Articles | Volume 16, issue 10
Hydrol. Earth Syst. Sci., 16, 3485–3498, 2012
https://doi.org/10.5194/hess-16-3485-2012

Special issue: Assessing the impact of climate change for adaptive water...

Hydrol. Earth Syst. Sci., 16, 3485–3498, 2012
https://doi.org/10.5194/hess-16-3485-2012

Research article 01 Oct 2012

Research article | 01 Oct 2012

Compiling geophysical and geological information into a 3-D model of the glacially-affected island of Föhr

T. Burschil1, W. Scheer2, R. Kirsch2, and H. Wiederhold1 T. Burschil et al.
  • 1Leibniz Institute for Applied Geophysics LIAG, Hannover, Germany
  • 2State Agency for Agriculture, Environment and Rural Areas of the Federal State Schleswig-Holstein LLUR, Geological Survey, Flintbek, Germany

Abstract. Within the scope of climatic change and associated sea level rise, coastal aquifers are endangered and are becoming more a focus of research to ensure the future water supply in coastal areas. For groundwater modelling a good understanding of the geological/hydrogeological situation and the aquifer behavior is necessary. In preparation of groundwater modelling and assessment of climate change impacts on coastal water resources, we setup a geological/hydrogeological model for the North Sea Island of Föhr.

Data from different geophysical methods applied from the air, the surface and in boreholes contribute to the 3-D model, e.g. airborne electromagnetics (SkyTEM) for spatial mapping the resistivity of the entire island, seismic reflections for detailed cross-sections in the groundwater catchment area, and geophysical borehole logging for calibration of these measurements. An iterative and integrated evaluation of the results from the different geophysical methods contributes to reliable data as input for the 3-D model covering the whole island and not just the well fields.

The complex subsurface structure of the island is revealed. The local waterworks use a freshwater body embedded in saline groundwater. Several glaciations reordered the youngest Tertiary and Quaternary sediments by glaciotectonic thrust faulting, as well as incision and refill of glacial valleys. Both subsurface structures have a strong impact on the distribution of freshwater-bearing aquifers. A digital geological 3-D model reproduces the hydrogeological structure of the island as a base for a groundwater model. In the course of the data interpretation, we deliver a basis for rock identification.

We demonstrate that geophysical investigation provide petrophysical parameters and improve the understanding of the subsurface and the groundwater system. The main benefit of our work is that the successful combination of electromagnetic, seismic and borehole data reveals the complex geology of a glacially-affected island. A sound understanding of the subsurface structure and the compilation of a 3-D model is imperative and the basis for a groundwater flow model to predict climate change effects on future water resources.