We would like to present a study on the Thuringian Basin, a large area in central Germany. Within this basin exist areas with very different interesting geo- and hydrological properties. We set up models and simulations for four subdomains within the basin, which describe different depositional environments - Eolian, Fluvial, Sandflat and Lacustrine. Researchers would like to investigate which paths is the water taking in the subsurface and how fast it is moving. The aim of this study is to gain knowledge about flow paths within these four model areas with regard to their architectural design. First simulation results suggest dependencies of flow paths and flow velocities due to different architectural elements (from the sequence of the subsurface layers) and characteristics such as the varying permeabilities.
Fischer, Thomas; Kunkel, Cindy; Naumov, Dmitri; Gaupp, Reinhard; and Kolditz, Olaf, "Examining Flow Paths In Bunter Sediments In Thuringian Basin" (2014). CUNY Academic Works.
Session R17, Groundwater Flow Modeling I