A FLOW DEFICIT, EVAPOTRANSPIRATION AND INFILTRATION IN ARID AREAS: THE CASE OF SOUTHERN TELLIAN ATLAS SUB-BASINS, EASTERN ALGERIA
DOI:
https://doi.org/10.4314/jfas.v13i1.29Keywords:
Flow deficit; Evapotranspiration; Geology; Hodna; Infiltration; Sub-basin.Abstract
Knowledge of inputs into an aquifer environment still remains a task difficult to identify for a groundwater model implementing software to simulate scenarios over long periods. Due to several related factors such rain and flow regimes, and the geology and morphometry of hydrological units, the water entering in the system is a random parameter. The objective of this study is to assess the flow deficit and the recharge rate in the North of Hodna region. The hydrometric stations network managed by the Agence Nationale des Ressources Hydrauliques (ANRH), sometimes within the same watercourse, presents sufficient series to make comparisons between the flow deficits. Thus, starting from there, taking into account the sub-basins geology, we dissociated the evapotranspiration portion of water input from the infiltration. This method showed an 8% of recharge and 82% of deficit.
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References
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[2] Allen R G, Pereira L S, Raes D, Smith M, Crop evapotranspiration - Guidelines for computing crop water requirements - FAO Irrigation and drainage paper, Rome, 1998, 56 pages
[3] Amroune A. Hydrogéologie et qualité des eaux souterraines de la plaine de M’Sila, Mémoire de Magister, Université de Batna, (Algérie), 2008,133 pages
[4] Benabderrahmane A. Simulation numerique de la pollution saline d’un système aquifère dans une région semi-aride à aride, example des systèmes aquifères de la plaine de M’Sila (Hodna, Algérie). Thèse de Doctorat, Université de Franche Comté, France, 1988, 185 pages
[5] Bladini P. Couverture géologique de Tarmount avec note explicative. ANRH, Alger, Algérie, 1966, 32 pages
[6] Berengena J, Gavilan P. Reference ET estimation in a highly advective semiarid environment. J. Irrig. Drain. Eng. ASCE, 2005, 131 (2)
[7] Coutagne A. Communication presented at the 68th Congress of Learned Societies, the flow deficit and evaporation in the Lyon region, 1935, Lyon, France
[8] Delin G N, Healy R W, Lorenz D L, Nimmo J R. Comparison of local- to regional-scale estimates of groundwater recharge in Minnesota USA J Hydrol., 2007, 334: 231–249
[9] DRE M’Sila. Inventaire des forages. Direction des Resources Hydrauliques de la wilaya de M’Sila, 2011, 20 pages.
[10] Drexler J Z, Snyder R L, Spano D, Paw K T. A review of models and micrometeorological methods used to estimate wetland evapotranspiration. Hydrol. Proc., 2005, 18: 2071–2101
[11] Gavilan P, J. Berengena, R. G Allen. measuring versus estimating net radiation and soil heat flux: impact on Penman–Monteith reference ET estimates in semiarid regions. Agric. Water Manage., 2007, 89: 275 - 286.
[12] Grine R. Annuaire piézometrique, ANRH, Alger, Algérie, 2007, 18 pages
[13] Grisoni M, Ducroux J. Course in surface hydrology, Ed. Environmental studies and hydraulic research department, Hydrology department. 1972, 285 pages.
[14] Guiraud R. Couverture géologique de Souk Ouled Nadja avec note explicative, ANRH. 1971, 30 pages
[15] Healy R W. Estimating groundwater recharge. Cambridge University Press. 2010, Cambridge
[16] Jensen M E, Burman R D, Allen R G. Evapotranspiration and irrigation water requirements. In: ASCE Manual no. 70, ASCE, New York, 1990.
[17] Kieken G. Couverture géeologique avec de Maginot avec note explicative. ANRH, 1948. 28 p.
[18] Lenka S, Singh A K, Lenka N K, Water and nitrogen interaction on soil profile water extraction and ET in maize–wheat cropping system. Agric. Water Manag., 2009, 96: pp. 195–205.
[19] ANRH, Séries pluviales des postes Sidi Aissa, Ain Nessissa et Rocade Sud. Agence Nationale des Ressources Hydrauliques., 2012. Alger, Algérie, 23 pages
[20] ANRH. Apports des stations hydrometriques de Ced Faguès, Nessissa et Rocade Sud. Agence Nationale des Ressources Hydrauliques, Alger, Algérie., 2012, 28 pages
[21] Phillips F M, Hogan J F, Scanlon B.R. Introduction and overview. In: Hogan JF, Phillips FM, Scanlon BR (eds) Groundwater recharge in a desert environment. AGU, Washington, DC., 2004. pp 1–14
[22] Remenieras G, Hydrologie de l’ingénieur. Ed. Eyrolles., 1986. 451 pages
[23] Scanlon B R, Healy R W, Cook P G, choosing appropriate techniques for quantifying groundwater recharge. Hydrogeol J., 2002, 10: pp. 18–39
[24] Sharma M L, In: Hillel, D. (Ed.), Estimating Evapotranspiration, Advances in Irrigation, vol. 3. Academic, New York., 1985, pp. 213–281
[25] Subrahmanyam V P, The Water Balance of India According to Thornthwaite's Concept of Potential Evapotranspiration. Annals of the Association of American Geographers., 1956, 46(3): pp. 300-311
[26] Thornthwaite C W, Mather J R. The Water Balance, Climatology, vol.8, no.l. C.W. Thornthwaite & Associates, Centerton, New Jersey., 1955.
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Published
2020-10-13
How to Cite
AMROUNE, A.; GRINE, R.; GUASTALDI, E. A FLOW DEFICIT, EVAPOTRANSPIRATION AND INFILTRATION IN ARID AREAS: THE CASE OF SOUTHERN TELLIAN ATLAS SUB-BASINS, EASTERN ALGERIA. Journal of Fundamental and Applied Sciences, [S. l.], v. 13, n. 1, p. 533–546, 2020. DOI: 10.4314/jfas.v13i1.29. Disponível em: https://jfas.info/index.php/JFAS/article/view/894. Acesso em: 30 jan. 2025.
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