Articles | Volume 58
https://doi.org/10.5194/adgeo-58-47-2022
https://doi.org/10.5194/adgeo-58-47-2022
14 Nov 2022
 | 14 Nov 2022

Upwelling mechanisms of deep saline waters via Quaternary erosion windows considering varying hydrogeological boundary conditions

Elena Chabab, Michael Kühn, and Thomas Kempka

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Cited articles

Beutler, G. and Stackebrandt, W.: The tectonic pattern of the sedimentary cover of Brandenburg – suggestion for a uniform nomenclature, Brandenburg. Geowiss. Beitr., 19, 93–109, 2012 (in German). 
Brose, D. and Hermsdorf, A.: Geogenic salinization in aquifers of Brandenburg, Brandenburg. Geowiss. Beitr., 24, 7–16, 2017 (in German). 
Cai, J., Taute, T., and Schneider, M.: Saltwater Upconing Below a Pumping Well in an Inland Aquifer: a Theoretical Modeling Study on Testing Different Scenarios of Deep Saline-Groundwater Pathways, Water Air Soil Pollut., 225, 2203, https://doi.org/10.1007/s11270-014-2203-7, 2014. 
Chandler, R. and McWhorter, D.: Upconing of the salt-water-fresh-water interface beneath a pumping well, Ground Water, 13, 354–359, https://10.1111/j.1745-6584.1975.tb03599.x, 1975. 
FUGRO GmbH Berlin: Grundlagenermittlung zur Stofftransportmodellierung Schwarze Pumpe – Tabelle 4, Berlin, 1998 (unpublished, in German). 
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Short summary
The present study, uses density-driven flow and transport models to evaluate mechanisms of saline water intrusion from deep aquifers into the freshwater column used for drinking water supply under different boundary conditions and for a specific site in the German Federal State of Brandenburg. Results show that mainly decreasing groundwater recharge leads to increased and earlier salinisation which highlights the need for waterworks to initiate effective countermeasures quickly and in time.