in soils generally precludes substantial export from fertilizer applications (Fisher et al., 2016). Losses via leaching and overland flow are brief and typically small even under heavy rainfall conditions (Han et al., 2015;Kibet et al., 2016). In a synoptic watershed study on the Delmarva Peninsula, Tzilkowski (2013) found no evidence that storms in the weeks after poultry manure application led to increased ur...