@mastersthesis {5702,
	title = {Contribution au Suivi pi{\'e}zom{\'e}trique et hydrochimie  dans la plaine de Belezma (W, de Batna)},
	year = {2017},
	author = {Righi Asma}
}
@mastersthesis {5697,
	title = {{\'E}tude stratigraphique et s{\'e}dimentologique du Campanien sup{\'e}rieur du massif d\&$\#$39;El Kantara},
	year = {2017},
	author = {Touahria Kamel and Khabar Ali}
}
@mastersthesis {5689,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude hydrog{\'e}ologique de la nappe Mio-Plioc{\`e}ne de la r{\'e}gion de Tolga},
	year = {2017},
	author = {Toumi.A}
}
@mastersthesis {5686,
	title = {Impact des plans d\&rsquo;eau artificiels sur les r{\'e}gimes hydrologiques - Cas du barrage de beni haroune - mila - Est alg{\'e}rien},
	year = {2017},
	author = {Ghemima. Z}
}
@mastersthesis {5681,
	title = {Les effondrements dans les terrains karstiques du plateau de Cheria (NE de l\&$\#$39;Alg{\'e}rie), impacts gotechnique et environnementaux et cartographie des zones vuln{\'e}rables au ph{\'e}nom{\`e}ne.},
	year = {2017},
	abstract = {Les effondrements des cavit{\'e}s souterraines dans les calcaires karstifi{\'e}s constituent un al{\'e}a g{\'e}ologique s{\'e}rieux qui continue {\`a} recevoir une intention particuli{\`e}re {\`a} l{\textquoteright}{\'e}chelle de la plan{\`e}te. Il s{\textquoteright}agit d{\textquoteright}un ph{\'e}nom{\`e}ne tr{\`e}s connus, li{\'e} {\`a} la pr{\'e}sence de vides souterrains dans les terrains calcaires, dolomitiques et gypsif{\`e}res. Le plateau de Ch{\'e}ria correspond {\`a} une structure synclinale, grossi{\`e}rement triangulaire d{\textquoteright}orientation NE {\textendash} SW affect{\'e} par une fracturation orthogonale {\`a} l{\textquoteleft}axe du pli. Il est essentiellement form{\'e} de calcaires Eoc{\`e}ne largement karstifi{\'e} et recouvert de mat{\'e}riaux meubles, essentiellement des alluvions, des argiles et des encroutements calcaires. Ce bassin en question abrite trois aquif{\`e}res superpos{\'e}s, l{\textquoteright}aquif{\`e}re du Maastrichtien, l{\textquoteright}Eoc{\`e}ne et la nappe alluviale du Moi-Plio-Quaternaire. Celle qui fait l{\textquoteright}objet de cette {\'e}tude est la nappe de l{\textquoteright}Eoc{\`e}ne. Le sens d{\textquoteright}{\'e}coulement g{\'e}n{\'e}rale dans les nappes souterraines notamment les alluvions et l{\textquoteright}Eoc{\`e}ne est sensiblement Nord-Sud. La surexploitation actuelle des eaux souterraines a rendu la nappe des alluvions sans int{\'e}r{\^e}t hydrog{\'e}ologique, et a caus{\'e} un grand rabattement dans les calcaires de l{\textquoteright}Eoc{\`e}ne. Les m{\'e}thodes directes et indirectes d{\textquoteright}explorations du sous-sol de la r{\'e}gion ont r{\'e}v{\'e}l{\'e}s la pr{\'e}sence de plusieurs cavit{\'e}s souterraines de dimensions importantes. La m{\'e}thode de tomographie {\'e}lectrique, G{\'e}oradar et les sondages m{\'e}caniques ont montr{\'e} l{\textquoteright}existence {\`a} faible profondeur des cavit{\'e}s dans la r{\'e}gion d{\textquoteright}{\'e}tude. La stabilit{\'e} de ces cavit{\'e}s d{\'e}pend d{\textquoteright}un c{\^o}t{\'e} des propri{\'e}t{\'e}s m{\'e}caniques de la masse rocheuse formant le toit de la galerie, et les dimensions de cette derni{\`e}re. Cette {\'e}tude nous a permis d{\textquoteright}{\'e}tablir des relations entre l{\textquoteright}{\'e}paisseur du toit, largeur de cavit{\'e}, et la charge pour un RMR (Rock masse rating) variable. La cartographie men{\'e}e {\`a} l{\textquoteright}{\'e}chelle de la r{\'e}gion a pu d{\'e}limiter les zones susceptibles de pr{\'e}senter des cavit{\'e}s naturelles instables et cela va permet en cons{\'e}quence de trouver des solutions au probl{\`e}me de l{\textquoteright}effondrement {\`a} l{\textquoteright}{\'e}chelle de la r{\'e}gion},
	url = {http://www.secheresse.info/spip.php?article79566},
	author = {Azizi Yacine}
}
@mastersthesis {5679,
	title = {APPROCHES HYDROGEOCHIMIQUES ET GEOTHERMOMETRIQUES POUR L\&rsquo;ETUDE DES EAUX THERMALES  CAS DU SYSTEME GEOTHERMAL EXPLOITE DANS LA REGION DE BISKRA AU SUD ALGERIEN},
	year = {2017},
	author = {Chafou Nasereddine}
}
@proceedings {4888,
	title = {{\'E}tude tectono-s{\'e}dimentaire de la s{\'e}rie campanienne de Dj. Lekhal (plaine d\&$\#$39;ain Touta)},
	journal = {La 4eme {\'e}dition du Congr{\`e}s des Doctorants 2017 de la FSTGAT se tiendra le 24 et 25 Avril 2017, \&aacut la maison de la science, USTHB, Alger},
	year = {2017},
	author = {Benmansour Sana}
}
@proceedings {4871,
	title = {Sedimentology, Geochemistry and Various Microfaunal Component Responses to Environmental Fluctuations of the Cenomanian-Turonian Boundary at Th{\'e}ni{\`e}t El Manchar (Batna, NE Algeria)},
	journal = {19th International Conference on Geological and Earth Sciences, Word Academy of Science Energinee Ring and Technology, Rome, Italy },
	year = {2017},
	author = {Slami Rafika}
}
@proceedings {4870,
	title = {Les impactes des plans d\&rsquo;eaux artificielles sur les r{\'e}gimes climatiques et hydrologiques {\`a} l\&rsquo;{\'e}chelle. Cas d\&rsquo;un bassin versant du barrage de Beni Haroune, (Mila Est Alg{\'e}rien)},
	journal = {Colloque International Eau-Soci{\'e}t{\'e}-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre 2017.},
	year = {2017},
	author = {ATHAMENA Ali and DJAIZ Fouad and Belalit Halima and Guemima. Z and Toufaha. S and Kihel. K}
}
@proceedings {4869,
	title = {G{\'e}om{\'e}trie de l\&rsquo;aquif{\`e}re N{\'e}og{\`e}ne dans le bassin d\&rsquo;El Outaya, Atlas saharien au sud alg{\'e}rien},
	journal = {Colloque International Eau-Soci{\'e}t{\'e}-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre 2017},
	year = {2017},
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@proceedings {4850,
	title = {caracterisation hydrogeologique et hydro-chimique du bassin neogene de timgad (nord-est algerien)},
	journal = {The 1st International Symposium (WREIANA 2017) Water Resources and Environmental Impact Assessment in North Africa, Gafsa, Tunisie},
	year = {2017},
	author = {Brinis Nafaa}
}
@proceedings {4836,
	title = {Caract{\'e}risation hydrog{\'e}ologique et hydrochimique du bassin n{\'e}og{\`e}n,e de Timgad, NE alg{\'e}rien},
	journal = {1er International symposium - WREIANA, 24-26, Gafsa, Tunisie},
	year = {2017},
	author = {Lebchek Soumia and MENANI Mohamed redha and Brinis Nafaa}
}
@article {3629,
	title = {Le campanien -Maastrichtien du bassin des Aur{\`e}s, Alg{\'e}rie: Biostratigraphie, Pal{\'e}oenvironnements et leurs implications.},
	journal = {Annal de pal{\'e}ontologie , Science Direct-Elsevier masson France},
	year = {2017},
	url = {http://doi.org/10.1016/j.annpal. 2017.11.001},
	author = {Benmansour Sana and Yahiaoui Abdelouahab}
}
@article {3625,
	title = {EVALUATION OF THE WATER NEEDS OF CROPS UNDER ARID CLIMATIC CONDITIONS. CASE OF TINIBAOUINE REGION (NORTH EAST OF ALGERIA), Feb, ISSN / e-ISSN: 2186-2990 / 2186-2990 },
	journal = {International Journal of GEOMATE},
	volume = {Vol. 12},
	number = {Issue 30},
	year = {2017},
	pages = {pp. 1 - 7},
	abstract = {The Tinibaouine region, located in north-eastern Algeria on the borders of the Batna-Belezma Mountains, is characterized by a semi-arid to arid climate with an average annual rainfall not exceeding 465 mm and an average annual temperature of around 22 C. This region is characterized by the cultivation of apricots as essential crop followed by that of olives, whose plots are all irrigated with the Tinibaouine spring water. These are 450 Ha of trees for apricot and 108 Hectare for olives which constitute the principal revenue of the citizens of this small village. This paper estimated the crop reference and actual evapotranspiration (ETO) respectively and the irrigation water requirement of apricot trees and olive trees. The long recorded climatic data, crop and soil data, effective water allocation and planning, the information about crop water requirements, irrigation withdrawals were computed with the Cropwat model which is based on the United Nations{\textquoteright} Food and Agriculture Organization (FAO), the Penman-Monteith method was used to estimate ETo. Crop coefficients (Kc) from the phenomenological stages of apricot and olive were applied to adjust and estimate the actual evapotranspiration ETc through a water balance of the irrigation water requirements (IR). The results showed that the annual reference evapotranspiration (ETO) was estimated at 3.71 mm/day. The irrigation requirements were estimated at 35800 m3/hectare for apricot, 6980 m3/hectare for olive, also Irrigation needs estimated on land at 14185, 05 m3/hectare for olive and apricot.},
	url = {https://www.researchgate.net/publication/313316435_Assessment_of_the_water_needs_of_apricot_and_olive_crops_under_arid_climatic_conditions_Case_study_of_Tinibaouine_region_Northeast_of_Algeria},
	author = {Mansouri Zineb and MENANI Mohamed redha}
}
@mastersthesis {2921,
	title = {Etudes s{\'e}dimentologiques de la s{\'e}rie coniacienne du Dj Metlili (Algerie nord oriental)},
	year = {2017},
	author = {Bentahar Fahima}
}
@mastersthesis {2918,
	title = {Etude Pal{\'e}o-Environnemental de la R{\'e}gion de Ain Touta Au Quaternaire : Terrasses Fluviatiles d\&rsquo;Oued El Hai.},
	year = {2017},
	author = {Brikat and Sehtal Sami}
}
@mastersthesis {2917,
	title = {Etude Pal{\'e}o-Environnemental de la R{\'e}gion d\&rsquo;El Mather Au Quaternaire : Terrasses Fluviatiles d\&rsquo;Oued El Gourzi},
	year = {2017},
	author = {Bekkari Sif eddine and Adel Abdelhak}
}
@mastersthesis {2449,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude hydrog{\'e}ologique de la r{\'e}gion du Droh (w) Biskra},
	year = {2017},
	author = {Saada Brahim~Oussama}
}
@mastersthesis {2448,
	title = {Contribution {\`a} l\&rsquo;{\'e}tude hydrog{\'e}ologique du champ captant de l\&rsquo;oued Biskra},
	year = {2017},
	author = {Saber A}
}
@proceedings {2417,
	title = {hydrochemical analysis and evaluation of groundwater quality of an alluvial aquifer. algeria},
	journal = {1st Euro-Mediterranean Conference for Environmental Integration (EMCEI) Springer, Sousse. Tunisia},
	year = {2017},
	address = {Sousse. Tunisia},
	url = {https://www.emcei.net},
	author = {Drias Tarek and Fehdi Chemseddine and Belloula Moufida}
}
@proceedings {2326,
	title = {Qualit{\'e} chimique des eaux de l\&rsquo;aquif{\`e}re Moi-plioc{\`e}ne utilis{\'e} pour l\&rsquo;irrigation de la plaine d\&rsquo;El Outaya au sud Alg{\'e}rien},
	journal = {Colloque International Eau-Soci{\'e}t{\'e}-Climat 2017(ESC- 2017) Hammamet 2-3-4 Octobre },
	year = {2017},
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@proceedings {2297,
	title = {Qualit{\'e} des eaux du Complexe Terminale du Nord-Est Alg{\'e}rien. R{\'e}gion de Tolga},
	journal = {The 1St Atlas Georessources International Congress, (AGIC). 20-22 March, Hammet, Tunisia.},
	year = {2017},
	address = { Hammet, Tunisia.},
	author = {Zouaoui Siham and MENANI Mohamed redha and Bouabid Abd Ennasser}
}
@article {2195,
	title = {Rock Typing: Reservoir Determination from rock \&ndash; fluid interaction and dynamic behavior : Case Study from an Algerian Oil Field Reservoir},
	journal = {DGMK/{\"O}GEW-Fr{\"u}hjahrstagung, Fachbereich Aufsuchung und Gewinnung Celle, 5./6. April},
	year = {2017},
	abstract = {
	Rock typing is a process of rock classification based on mineralogical composition, grainshape pore size distribution (PSD) and communication. In addition to rock-fluid interaction, dynamic behavior and the capillary effect are also considered. In that purpose data need process involve: integrating, analyzing and synthesizing data brought out from different source: Petrophysics, cores analysis, well tests, MDT tooland production profiles. Achievement of rock typing reservoir based on fluid - solid behavior and their relation constitute an important issue not only for making distinguished different rock types but also for fluid gas contacts.For the case study, our investigation is concerned with the determination of the rock type dynamism resulting in reservoir rocks having similar dynamic behavior. Outcome from this process is to establish a representative petrophysical model able to predict any effect own to the change of the rock properties or fluid characteristics. Establishment of numerical model in\&nbsp; that context, and its relative changes can be ascribed to rapid petrophysical variation characteristics: related to pore size, geometry, grain size distribution, fluid behavior and circulation with essential reference to permeability. This latter can affect the simulation time and consequently, the accuracy in the calculation process.



	In this conducted investigation, application of linear regression method is involving permeability and porosity core measurement, stressing on their coefficient of correlation. Results have led to different clusters classification according to the linearity regarding permeability-porosity changes. Extrapolation can be made for the non-cored reservoir sections or non-cored boreholes associated to the considered field. In that principle geological models can be set.



	Application of these listed method for TAGI (TriasArgilo-GreseuxInferieur: Lower Shaly {\textendash} SansdtoneTriasic Formation) in B-H Basin (Algeria) has revealed the presence of six main rock types: sand type 1 (RT-1), sand Type 2 (RT-2), sand type 3 (RT-3), sand type 4 (RT-4), sand type 5 (RT-5) and sand type 6 (RT-6).

},
	author = {Benzagouta Mohammed Said and Belhouchet Houssam and Achi. N and Amro.M}
}
@proceedings {2173,
	title = {Caract{\'e}risation g{\'e}ologique et apport de la g{\'e}ophysique pour la mobilisation des ressources hydrique dans le bassin d\&$\#$39;Ain Djasser (Sud-setifien, Alg{\'e}rien NE)},
	journal = {Colloque international Eau{\textendash}Soci{\'e}t{\'e}{\textendash}Climat{\textquoteright}2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre .},
	year = {2017},
	address = {Hammamet, Tunis},
	author = {DJAIZ Fouad and Defaflia Nabil and Boushaba Abdellah and Marmi Ramdane and Dardakhe Mohamed and ATHAMENA Ali and ATHAMENA Malika}
}
@proceedings {2171,
	title = {Impacts des plans d\&$\#$39;Eau sur les r{\'e}gimes hydro-climatiques a l\&$\#$39;{\'e}chelle d\&$\#$39;un bassin verssant, cas du barrage de Beni Haroun, Milan Est Algerien},
	journal = {Colloque international Eau{\textendash}Soci{\'e}t{\'e}{\textendash}Climat{\textquoteright}2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre},
	year = {2017},
	address = {Hammamet, Tunis},
	author = {ATHAMENA Ali and DJAIZ Fouad and Bilalite Halima and Ghenima Z and Teffaha S and Kihel K}
}
@proceedings {2148,
	title = {G{\'e}om{\'e}trie de l\&rsquo;aquif{\`e}re N{\'e}og{\`e}ne dans le bassin d\&rsquo;El-Outaya, Atlas saharien au sud alg{\'e}rien },
	journal = {Colloque international Eau{\textendash}Soci{\'e}t{\'e}{\textendash}Climat{\textquoteright}2017 (ESC-2017), Hammamet, Tunis le 2, 3 et 4 Octobre },
	year = {2017},
	address = {Hammamet, Tunis },
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@proceedings {2145,
	title = {Qualit{\'e} chimique des eaux de l\&rsquo;aquif{\`e}re Mio-plioc{\`e}ne utilis{\'e}es pour l\&rsquo;irrigation de la plaine d\&rsquo;El-Outaya au sud alg{\'e}rien},
	journal = {Colloque international Eau{\textendash}Soci{\'e}t{\'e}{\textendash}Climat{\textquoteright}2017 (ESC-2017),Hammamet, Tunis le 2, 3 et 4 Octobre },
	year = {2017},
	address = {Hammamet, Tunis },
	author = {Brinis Nafaa and Boudoukha Abderahmane and DJAIZ Fouad}
}
@proceedings {2137,
	title = {Caract{\'e}risation des {\'e}coulements souterrains dans le socle precambrien fissure  de la region de tamanrasset},
	journal = {The 1st international symposium WREIANA, Gafsa 24-26 mars },
	year = {2017},
	address = { Gafsa },
	author = {Boulahbal Souad and MENANI Mohamed redha}
}
@proceedings {2136,
	title = {Etude des ecoulements souterrains dans les gneiss schisteux fissur{\'e}s du pr{\'e}cambrien de la region de tamanrasset},
	journal = {The 1st Atlas Georesources International Congress, Hammamet, tunisia 20-22 mars},
	year = {2017},
	address = {Hammamet, tunisia},
	author = {Boulahbal Souad and MENANI Mohamed redha}
}
@proceedings {2061,
	title = {Assessment of water requirements of olive and apricots trees in Tinibaouine region (north-eastern of Algeria). Impacts of Global Change on Western Mediterranean Aquifers,},
	journal = {Proceedings Congress on Groundwater and Global Change in the Western Mediterranean, Granada },
	year = {2017},
	pages = {pp 277-282},
	address = {Granada },
	url = {http://www.aih-ge.org/index.php/gwm-change-2017/},
	author = {Mansouri Zineb and MENANI Mohamed redha}
}
@proceedings {2011,
	title = {Influence des variations climatiques sur les r{\'e}serves d\&rsquo;eau souterraine des plaines de Zana Chott Saboun et Gadaine (Nord-Est Alg{\'e}rien)},
	journal = {Proceedings Congress on Groundwater and Global Change in the Western Mediterranean Granada. Impacts of Global Change on Western Mediterranean Aquifers},
	year = {2017},
	pages = {pp 171-176},
	address = {Granada},
	url = {http://www.aih-ge.org/index.php/gwm-change-2017/},
	author = {Bilalite Halima and MENANI Mohamed redha}
}
@article {1892,
	title = {Assessing soil loss using GIS based RUSLE methodology. Case of the Bou Namoussa watershed \&ndash; North-East of Algeria, 2018, PL ISSN 1429\&ndash;7426., Polish Academy of Sciences (PAN), Committee on Agronomic Sciences, Degruyte, DOI: 10.2478/jwld-2018},
	journal = {Journal of Water and Land Development },
	number = {No. 36 (I{\textendash}III)},
	year = {2017},
	pages = {pp 27{\textendash}35},
	abstract = {This study aims to estimating annual soil erosion rate and its spatial distribution in the Bou Namoussa water-shed located in the North-East of Algeria by applying the revised universal soil loss equation (RUSLE) within a Geographical Information System environment (GIS). The application of the RUSLE model in different natural environments and on every scale takes into account five key factors namely: the rainfall erosivity, the soil erodi-bility, the steepness and length of slopes, the vegetation cover and the conservation support practices. Each of these factors was generated in GIS as a raster layer, their combination, resulted in the development of a soil loss map indicating an average erosion rate of 7.8 tꞏha{\textendash}1ꞏy{\textendash}1. The obtained soil loss map was classified into four ero-sion severity classes; low, moderate, high and very high severity representing respectively 40, 30.48, 22.59 and 6.89\% of the total surface. The areas, showing moderate, high and very high erosion rates which represent more than half of the basin area were found generally located in regions having high erodibility soils, steep slopes and low vegetation cover. These areas should be considered as priorities in future erosion control programs in order to decrease the siltation rate in the Cheffia reservoir. },
	url = {http://www.itp.edu.pl/wydawnictwo/journal/36_2018_I_III/Bouhadeb.pdf},
	author = {BOUHADEB and MENANI Mohamed redha and BOUGUERRA H and DERDOUS O}
}
@article {1891,
	title = {The contribution of fracturations in the emergence of the thermal springs in Setif city, Eastern Algeria, Carbonates Evaporites},
	journal = {Springer},
	year = {2017},
	abstract = {Setif city covers an area of 6550\&nbsp;km2; it is located about 300\&nbsp;km southeast of Algiers and 100\&nbsp;km to the south of the Mediterranean sea. The aim of our study is to know the tectonic mechanisms responsible for the emergencies and to highlight their chemical characteristics of water springs in Setif. Wherein thermalism is characterized by the presence of a number of thermal springs, the latest are usually related to recent large fractures deeply affecting the sedimentary formations and sometimes even crystallin basement. These fractures are often injected by Triassic evaporates; their directions are NNW{\textendash}SSE, NW{\textendash}SE, and NE{\textendash}SW and limiting great structural units. Four groundwater facies were identified: the high percentage of sources, staking major accidents related to limestone mountains or to the basement, shows a calcium or sodium sulfate facies; and the sources are often hot (meso or hyperthermal). A second group, related to terrigenous saliferous formations, shows a sodium bicarbonate or sodium chloride facies. The geothermic interpretation allows us to conclude that the reservoir supplies the two aquifer systems of the thermal complex, and is stored in fissured Jurassic limestone, where water storage and circulation is beyond 2600\&nbsp;m deep.},
	url = {https://www.researchgate.net/publication/318603314_The_contribution_of_fracturations_in_the_emergence_of_the_thermal_springs_in_Setif_city_Eastern_Algeria},
	author = {DJEMMAL S and MENANI Mohamed redha and CHAMEKH K and BAALI F}
}
@article {1890,
	title = {Assessment of the water needs of apricot and olive crops under arid climatic conditions: case study of Tinibaouine Region (northeast of Algeria), Special Issue on Science, Engineering \&amp; Environment, ISSN: 2186-2990, Japan. Feb,2017},
	journal = {International Journal of GEOMATE},
	volume = { Vol. 12},
	number = {Issue 30},
	year = {2017},
	pages = {pp. 46 - 52. },
	abstract = {The Tinibaouine region, located in north-eastern Algeria on the borders of the Batna-Belezma Mountains, is characterized by a semi-arid to arid climate with an average annual rainfall not exceeding 465 mm and an average annual temperature of around 22 {\textdegree} C. This region is characterized by the cultivation of apricots as essential crop followed by that of olives, whose plots are all irrigated with the Tinibaouine spring water. These are 450 Ha of trees for apricot and 108 Hectare for olives which constitute the principal revenue of the citizens of this small village. This paper estimated the crop reference and actual evapotranspiration (ETO) respectively and the irrigation water requirement of apricot trees and olive trees. The long recorded climatic data, crop and soil data, effective water allocation and planning, the information about crop water requirements, irrigation withdrawals were computed with the Cropwat model which is based on the United Nations{\textquoteright} Food and Agriculture Organization (FAO), the Penman-Monteith method was used to estimate ETo. Crop coefficients (Kc) from the phenomenological stages of apricot and olive were applied to adjust and estimate the actual evapotranspiration ETc through a water balance of the irrigation water requirements (IR). The results showed that the annual reference evapotranspiration (ETO) was estimated at 3.71mm / day. The irrigation requirements were estimated at 35800 m3/ hectare for apricot, 6980 m3/ hectare for olive, also Irrigation needs estimated on land at 14185, 05 m3/ hectare for olive and apricot},
	url = {https://www.geomatejournal.com/sites/default/files/articles/46-52-160424-Zineb-Feb-2017.pdf},
	author = {Mensouri Z and MENANI Mohamed redha}
}
