@conference {8520,
	title = {Geoelectric Characterization of Bir Haddada Plain, NE Algeria},
	booktitle = {Conference of the Arabian Journal of Geosciences},
	year = {2024},
	pages = { 89{\textendash}92},
	publisher = { Advances in Science, Technology \& Innovation ((ASTI))},
	organization = { Advances in Science, Technology \& Innovation ((ASTI))},
	abstract = {
	The Bir Haddada Plain is located in eastern Algeria and is characterized by a semi-arid climate with low rainfall. The irrigation of this region{\textquoteright}s agricultural lands is almost assured by hundreds of wells that exploit the shallow aquifer. The strong pumping of the shallow aquifer triggered the latter{\textquoteright}s utter exhaustion. To resolve the irrigation water shortage, we need to explore the subsoils to find potentially exploitable aquifers more closely. The objective is the geoelectric characterization of this area and also the detection of underground water aquifers. The geophysical study by vertical electrical survey (VES) is more adequate because it allows identifying the conductive and resistant layers to the electric field. Exploration by VES was carried out with a spacing of the measuring electrodes ranging from\&nbsp;AB = 100 to\&nbsp;AB = 1000\&nbsp;m. The study of the results obtained indicates that the prospective zone is distinguished by a filling exceeding 300\&nbsp;m corresponding to the miopliocene formations. These formations are generally clays, conglomerates, and lacustrine limestones. In contrast, the low resistivity values seem to be related to the presence of conductive formations such as Miopliocene gypsum clays or to the presence of Triassic rocks linked to the contact of the bedrock. The maps of the apparent resistivity often show a network of different direction faults.

},
	url = {https://link.springer.com/chapter/10.1007/978-3-031-43807-3_18?utm_source=researchgate.net\&utm_medium=article},
	author = {Djenba, Samir and Abdelhamid Khedidja and Adjroud, Sonia}
}
@conference {4868,
	title = {TERRASSES FLUVIATILES QUATERNAIRES DE L\&$\#$39;OUED EL HAY (BATNA, NE ALG{\'E}RIE): S{\'E}DIMENTOLOGIE ET CARACT{\'E}RISTIQUES DE L\&$\#$39;ENVIRONNEMENT S{\'E}DIMENTAIRE.},
	booktitle = {4{\`e}me Colloque International les G{\'e}osciences au service du D{\'e}veloppement durable (2018)  T{\'e}bessa, Alg{\'e}rie},
	year = {2018},
	abstract = {Une {\'e}tude stratigraphique et s{\'e}dimentologique a {\'e}t{\'e} r{\'e}alis{\'e}e sur une terrasse alluviale de la r{\'e}gion d{\textquoteright}Oued El Hay, au sud de Batna (NE Alg{\'e}rie). Les structures s{\'e}dimentaires observ{\'e}es sont principalement des zones d{\textquoteright}{\'e}rosion, des zones inondables, des figures en biseau et des variations d{\textquoteright}{\'e}paisseur associ{\'e}es {\`a} des joints de stratification. Du point de vue s{\'e}dimentologique, les s{\'e}diments sont domin{\'e}s par des fractions argilo-limono-sableuses, suivies par des fractions de gravier et de cailloux. Les teneurs mod{\'e}r{\'e}es en CaCO3 r{\'e}sultent de la dissolution des reliefs calcaires {\`a} proximit{\'e} (calcaire cr{\'e}tac{\'e}) associ{\'e}e {\`a} l{\textquoteright}augmentation de la temp{\'e}rature et l{\textquoteright}humidit{\'e} du milieu. L{\textquoteright}observation morphoscopique de grains de quartz avec une loupe binoculaire permet d{\textquoteright}offrir une {\'e}volution plus ou moins importante, car ils sont souvent {\'e}mouss{\'e}s ou sous-arrondis. L{\textquoteright}{\'e}tude s{\'e}dimentologique a {\'e}t{\'e} r{\'e}alis{\'e}e sur 16 {\'e}chantillons pr{\'e}lev{\'e}s syst{\'e}matiquement du haut vers le bas de la coupe stratigraphique. L{\textquoteright}examen de la taille brute de la fraction inf{\'e}rieure {\`a} 2 mm a permis d{\textquoteright}individualiser 03 niveaux dans des couches s{\'e}dimentaires, certaines fractions grossi{\`e}res riches (gravier, cailloux et blocs) alternant avec des couches riches en sable et en limon. Le pourcentage de fraction d{\textquoteright}argile est dominant et reste pratiquement constant presque tout au long de la section stratigraphique.},
	url = {https://www.researchgate.net/publication/330038660_TERRASSES_FLUVIATILES_QUATERNAIRES_DE_L{\textquoteright}OUED_EL_HAY_BATNA_NE_ALGERIE_SEDIMENTOLOGIE_ET_CARACTERISTIQUES_DE_L{\textquoteright}ENVIRONNEMENT_SEDIMENTAIRE},
	author = {Fouad Djaiz and Defaflia Nabil and Bachir Lamouri and ATHAMENA Ali and Boushaba Abdellah}
}
