The Pantano Formation arenitic aquifer, in the Northern Apennine chain between Modena and Bologna (Italy). through an array of geological, hydrogeological and geochemical investigations across distinct members of the Miocene Pantano Formation, this study aims at assessing the influence of depositional environments on aquifer performance (i.e., recharge and storage capacity, spring discharge). As the investigated aquifer represents a key resource for drinking water in the Northern Apennines, interpreting depositional environments might drive future applications in areas understudied from a hydrogeological viewpoint. this study emphasizes the critical role of depositional environments in shaping the aquifer characteristics of the Pantano Formation. Sedimentary facies formed in relatively proximal environments, close to the paleo shoreline, exhibit higher bulk hydraulic conductivity, recharge potential, and storage than those formed in a more distal (open shelf) position, resulting in discharge through larger springs more resilient to droughts. These differences are attributed to depositional factors, such as textural heterogeneity and carbonate content facilitating karst dissolution. Moreover, numerical modeling indicated the feasibility of sustainable groundwater withdrawal though pumping, especially in nearshore sediments, offering a mitigation measure for future water supply challenges during droughts. Therefore, nearshore deposits cropping out in other sectors of the Northern Apennines hold a great potential to mitigate groundwater shortages during droughts and should be the object of further hydrogeological investigations. • Aquifer performance is a function of depositional environments in the study region • Aquifer performance and yield decline with distance from the paleo shoreline • Sustainable pumping can mitigate drought impacts on water supply in the region • Depositional environments can drive hydrogeological knowledge in other regions
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Filippini et al. (2025) studied this question.
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