- 1Helmholtz Centre for Environmental Research - UFZ, Department of Aquatic Ecosystem Analysis and Management, Magdeburg, Germany (michael.rode@ufz.de)
- 2The National Key Laboratory of Water Disaster Prevention, Yangtze Institute for Conservation and Development Hohai University Xikang Road No. 1, Nanjing 210098, China
- 3College of Environmental Engineering, Nanjing Institute of Technology, Nanjing, 211167, China
High-frequency nitrate-N () data are increasingly available, while accurate assessments of the importance of in-stream retention processes is deviating stream orders are still unclear. In this presentation we hypothesize that similar diurnal nitrate uptake pattern exists in different stream orders and that these patterns can reveal insights into the dominance of uptake processes across stream scales. To test this assumption continuous 15-min estimates of retention was derived in a 1st stream and a 6th-order reach of the lower Bode River network (27.4 km, central Germany) using a one station method for the 1st order agricultural headwater stream and a two-station approach for the 6th order stream applying a data fusion framework capturing river hydraulics and their impacts on solute signal propagation through river hydrodynamic modelling (Yang et al. 2023). This methodological setting was used for long-term sensor monitoring data from 2015-2023 capturing highly deviating hydrological (normal and drought) and stream morphological conditions. The unique retention estimates revealed very similar characteristic diurnal variation of retention pattern. Three very similar clusters of diel uptake patterns were identified in both streams, potentially representing changes in dominant autotrophic and heterotrophic retention processes. While the dominating N-uptake clusters were similar in both systems, their seasonal occurrence showed significant differences between the two streams. For example, clusters reflecting assimilatory N-uptake dominated in the 1st order stream in all years and seasons. In the 6th order reach autotrophy-characterized clusters mostly occurred during early seasons, which are then followed by a shift to heterotrophic-dominated uptake pattern during summer- autumn low-flow periods. In addition, dominance of autotrophic retention extended more widely across seasons during the drought years. In contrast, the 1st order stream showed relevance of both autotrophic and heterotrophic uptake even in the winter month due to the stimulation by elevated spring water temperature. The analysis of characteristic uptake clusters and the suggested framework can be flexibly transferred across sites and scales, thereby complementing high-frequency monitoring to identify in-stream uptake processes and to inform river management.
Reference
Yang, X., Zhang, X., Graeber, D., Hensley, R., Jarvie, H., Lorke, A., Borchardt, D., Lif, Q., Rode, M. (2023) Large-stream nitrate retention patterns shift during droughts: Seasonal to sub-daily insights from high-frequency data-model fusion. Water Research, 243, 120347.
How to cite: Rode, M., Yang, X., Zhang, X., and Shawon, S.: Similar pattern of diurnal nitrate retention in different stream orders: seasonal to sub-daily insights from high-frequency data, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-8876, https://doi.org/10.5194/egusphere-egu25-8876, 2025.