EGU22-1643, updated on 02 Mar 2023
https://doi.org/10.5194/egusphere-egu22-1643
EGU General Assembly 2022
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

The fate of trace organic compounds and their transformation products along specific hyporheic flow paths

Christoph J. Reith1, Malte Posselt2, Stephanie Spahr1, Anke Putschew3, Finn Amann4, Reinhard Hinkelmann4, and Jörg Lewandowski1,5
Christoph J. Reith et al.
  • 1Leibniz Institute of Freshwater Ecology and Inland Fisheries, Department Ecohydrology and Biogeochemistry, Berlin, Germany
  • 2Stockholm University, Department of Environmental Science (ACES), Stockholm, Sweden
  • 3Technische Universität Berlin, Department of Environmental Sciences and Technology, Chair of Water Quality Engineering, Berlin, Germany
  • 4Technische Universität Berlin, Department of Civil Engineering, Chair of Water Resources Management and Modeling of Hydrosystems, Berlin, Germany
  • 5Humboldt University of Berlin, Department Geography, Berlin, Germany

Trace organic compounds (TrOCs) are frequently detected in surface waters such as rivers. Possible entry pathways into the environment include stormwater runoff, industrial effluents, and wastewater treatment plant (WWTP) effluents. Understanding the behavior of TrOCs and their transformation products (TPs) is important, as they represent a risk to ecosystem and human health. The hyporheic zone of a river shows high turnover rates for nutrients, dissolved organic carbon, metals, pathogens, and TrOCs. Turnover rates are dependent on both, hydrological and biogeochemical conditions. We conducted a high-frequency sampling campaign in the urban lowland River Erpe (Brandenburg, Germany) which receives treated wastewater from the WWTP Muenchehofe. The aim was to study the fate of TrOCs and respective TPs along specific hyporheic flow paths. The basic idea was to enable the sampling of water parcels along specific hyporheic flow paths by forcing the flow path with a pipe (diameter: 8 cm, length: 27 cm, maximum depth: 17 cm) onto a specific path similar to the natural one. Wood on top of the pipe should increase the hyporheic exchange flow through the pipe and mimic the effect of woody debris which is often used in river restorations. Samples from the hyporheic zone and the surface water were taken every 2 hours for 14 hours. The samples were analyzed for oxygen concentrations, redox parameters, nutrients, and TrOCs. We found a clear redox zonation along the flow paths inside the pipes and investigated its impacts on the fate of TrOCs and their TPs. The hyporheic zone proved as an important river compartment for the retention of TrOCs and their TPs.

How to cite: Reith, C. J., Posselt, M., Spahr, S., Putschew, A., Amann, F., Hinkelmann, R., and Lewandowski, J.: The fate of trace organic compounds and their transformation products along specific hyporheic flow paths, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-1643, https://doi.org/10.5194/egusphere-egu22-1643, 2022.