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Isotope hydrology and water sources in a heavily urbanised stream
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  • Christian Marx,
  • Doerthe Tetzlaff,
  • Reinhard Hinkelmann,
  • Chris Soulsby
Christian Marx
Technische Universität Berlin

Corresponding Author:[email protected]

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Doerthe Tetzlaff
Leibniz-Institut für Gewässerökologie und Binnenfischerei im Forschungsverbund Berlin eV
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Reinhard Hinkelmann
Technische Universität Berlin
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Chris Soulsby
University of Aberdeen
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Complex networks of both natural and engineered flow paths control the hydrology of streams in major cities through spatio-temporal variations in connection and disconnection of water sources. We used spatially extensive and temporally intensive sampling of water stable isotopes to disentangle the hydrological sources of the heavily urbanized Panke catchment (≈ 220 km²) in the north of Berlin, Germany. The isotopic data enabled us to partition stream water sources across the catchment using a Bayesian mixing analysis. The upper part of the catchment streamflow here is dominated by groundwater from gravel aquifers underlying surrounding agricultural land. In dry summer periods, streamflow becomes intermittent; possibly as a result of local groundwater abstractions. Urban storm drainage is also an important part of runoff generation, dominating the responses to precipitation events. Although this dramatically changes the isotopic composition of the stream, it only accounts for 10-15% of annual streamflow. Moving downstream, subtle changes in sources and isotope signatures occur as catchment characteristic vary and the stream is affected by different tributary inflows. However, effluent from a wastewater treatment plant (WWTP) serving 700,000 people dominates the stream in the lower catchment where urbanisation effects are more dramatic. The associated increase in sealed surfaces downstream also reduces the relative contribution of groundwater to streamflow. The volume and isotopic composition of storm runoff is again dominated by urban drainage. As a result, only about 10% of annual runoff in the lower catchment comes from urban storm drains. The study shows the potential of stable water isotopes as inexpensive tracers in urban catchments that can provide a more integrated understanding of the complex hydrology of major cities. This offers an important evidence base for guiding the plans to develop and re-develop urban catchments to protect, restore and enhance the ecological and amenity value of these important resources.
26 Apr 2021Submitted to Hydrological Processes
26 Apr 2021Submission Checks Completed
26 Apr 2021Assigned to Editor
27 Apr 2021Reviewer(s) Assigned
07 Jun 2021Review(s) Completed, Editorial Evaluation Pending
07 Jun 2021Editorial Decision: Revise Major
10 Aug 20211st Revision Received
11 Aug 2021Assigned to Editor
11 Aug 2021Submission Checks Completed
11 Aug 2021Reviewer(s) Assigned
25 Aug 2021Review(s) Completed, Editorial Evaluation Pending
26 Aug 2021Editorial Decision: Revise Minor
06 Sep 20212nd Revision Received
06 Sep 2021Submission Checks Completed
06 Sep 2021Assigned to Editor
06 Sep 2021Reviewer(s) Assigned
06 Sep 2021Review(s) Completed, Editorial Evaluation Pending
06 Sep 2021Editorial Decision: Accept