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Sustainability of a hydraulic facility and flood risk of its downstream section: the case of the Foum El-Gherza dam (Ziban east, Algeria)

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Due to advanced silting, the Foum El-Gherza dam has lost more than two thirds of its initial capacity (47 hm3) and is no longer able to withstand the floods that threaten its downstream section. Indeed, the damage recorded in recent years has confirmed the vulnerability of the man-made structures located on both banks of the Oued Labiod. Thus, we believe that the hydrological behaviour of the catchment area is no longer influenced by the dam. Therefore, the hydrological study involved a critical analysis (homogeneity tests) of the hydro-climatic data in order to highlight the characteristics of the historical events recorded during the period 1950–2019. The frequency study of the maximum daily rainfall and floods recorded at the dam allowed us to determine the rainfall and flow rates of the return periods (10, 25, 50, 100, 500 and 1000 years). The flooding of the 28 October 2011 were used as a standard for the calibration of the model calculated by the HEC-Ras software. After validation of the model, a prediction of the water levels and flood extent was made for the selected return periods. The results obtained show that a part of the town of Seryana (district located on the edge of the right bank) suffers from flooding proportionally to the return periods of the floods. In addition, some agricultural areas bordering the Oued are also affected by the floodings. The hazard modelling maps can be considered as a basis for a flood risk prevention plan (PPRI) and as a decision support tool.
Rocznik
Tom
Strony
7--22
Opis fizyczny
Bibliogr. 29 poz., rys., tab.
Twórcy
autor
  • Laboratory of Territorial Sciences, Natural Resources and Environment ‘Lasterne’ Department of Spatial Planning Faculty of Earth Sciences, Geography and Spatial Planning University of Constantine 1, Algeria
  • Laboratory of Territorial Sciences, Natural Resources and Environment ‘Lasterne’ Department of Spatial Planning Faculty of Earth Sciences, Geography and Spatial Planning University of Constantine 1, Algeria
  • Laboratory of Natural Risks and Territorial Planning ‘Lrnat’ Institute of Earth and Universe Sciences University of Batna-2, Algeria
Bibliografia
  • Abbas S.A., Al-Aboodi A.H., Ibrahim H.T. 2020. Identification of Manning’s coefficient using HEC-RAS model: upstream Al-Amarah barrage. Journal of Engineering.
  • Aidaoui S. 1994. Ressource en eau et aménagement hydro-agricole dans la région de Biskra Ziban [Algérie].
  • Amrani K., Abdelhakim S. 2023. Évaluation de la Durabilité des Agro-systèmes Oasiens dans le Sahara Septentrional Algérien et réflexions autour de la conception d’une grille d’évaluation évolutive. HAL open science. hal-03934310
  • Army Corps of Engineers, U.S. 1997. HEC-RAS River Analysis System: Hydraulic Reference Manual Version 5.0.
  • Benkhaled A., Rezgui Z., Sakhraoui F. 2013. Floods in Abiod Wadi: analysis of database. LARHYSS Journal P-ISSN 1112-3680/E-ISSN 2521-9782 14.
  • Boudjerda M., Touaibia B., Mihoubi M.K., Basson G.R., Vonkeman J.K. 2022. Application of sediment management strategies to improve reservoir operation: a case study Foum El- Gherza Dam in Algeria. International Journal of Environmental Science and Technology, 19, 11, 10957–10972.
  • Brinis N., Brahmia A., Hamel A., Benhamida S. 2021. Origine et dynamique des ions controlant la mineralisation des eaux des sources dans la partie amont de la vallee de L’oued Labiod, Batna, Algerie. Regions: Ichemoul, Arris, T’kout et Ghassira. LHB, 107, 1, 1–10.
  • Chebbah M. 2007. Lithostratigraphie, Sédimentologie et modèles les de Bassins des dépôts néogènes de la région de Biskra, de part et d’autre de l’accident Sud Atlasique (Ziban, Algérie). Mentouri University-Constantine.
  • Chebbah M. 2016. A Miocene-restricted platform of the Zibane zone (Saharan Atlas, Algeria), depositional sequences and paleogeographic reconstruction. Arabian Journal of Geosciences, 9, 2, 151.
  • Cote M. 1991. Biskra. Encyclopédie berbère, 10, 1517–1522.
  • Ghachi M.E.G.E., Ouakhir H.O. 2019. Dynamique fluviale dans l’oued El Abid: Suivi et quantification d’un tronçon fluvial à l’amont du barrage de Bin El Ouidane 2016/2017 (Haut Atlas Central/Maroc). Revue Marocaine de Géomorphologie, 3.
  • Guiraud R. 1973. Evolution post-triasique de l’avant-pays de la chaîne alpine en Algérie.
  • Guiraud R. 1990. Evolution post-triasique de l’avant-pays de la chaîne alpine en Algérie: d’après l’étude du Bassin du Hodna et des régions voisines. Office National de la Géologie.
  • Hachemi A. 2017. Contribution à l’étude des crues de oued Abiod (Biskra). http://thesis.univbiskra.dz/4390/1/Th%C3%A8se_A.H.pdf
  • Hamamouche M.F., Kuper M., Riaux J., Leduc C. 2017. Conjunctive use of surface and ground water resources in a community-managed irrigation system. The case of the Sidi Okba palm grove in the Algerian Sahara. Agricultural Water Management, 193, 116–130.
  • Huţanu E., Mihu-Pintilie A., Urzica A., Paveluc L.E., Stoleriu C.C., Grozavu A. 2020. Using 1D HEC-RAS modeling and LiDAR data to improve flood hazard maps accuracy: A case study from Jijia Floodplain (NE Romania). Water, 12, 6, 1624.
  • Khomri Z., Chabaca M.N., Boudibi S., Menadi S., Kharfallah N. 2022. Spatial simulation of groundwater recharge in an arid region (Biskra, SE Algeria). Euro-Mediterranean Journal for Environmental Integration, 7, 1, 103–117.
  • Michalec B. 2022. Determination of the silting rate of thuringian dam reservoirs on the example of Dachwig and Ohra reservoirs. Geomatics, Landmanagement and Landscape, 1.
  • Mohamed J., Ali D.A., Warsame A.A., Adam M.B. 2022. Two phases of long-term shift in extreme precipitation in Somalia. Meteorology and Atmospheric Physics, 134, 3, 54.
  • Nguimalet C.R. 2021. Evolution des crues en sècheresse hydrologique dans le centre centrafricain.
  • Noui A., Guesbaya Z. 2022. Modélisation Numérique de l’Equilibre Hydrogéologique Application à la nappe Mio-pliocène de Biskra. Communication science et technologie, 11, 2, 57–62.
  • Ouamane A., Sekkour I., Athmani B. 2022. Mobilisation des eaux de surface: Commentaires généraux sur les barrages en Algérie dans le passé, le présent et le futur. Agua y Territorio / Water and Landscape 20, e5298–e5298.
  • Pathan A.I., Agnihotri P.G. 2021. Application of new HEC-RAS version 5 for 1D hydrodynamic flood modeling with special reference through geospatial techniques: a case of River Purna at Navsari, Gujarat, India. Modeling Earth Systems and Environment, 7, 1133–1144.
  • Phiri D., Simwanda M., Salekin S., Nyirenda V.R., Murayama Y., Ranagalage M. 2020. Sentinel-2 data for land cover/use mapping: a review. Remote Sensing, 12, 14, 2291.
  • Puno G.R., Amper R.A.L., Opiso E.M., Cipriano J.A.B. 2020. Mapping and analysis of flood scenarios using numerical models and GIS techniques. Spatial Information Research, 28, 2, 215–226.
  • Rechachi Miled Zohra. 2019. Evaluation et modélisation géochimiques de la qualité des eaux souterraines utilisées pour l’irrigation des terres agricoles dans une zone aride: cas de la région de sidi okba geochemical evaluation and modelling of the quality of groundwater used for irrigation in arid area: sidi okba a case study.
  • Remini B., Maazouz M. 2018. The density current in the Foum El Gherza dam (Algeria). LARHYSS Journal P-ISSN 1112-3680/E-ISSN 2521-9782 35, 87–105.
  • Soualmia A., Gharbi M. 2014. Tests de simulations des crues éclair. Lebanese Science Journal, 15, 2, 13.
  • Souanef N. 2015. Analyse fréquentielle des débits max de crues de L’Oued Abiod.
Uwagi
Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-e82c6713-b9ec-45a7-96c3-0def8c0ac39b
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