Controls of nitrogen cycling under gaining and losing conditions in a first order agricultural stream

Abstract

Low order streams drain a big proportion of river catchments. They are not only fed by groundwater, but may also lose water to their connected aquifers and, in turn, can contribute to a substantial fraction of groundwater recharge. In such cases, these streams are typically characterized by the coexistence of gaining and losing stream reaches. Along the bidirectional exchange flow paths large biogeochemical gradients can evolve so that the exchange zones can function as hotspots for biogeochemical processes (such as the important (de)nitrification processes in croplands), which can substantially change under these two conditions. An agricultural first order stream (Schönbrunnen) in south-western Germany was equipped with stream gauging stations and piezometers were installed in the adjacent shallow aquifer, in order to find out how these biogeochemical processes change under losing versus gaining conditions. Hydrological and hydrochemical variables within the immediate vicinity of the stream, as well as stable nitrogen isotopes have been monitored between August 2017 and May 2020 to spatially and temporally identify the controls of nitrogen cycling dynamics in the Schönbrunnen.