@proceedings {63446,
	title = {Caract{\'e}risation g{\'e}ologique et apport de la g{\'e}ophysique pour la mobilisation des ressources hydriques dans le bassin de Gadaine (Ain Yagout, Alg{\'e}rie NE)},
	journal = {Le 1er S{\'e}minaire National en G{\'e}osciences et Environnement 23{\textendash} 24 Octobre (SGSE-2019)},
	year = {2019},
	month = {2019},
	address = {Tamanrasset, Algeria},
	url = {https://www.researchgate.net/profile/Athamena-Ali/publication/337603986_CARACTERISATION_GEOLOGIQUE_ET_APPORT_DE_LA_GEOPHYSIQUE_POUR_LA_MOBILISATION_DES_RESSOURCES_HYDRIQUES_DANS_LE_BASSIN_DE_GADAINE_AIN_YAGOUT_ALGERIE_NE/links/5e865d7ba6fdcca789ec8f40/CAR},
	author = {Fouad, DJAIZ and Ali, ATHAMENA and Bachir, Lamouri and Bousahaba, A. and Halima, BELALITE and Rachid, Touansa and Soumia, Khanfer and Manal, Marred and Imen, Chairat}
}
@article {64953,
	title = {Geological Characterization and contibution of Geophysics to the mobilization of water resources in the ain djasser basin (South-S{\'e}tifien, Algeria NE)},
	journal = {The Euro-arab Organization for Environment,Water and Desert Researches, (2018) Antalya, TurquieThe Euro-arab Organization for Environment,Water and Desert Researches, (2018) Antalya, Turquie},
	year = {2018},
	month = {2018},
	author = {Fouad, DJAIZ and Nabil, Defaflia and Ali, ATHAMENA and Bachir, Lamouri and Mabrouk, Boughdiri and Halima, BELALITE and Abdellah, Boushaba}
}
@proceedings {65170,
	title = {The Impact of the Mobilization of Water Resources in Semi-Arid Areas on Sustainable Development: The Case of Timgad Basin, Northeastern of Algeria},
	journal = {Conference of the Arabian Journal of Geosciences},
	year = {2018},
	month = {2018},
	pages = {355-357},
	publisher = {Springer},
	author = {Ali, ATHAMENA and Redha, MENANI Mohamed and Fouad, DJAIZ and Halima, BELALITE}
}
@article {61435,
	title = {Flux azot{\'e} dans les eaux souterraines, origine et devenir, cas de la plaine de Zana, est alg{\'e}rien},
	year = {2018},
	abstract = {
	We tried, by this work, to contribute a share to study it the aquifers of the plain of Zana, and to evaluate the



	risks of pollu



	tion related to nitrogenized flow.



	The plain of Zana belongs to the catchment area of the high plateaus constantinois and more precisely of under



	area catchment Merdja Zana, which extends on a surface of approximately 369 Km{\texttwosuperior}.



	The study of geology with



	the data of geophysics highlights the existence of two formations.



	First formation, of



	Mio



	-



	Plio



	-



	Quaternary surface of age formed by levels of sand, gravel, water limestone and argillaceous



	intercalations.



	The second formation, it is carbonated and formed



	primarily by limestones of the lower Cretaceous and



	Jurassic superior of the southern unit s{\'e}tifien and parautochtone aur{\'e}sien.



	The covering of surface reaches in certain



	places the 150m thickness in particular in the medium of the plain and a low thicknes



	s in the vicinity of the solid



	masses.



	As for the carbonated formations they have 350m thickness.



	The geomorphology, shows that our basin is lengthened, it has an average altitude of 935m and it is



	characterized by a moderate relief and of soft slope.



	Th



	e hydrographic network is fart to develop and of endoreic type



	with a temporary flow.



	The climatological study showed that the area of study has an arid semi climate with an overdrawn



	hydrological assessment.



	The outline hydrogeologic of the plain show



	s that the trainings of the lower Cretaceous and the Jurassic



	superior can offer very interesting aquiferous possibilities just as the surface formation, it presents considerable



	aquiferous potentialities.



	Piezometry shows a convergence towards the depress



	ions of Merdja de Zana and Chott



	Saboun, which represent natural discharge system of the tablecloth.



	The hydrochimic study made it possible to allot the evaporitic origin to the elements Na



	+



	, Mg



	++



	, K



	+



	, Cl



	-



	,



	SO4



	--



	, as for element HCO3



	-



	,



	it results fr



	om the carbonated formations



	The two partners of analyses carried out show that water resulting from the aquifer surface and the karstic aquifer has



	the same facies hydrochimic which of magnesian type is chlorinated and sulphated, which testifies to the



	existence of a



	probable interaction between the two aquifers.



	.



	Nitric pollution is not visible although the area is with agricultural vocation

},
	url = {http://docplayer.fr/66130950-Flux-azote-dans-les-eaux-souterraines-origine-et-devenir-cas-de-la-plaine-de-zana-est-algerien.html},
	author = {Ali, ATHAMENA and Redha, MENANI Mohamed and Halima, BELALITE}
}
