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Towards an improved understanding of transport processes governing the spatiotemporal dynamics of particles and fecal bacteria in karst aquifers – IMPART

Subject Area Hydrogeology, Hydrology, Limnology, Urban Water Management, Water Chemistry, Integrated Water Resources Management
Term from 2020 to 2024
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 432288610
 
Final Report Year 2024

Final Report Abstract

Karst aquifers provide drinking water for 9.2% of the global population. The generally good water quality is often interrupted by rapid and strong contamination events. To understand the detailed transport processes and spatiotemporal changes in water quality the IMPART project was conducted at Germany’s second largest karst spring (Blautopf). Deeper insight into the structure of the karst system was gained by two large scale tracer tests, with a total of 7 tracer injections at the surface and inside the active conduit network, and monitoring locations in the cave system and at the spring. The results demonstrated that the catchment can be subdivided into two sub-catchments of similar size and allowed to quantify the variability of transport velocities, which were up to three times higher at high-flow than at low-flow conditions. Sediment particles play a significant role as transport vectors for contaminants. A comparative tracer test using suspended cave sediments and solute tracers, along with detailed geochemical analyses, revealed that sediment particles were transported faster than solutes, which is explained by preferential transport along the main flow paths of the conduit. All particle sizes (< 10 µm) were transported similarly, and a sediment-associated transport could be demonstrated for all geochemical elements. The results represent an important step forward as they lead to a deeper understanding of the transport processes of sediment-bound pollutants. The comprehensive investigation of the water quality by means of a 30-month long-term monitoring, intensive sampling of a rainfall event and a spatial sampling within the cave system, demonstrated that the spring exhibits only moderate seasonal variations, but shows a strong response to intense precipitation events, e.g., fecal bacteria (E. coli) increased 100-fold (up to 17,168 MPN/100 ml) during a monitored event. A paired-catchment approach was successfully implemented for the first time to a subsurface karst- and cave system. Chemical and microbial water quality differed significantly between both sub-catchments and could be associated to different land use. Nitrate was linked to agriculture whereas potassium, chloride, gadolinium and fecal bacteria could be identified as indicators for waste water effluents. This study underlines the susceptibility of karst springs and demonstrates the applicability of spatial-temporal water quality monitoring as a powerful tool to identify impacts of land use activities. Additionally, the discharge behavior of Blautopf was analyzed for historic and future responses to climate change. Historic time series (1952–2021) of climate variables and discharge were statistically evaluated and used to calibrate a reservoir model, which was then used to simulate the expected impacts of climate change on spring discharge. Results show no significant changes for annual mean and low discharge in the historic data, but the annual peak discharge shifted to a lower state since 1988 due to decreasing precipitation, decreasing snowmelt and increasing air temperature. According to the projections of all climate-change scenarios, peak discharge may decrease by 50% and baseflow by 35–55% by 2100 due to increasing evapotranspiration and decreasing snow cover. Results show the prolonged impact of climate change and variability on the floods and droughts at the springs and may imply water scarcity risks at similar climatic and geologic settings.

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