Compilation and mapping of hydrogeological data for the Tadla irrigation perimeter
With its lush fields and neighboring mountains, the Tadla Plain in central Morocco is an important agricultural area. Its climate is semi-arid to arid, with a dry season from June to September and a rainy season from October to May. Summer temperatures exceed 30°C, while winter temperatures fall bel...
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EDP Sciences
2025-01-01
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author | Iharzi Chaimae Najine Abdessamad Kassou Amina Benmoussa Amroumousa Mouzoun Ouafae Essahlaoui Ali Khrabcha Abdelali |
author_facet | Iharzi Chaimae Najine Abdessamad Kassou Amina Benmoussa Amroumousa Mouzoun Ouafae Essahlaoui Ali Khrabcha Abdelali |
author_sort | Iharzi Chaimae |
collection | DOAJ |
description | With its lush fields and neighboring mountains, the Tadla Plain in central Morocco is an important agricultural area. Its climate is semi-arid to arid, with a dry season from June to September and a rainy season from October to May. Summer temperatures exceed 30°C, while winter temperatures fall below 5°C. The area, which is a part of the Oum Erbia River basin, is mostly dependent on groundwater for industry, agriculture, and drinking. In this study, 58 wells (42 from ORMVAT and 16 from ABHOER) were analyzed to determine the water table levels and groundwater quality. Different physico-chemical and bacteriological parameters were analyzed, such as, pH, EC, Cl⁻, NO₃⁻,SO₄²⁻, etc. As well as hydrodynamic data including permeability, transmissivity, storage coefficients, and piezometric levels. With permeability between 10⁻⁵ and 10⁻³ m/s and transmissivity between 1×10⁻³ and 5×10⁻² m²/s, groundwater flows from northeast to southwest, indicating moderate to strong water transmission. Moderate storage capacity is indicated by storage coefficients ranging from 3×10⁻² to 6×10⁻². However, the quality of groundwater varies; many wells, particularly in the Beni Amir nappe, exhibit poor quality. Concentrations of electrical conductivity (EC) and chloride ions (Cl-) are high in most wells. |
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institution | Kabale University |
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language | English |
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spelling | doaj-art-6ea02dfa750a445ba86143f3a4e5eec72025-02-05T10:49:23ZengEDP SciencesE3S Web of Conferences2267-12422025-01-016070200410.1051/e3sconf/202560702004e3sconf_errachidia2024_02004Compilation and mapping of hydrogeological data for the Tadla irrigation perimeterIharzi Chaimae0Najine Abdessamad1Kassou Amina2Benmoussa Amroumousa3Mouzoun Ouafae4Essahlaoui Ali5Khrabcha Abdelali6Geo-Resource Geo-Environment Geological and Oasis Heritage Research Team, Department of Geosciences, Faculty of Sciences and Techniques, Moulay Ismail UniversityGeoresources and Environment Laboratory, Department of Earth Science, Faculty of Science and Technology, Moulay ISlimane UniversityGeo-Resource Geo-Environment Geological and Oasis Heritage Research Team, Department of Geosciences, Faculty of Sciences and Techniques, Moulay Ismail UniversityGeoresources and Environment Laboratory, Department of Earth Science, Faculty of Science and Technology, Moulay ISlimane UniversityGeo-Resource Geo-Environment Geological and Oasis Heritage Research Team, Department of Geosciences, Faculty of Sciences and Techniques, Moulay Ismail UniversityLaboratory of Geoengineering and Environment, Research Group “Water Sciences and Environment Engineering”, Department of Geology, Faculty of Sciences, Moulay Ismail UniversityLaboratory of Geoengineering and Environment, Research Group “Water Sciences and Environment Engineering”, Department of Geology, Faculty of Sciences, Moulay Ismail UniversityWith its lush fields and neighboring mountains, the Tadla Plain in central Morocco is an important agricultural area. Its climate is semi-arid to arid, with a dry season from June to September and a rainy season from October to May. Summer temperatures exceed 30°C, while winter temperatures fall below 5°C. The area, which is a part of the Oum Erbia River basin, is mostly dependent on groundwater for industry, agriculture, and drinking. In this study, 58 wells (42 from ORMVAT and 16 from ABHOER) were analyzed to determine the water table levels and groundwater quality. Different physico-chemical and bacteriological parameters were analyzed, such as, pH, EC, Cl⁻, NO₃⁻,SO₄²⁻, etc. As well as hydrodynamic data including permeability, transmissivity, storage coefficients, and piezometric levels. With permeability between 10⁻⁵ and 10⁻³ m/s and transmissivity between 1×10⁻³ and 5×10⁻² m²/s, groundwater flows from northeast to southwest, indicating moderate to strong water transmission. Moderate storage capacity is indicated by storage coefficients ranging from 3×10⁻² to 6×10⁻². However, the quality of groundwater varies; many wells, particularly in the Beni Amir nappe, exhibit poor quality. Concentrations of electrical conductivity (EC) and chloride ions (Cl-) are high in most wells.https://www.e3s-conferences.org/articles/e3sconf/pdf/2025/07/e3sconf_errachidia2024_02004.pdfgroundwater qualityhydrogeologyhydrologyhydrochemistry1hydrodynamicsgistadla plain |
spellingShingle | Iharzi Chaimae Najine Abdessamad Kassou Amina Benmoussa Amroumousa Mouzoun Ouafae Essahlaoui Ali Khrabcha Abdelali Compilation and mapping of hydrogeological data for the Tadla irrigation perimeter E3S Web of Conferences groundwater quality hydrogeology hydrology hydrochemistry 1hydrodynamics gis tadla plain |
title | Compilation and mapping of hydrogeological data for the Tadla irrigation perimeter |
title_full | Compilation and mapping of hydrogeological data for the Tadla irrigation perimeter |
title_fullStr | Compilation and mapping of hydrogeological data for the Tadla irrigation perimeter |
title_full_unstemmed | Compilation and mapping of hydrogeological data for the Tadla irrigation perimeter |
title_short | Compilation and mapping of hydrogeological data for the Tadla irrigation perimeter |
title_sort | compilation and mapping of hydrogeological data for the tadla irrigation perimeter |
topic | groundwater quality hydrogeology hydrology hydrochemistry 1hydrodynamics gis tadla plain |
url | https://www.e3s-conferences.org/articles/e3sconf/pdf/2025/07/e3sconf_errachidia2024_02004.pdf |
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