4.6 Article

Application of Analytical Hierarchy Process and Geophysical Method for Groundwater Potential Mapping in the Tata Basin, Morocco

Journal

WATER
Volume 14, Issue 15, Pages -

Publisher

MDPI
DOI: 10.3390/w14152393

Keywords

groundwater potential map; analytical hierarchy process; geographic information system; teledetection; geophysics; Morocco

Funding

  1. King Saud University, Riyadh, Saudi Arabia [RSP-2021/249]

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Ensuring water availability in semi-arid mountainous regions requires controlling factors influencing groundwater availability. The use of GIS, remote sensing, and decision-making methods can help understand and assess water availability. In the Tata basin in Southeast Morocco, ten factors were used to explain the groundwater potentiality map, identifying different levels of potential zones.
Ensuring water availability for agriculture and drinking water supply in semi-arid mountainous regions requires control of factors influencing groundwater availability. In most cases, the population draws its water needs from the alluvial aquifers close to villages that are already limited and influenced by current climatic change. In addition, the establishment of deep wells in the hard rock aquifers depletes the aquifer. Hence, understanding the factors influencing water availability is an urgent requirement. The use of geographic information system (GIS), and remote sensing (RS), together with decision-making methods like analytical hierarchy process (AHP) will be of good aid in this regard. In the Tata basin, located in SE Morocco, ten factors were used to explain the groundwater potentiality map (GWPM). Five categories of potential zones were determined: very low (8.67%), low (17.74%), moderate (46.77%), high (19.95%), and very high (6.87%). The efficiency of the AHP model is validated using the ROC curve (receiver operating characteristics) which revealed a good correlation between the high potential groundwater zones and the spatial distribution of high flow wells. Geophysical prospecting, using electrical resistivity profiles, has made it possible to propose new well sites. It corresponds to conductive resistivity zones that coincide with the intersection of hydrogeological lineaments.

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