EGU26-19520, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-19520
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Wednesday, 06 May, 14:00–15:45 (CEST), Display time Wednesday, 06 May, 14:00–18:00
 
Hall A, A.126
Groundwater – surface water interactions revisited
Jan Fleckenstein
Jan Fleckenstein
  • Helmholtz Center for Environmental Research GmbH, UFZ, Department of Hydrogeology, Leipzig, Germany (jan.fleckenstein@ufz.de)

Interactions between groundwater (GW) and surface water (SW) have been a focus of hydrologic research for some time. Seminal early work by J. Toth (1963) and later T. Winter (1999) had shown the existence of nested GW flow systems and stressed that surface water bodies are integral parts of these flow systems. Despite this early, integral perspective, a simpler perception of GW and SW as two distinct compartments, which interact via some often loosely defined transfer mechanisms, still prevails. This perception can be found in many hydrologic models, but can be misleading, as it implies the existence to two clearly separable compartments, while in fact GW and SW are part of a hydrologic continuum (as a part of the terrestrial hydrologic cycle), in which water dynamically transitions back and forth between surface water bodies (rivers, lakes, wetlands) and shallow aquifers. For example, shallow riparian groundwater may become stream water in one moment and return back to the alluvial aquifer in the next with implications for water and solute exchange and biogeochemical turnover. While simplified conceptualizations of the GW-SW hydrologic continuum may be acceptable for the simulation of catchment streamflow response, they usually fall short, when trying to represent fluxes and dynamics of nutrients and other solutes, which are typically controlled by hydrological and biogeochemical processes in the transition zone between GW and SW. I argue that in our quest to understand coupled hydrological and biogeochemical processes and GW dependent ecosystems at the catchment and landscape scales, we needed to revisit the perception of GW and SW as a hydrologic continuum. I will use the example of dissolved organic carbon (DOC) export from a headwater catchment to stress this point and illustrate how rich field data and an integral numerical model can help to refine and improve a simplified conceptual model for catchment-scale DOC export.

 

Toth, J. (1963) A Theoretical Analysis of Groundwater Flow in Small Drainage Basins, Journal of Geophysical Research, 68(16)

Winter, T. (1999) Relation of streams, lakes, and wetlands to groundwater flow systems, Hydrogeology Journal, 7:28-45

How to cite: Fleckenstein, J.: Groundwater – surface water interactions revisited, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-19520, https://doi.org/10.5194/egusphere-egu26-19520, 2026.