Please use this identifier to cite or link to this item: http://localhost:8080/xmlui/handle/123456789/1903
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dc.contributor.authorMessaoudi, Khmais-
dc.date.accessioned2025-01-22T13:25:59Z-
dc.date.available2025-01-22T13:25:59Z-
dc.date.issued2010-
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/1903-
dc.description.abstractThis memory can be recognized as the first feet to study a phenomenon called “this rise of bottom water in region of OUDE SOUF“. Firstly, we shall treat this phenomenon generally various sides geographically, geologically, Hydro-logiclly, its relation ship with the climate and so with the type of soil, and also we’ll analyses this water chemically. After stating all these previous factors, and their influence in rising bottom water, we’ll try to discover the different causes that affect on; after that, we’ll give detailed analyses to this phenomenon. Finally, we’ll give different suggestions we hope that it is valid and useableen_US
dc.language.isofren_US
dc.relation.ispartofseries2-0012-10;-
dc.subjectDrainage ; Nappe phréatique ; Oued Soufen_US
dc.titleContribution a l'étude de drainage contre la remontée de la nappe phréatique dans la région d'Oued Souf (w. el Oued)en_US
dc.typeThesisen_US
Appears in Collections:Conception des Systèmes d'Irrigation et de Drainage

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