Volume 39, Issue 3 e70100
RESEARCH ARTICLE

Numerical Modelling of Groundwater Flow in an Urban Aquifer Under Extensive Artificial Recharge Forcings

Ameerah H. Alkandari

Ameerah H. Alkandari

Civil Engineering Department, College of Engineering and Petroleum (COEP), Kuwait University, Safat, Kuwait

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Abdullah A. Alsumaiei

Corresponding Author

Abdullah A. Alsumaiei

Civil Engineering Department, College of Engineering and Petroleum (COEP), Kuwait University, Safat, Kuwait

Correspondence:

Abdullah A. Alsumaiei ([email protected])

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First published: 07 March 2025
Citations: 1

Funding: The authors received no specific funding for this work.

ABSTRACT

With a steadily growing population and increasingly limited natural freshwater resources, water-scarce regions must implement smart interventions to sustainably manage their water resources. Using Groundwater Vistas software, a modelling framework for Kuwait City urban aquifer was developed to address this issue. This framework was employed to create a numerical model of the shallow aquifer beneath the urbanised aquifer of Kuwait City. The model was calibrated using groundwater levels from 15 calibration points across the modelled area. Two key factors influenced the calibration: the constant head boundary condition applied upstream in the model domain and the horizontal hydraulic conductivity. The model performed satisfactorily achieving a Nash-Sutcliffe efficiency coefficient of 0.983, a root-mean-square error of 1.134 m, and a Kling-Gupta efficiency of 0.971. These results were then used to simulate two complex hydrogeological processes affecting the Kuwait City aquifer: unplanned dewatering schemes and incidental recharge from anthropogenic watering practices. It was found that altering the pumping rate between 250 and 2250 m3/day, resembling the dewatering process, could lower the groundwater level by approximately 1.21–1.79 m in coastal areas. Conversely, an unplanned recharge of 1500–6000 m3/day could substantially raise groundwater levels by approximately 2.5–3 m in inland areas. However, these findings should be cautiously approached, as certain constraints may significantly influence the model's reliability. These constraints include the limited availability of data records and the possible existence of unknown sources/sinks to the aquifer. The outcomes of this study should aid water managers in establishing reliable groundwater control decisions in the study area and other areas with similar hydrogeologic characteristics.

Data Availability Statement

The data that support the findings of this study are available from the corresponding author upon reasonable request.

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