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WATPPASS is suited for small watershed with significant groundwater flows and complex aquifer systems.
Numerical ground water models have proven to be essential when dealing with complex aquifer situations.
The performance of the proposed model is evaluated on two hypothetical examples for simple and complex aquifer geometries, measurement error conditions, and different HS solution parameter sets.
This study presents the application of Evolutionary Polynomial Regression (EPR) as a pattern recognition system to predicate the behavior of nonlinear and computationally complex aquifer systems subjected to seawater intrusion (SWI).
To develop a conceptual model of recharge and inter-aquifer connectivity for a complex aquifer system in southwestern Victoria, Australia, a three-dimensional (3D) geological model was constructed and used to examine the influence of the regional geology on groundwater composition and age, as well as recharge mechanisms.
Pumping signals propagate through complex aquifer systems at different rates.
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Knowing this structure would probably improve the ability to design proper scenarios of water resources exploitation and management in complex aquifers.
Moreover, the groundwater of Peninsular gneissic complex aquifers in the Deccan plateau region are suspected to have high salt content and to be poor in quality (Suresh and Kottureshwara 2009; Kumar et al. 2009; Reddy and Patode 2013; Yadagiri et al. 2015).
It ranges from smallholder irrigation in remote locations to meet local needs (typical of Sahelian irrigation from basement complex aquifers) to large-scale commercial irrigation to feed national markets (wheat irrigation based on highly productive dolomite aquifers in Zambia).
The model domain comprised a hydrologically complex esker aquifer in Northern Finland with interconnected lakes, streams and wetlands.
The obtained results provide new knowledge on using natural tracers in complex glacial aquifer systems and can be used in integrated groundwater surface water management.
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