Time Series of Electrical Conductivity Fluctuations Give Insights Into Long‐Term Solute Transport Dynamics of an Urban Stream

Author:

Jaeger Anna12ORCID,Schaper Jonas L.13ORCID,Romeijn Paul4,Betterle Andrea56ORCID,Posselt Malte7ORCID,Krause Stefan48ORCID,Lewandowski Jörg12ORCID,Riml Joakim9ORCID

Affiliation:

1. Department Ecohydrology and Biogeochemistry Leibniz Institute of Freshwater Ecology and Inland Fisheries Berlin Germany

2. Geography Department Humboldt University Berlin Berlin Germany

3. Center for Applied Geoscience Eberhard Karls University of Tübingen Tübingen Germany

4. School of Geography, Earth and Environmental Sciences University of Birmingham Birmingham UK

5. European Commission Joint Research Centre Ispra Italy

6. Eawag Swiss Federal Institute of Aquatic Science and Technology Dübendorf Switzerland

7. Department of Environmental Science Stockholm University Stockholm Sweden

8. CNRS ENTPE UMR5023 Ecologie des Hydrosystèmes Naturels et Anthropisés (LEHNA) University Lyon Université Claude Bernard Lyon 1 Villeurbanne France

9. Department of Sustainable Development, Environmental Science and Engineering Royal Institute of Technology Stockholm Sweden

Abstract

AbstractArtificial tracers are often used for quantitative estimates of solute transport properties in rivers. However, single‐injection tracer tests give insights in transport characteristics limited to the ecohydrological conditions at the testing time. Series of time‐consuming and laborious tracer tests would be required to properly capture seasonal changes. The present study uses intrinsic diurnal fluctuations of electrical conductivity (EC) caused by discharge of treated wastewater as a tracer to evaluate solute transport processes along a 4.7‐km reach of the River Erpe, Germany. By reproducing the fluctuations recorded along the river using the solute transport model one‐dimensional transport with inflow and storage, this study investigated the long‐term dynamics in solute transport properties. Individual 48‐hr curves of EC were used in the steady state configuration of the model to gain 48‐hr‐integrated estimates of selected transport parameters. Using a sliding window approach in 1‐hr steps along the 2,270‐hr time series of EC the temporal variability of solute transport between April and June 2016 was assessed. To test the identifiability of parameters using the proposed method, sensitivity analyses and a breakthrough curve analysis of selected 48‐hr windows were implemented. With time advancing into the summer, a significant rising trend (Mann‐Kendall test p‐value < 0.05) of the cross sectional area of the channel was observed and attributed to the growth of macrophytes and a significant slightly decreasing trend for the storage rate was found. The presented method is of high value for river management, as promoting transient storage enhances biogeochemical cycling and benefits water quality.

Funder

Horizon 2020 Framework Programme

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

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