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Felix Ortmeyer, Kristina Volkova, Frank Wisotzky, Stefan Wohnlich, Andre Banning

• The mainly agricultural input of \(NO_{3}\)\(^{-}\) and compliance with drinking water guideline values pose major challenges for many water suppliers. Additionally, associated changes in hydrochemistry, especially concerning products of \(NO_{3}^{-}\) reduction (\(Fe^{2+/3+}\), \(Mn^{2+/4+}\), \(Ca^{2+}\), \(Mg^{2+}\), \(SO_4\)\(^{2-}\), \(HCO_3\)\(^-\)) and subsequent reactions, can have a major influence on mineral saturation states and well yield: well productivity can be strongly reduced by mineral precipitation and silting. To evaluate hydrogeochemical evolution and clogging potential for a given well field, thorough hydrochemical and geochemical investigations are required. Therefore, time-dependent and depth-specific ion concentrations in water samples (\(\it n\) = 818) were analysed in a catchment area of a waterworks in western Germany. The sediments of the aquifers were extensively investigated for their geochemistry (CS, scanning electron microscope, aqua regia digestion and dithionite solution; \(\it n\) = 253). In addition, PhreeqC was used to model saturation indices in order to identify possible mineral precipitation in the wells. Results show a high \(NO_{3}\)\(^{-}\) input into deep wells screened in Tertiary sediments due to an admixture of Quaternary groundwater. Directly at the Quaternary-Tertiary boundary, chemolithotrophic \(NO_{3}\)\(^{-}\) reduction consuming pyrite occurs. Protons released during the process are pH-buffered by dissolving carbonate minerals. Overall, the hydrochemistry and especially the saturation indices are strongly influenced by \(NO_{3}\)\(^{-}\) reduction and its degradation products. A change in well yield has not yet been observed, but future clogging by ochre formation or sintering cannot be excluded.