Real-time, continuous, in situ water quality sensors were deployed on a fourth-order Iowa (U.S.) stream draining an agricultural watershed to evaluate key in-stream processes affecting concentrations of nitrate during a 24-day late summer (Aug-Sep) period. Overall, nitrate-nitrogen (NO-N) concentrations declined 0.11 mg L km, or about 1.9% km and 35% in total across 18 km. We also calculated stream metabolic rates using in situ dissolved oxygen data and determined stream biotic N demand to be 108-117 mg m day. From this, we estimate that 11% of the NO-N concentration decline measured between two in-situ sensors separated by 2 km was a result of biotic NO-N demand, while groundwater NO-N data and estimates of groundwater flow contributions indicate that dilution was responsible for 53%. Because the concentration decline extends linearly across the entire 18 km of stream length, these processes seem consistent throughout the basin downstream of the most upstream sensor site. The nitrate-dissolved oxygen relationship between the two sites separated by 2 km, calculations of biotic NO-N demand, and diurnal variations in NO-N concentration all indicate that denitrification by anaerobes is removing less NO-N than that assimilated by aquatic organisms unable to fix nitrogen for their life processes, and thus the large majority of the NO-N entering this stream is not retained or removed, but rather transported downstream.
Download full-text PDF |
Source |
---|---|
http://dx.doi.org/10.1007/s10661-018-6599-1 | DOI Listing |
Enter search terms and have AI summaries delivered each week - change queries or unsubscribe any time!