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Mapping Favorable Groundwater Potential Recharge Areas Using a GIS-Based Analytical Hierarchical Process – A Case Study of Ferkla Oasis, Morocco

Ismail Ait Lahssaine, Lahcen Kabiri, Badre Messaoudi, Badre Essafraoui, Mohamed El Ouali, Lamya Ouali, Jean Albergel, Meryem El Amraoui, Amina Kassou, Essahlaoui Ali

Ecological Engineering & Environmental Technology

2024

Vol. 25, iss. 3

311--325

In the Ferkla Oasis, much like in numerous other oases across the southeastern region of Morocco, a range of socioeconomic and environmental challenges are intricately linked to the inadequate management of water resources. One proposed remedy to address these concerns is the implementation of artificial aquifer recharge, which stands as an alternative strategy to safeguard the crucial oasis ecosystems. Thus, to evaluate the viability of this method in promoting sustainable water resource usage, it becomes imperative to delineate groundwater recharge potential zones (GRPZs). This study aims to achieve this objective by mapping GRPZs within the Ferkla Oasis, employing a fusion of the analytical hierarchy process (AHP), geospatial information derived from remote sensing (RS), and geographic information system (GIS) technologies. In pursuit of this goal, an array of geological, topographical, pedological, hydrological, and climatic criteria have been meticulously selected, classified, and assigned weights following their relevance to water infiltration suitability. This comprehensive approach culminates in the generation of seven thematic maps: slope, lineament density, lithology, soil type, drainage density, land use/land cover, and rainfall distribution. Through the integration of these aforementioned maps, a tripartite classification of potential GRPZs emerges, comprising low, medium, and high categories. The findings underscore the distribution: 30% of the total study area exhibits a low potential for GRPZs, 50% of the total land area is characterized as having medium potential GRPZs, while the remaining 20% is designated as high potential GRPZs. These outcomes have been substantiated through validation against piezometric levels, which have been ascertained through recent field surveys. Consequently, these results stand as a testament to the efficacy of the presented approach as a robust decision-making tool. The approach effectively facilitates the establishment of conditions conducive to viable artificial recharge, thereby offering a means to safeguard the groundwater reservoirs that sustain the fragile oasis environments.

Temperatura wód podziemnych jako wskaźnik zasilania na przykładzie ujęcia dla Wrocławia

Błachowicz Marek, Buczyński Sebastian, Staśko Stanisław

Biuletyn Państwowego Instytutu Geologicznego

2019

nr 475, Hydrogeologia z. 16

19--25

Celem badań jest testowanie metody i wstępna ocena wielkości infiltracji efektywnej na podstawie wyników pomiarów temperatury w piezometrach w otoczeniu studni i stawów infiltracyjnych na terenach wodonośnych Wrocławia. Badania zmienności temperatury wód podziemnych w sieci obserwacyjnej na obszarze sztucznej infiltracji przeprowadzono w sieci 11 piezometrów. Wody pierwszego poziomu wodonośnego występują w aluwialnych osadach piaszczystych i zalegają na głębokościach 2–12 m. Roczne pomiary temperatur wód podziemnych w sieci obserwacyjnej na stałej głębokości (3–4 m) wykazały szeroki zakres zmian od 1,5 do 25,9°C. Przedstawiono charakterystyczne i typowe zakresy średnich zmian temperatur w przedziale 9,3–15,6°C zarejestrowane w 2018 r. Na podstawie profilowania termicznego w wybranym punkcie obliczono średnią wartość zasilania, stosując metodykę zaproponowana przez Taniguchiego (1993, 1994). Obliczona wstępnie wartość sztucznego zasilania wynosi 20,19 mm/d i odpowiada wielkości zasobów obliczonych na podstawie modelowania numerycznego.

The main goal of the research is to test the method and the preliminary assessment of the amount of the effective infiltration based on temperature measurement results in a piezometers network surrounded by wells and ponds for the infiltration water intake of the city of Wrocław. The study of temperature variation of the groundwater monitoring network in the area of artificial infiltration was conducted in 11 network observation points. Groundwater in the first shallow aquifer occurs in alluvial sediments at depths exceeding 2–12 m. Annual temperature measurements of the groundwater monitoring network for a constant depth (3–4 m) showed a wide range of changes from 1.5 to 25.9°C. The groundwater shows the typical values of medium temperature changes in the range of 9.3–15.6°C recorded in 2018. On the basis of thermal profiling in a selected point, the average recharge rate has been calculated by applying the method proposed by Taniguchi (1993, 1994). The preliminary calculated value of the groundwater artificial recharge is 20.19 mm/d and corresponds to the value evaluated by numerical modelling.