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The Ourika sub-watershed is composed of about twenty different watersheds with diverse lithology, slope, and structural organization. In order to better characterize the basin, we inventoried and extensively assessed the different types of thresholds implemented in each micro-watershed. The present study focused on the area located between Meltsen and Sidi Ali Oufarés faults, which includes several micro-watersheds that have been modified by the installation of structures. We selected 12 micro-watersheds from the main tributaries draining this zone, based on the level of risk: four micro-watersheds on the right bank from upstream to downstream (Wigrane and Walighane, Tachmacht, and Touggalkhir), and eight micro-watersheds on the left bank from upstream to downstream (Imintaddarte, Oussane, Tikhfert, Tighazrit, Igri Foudene, Asni, Taljarft, and Tarzaza). The results of our study allowed us to detect and inventory 545 erosion protection structures made of masonry, gabions, and dry stone. However, the majority of these structures were damaged in several micro-watersheds due to steep slopes, torrential rainfall, and especially the solid sediment load resulting from the erosion of easily erodible old alluvial cones. This study serves as a warning to various stakeholders and decision-makers to ensure proper management in this mountainous system. The distribution of these thresholds is as follows: 62 masonry thresholds, accounting for 13.37%; 247 gabion thresholds, accounting for 45.32%; and 236 dry stone thresholds, accounting for 43.30%. The assessment of these structures revealed anomalies such as the loss of 17.43% of embankment structures and the destruction of certain thresholds.
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Tom
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171--185
Opis fizyczny
Bibliogr. 24 poz., rys., tab.
Twórcy
autor
- Labo2GRNT, Geological Department, Faculty of Science Semlalia, Cadi Ayyad University, BP 2390, 40 000, Marrakech, Morocco
autor
- Labo2GRNT, Geological Department, Faculty of Science Semlalia, Cadi Ayyad University, BP 2390, 40 000, Marrakech, Morocco
- algouti@uca.ac.ma
autor
- Labo2GRNT, Geological Department, Faculty of Science Semlalia, Cadi Ayyad University, BP 2390, 40 000, Marrakech, Morocco
autor
- Labo2GRNT, Geological Department, Faculty of Science Semlalia, Cadi Ayyad University, BP 2390, 40 000, Marrakech, Morocco
Bibliografia
- 1. Affo Biao Kokou A. 2015. Contribution à l’étude phytoécologique et à l’évaluation de la qualité des écosystèmes ripisylves du bassin versant de l’Ourika (haut-atlas) (Mémoire de 3ème cycle). Ecole Nationale Forestière d’Ingénieurs, Salé. 99.
- 2. Bochet E., Poesen J., Rubio L. 2000. Mound development as an interaction of individual plants with soil, water erosion and sedimentation processes on slopes. Earth Surface Processes and Landforms, 25, 847–867.
- 3. Beuselinck L., Steegen A., Govers G., Nachtergaele J., Takken I., Poesen J. 2000. Characteristics of sediment deposits formed by intense rainfall events in small catchments in the Belgian Loam Belt. Geomorphology, 32, 69–82.
- 4. Combes F., Hurand A., Meunier M. 1995. The mountain forest: a flood remedy, in: Research report no. 3, BVRE by Draix, Cemagref Éditions, Grenoble,113–121.
- 5. Doukkali O. 2003. Evaluation of the longevity and performance of water and soil conservation techniques in the Ourika- DREF watershed of the High Atlas Morocco. 3rd cycle thesis ENFI, Salé, Morocco, 113.
- 6. El Alaoui el Fels A., Saidi M., Errachidi S. 2003. Flood frequency analysis and generation of flood hazard indicator maps in a semi-arid environment, case of Ourika watershed (western High Atlas, Morocco).
- 7. GTZ. 1998. Causes of soil degradation and approaches for promoting a sustainable land use, edit, Markgraf Verlag, Germany, 98.
- 8. Ilmen R. 2004. Contribution to the study of recreational use of the Ourika Valley with a view to its development. (Thesis of the 3° cycle of the National Forestry School of Engineers of Salé). ENFI, Salé (Morocco), 133.
- 9. Moir W.H., Ludwig J.A., Scholes R.T. 2000. Soil erosion and vegetation in grasslands of the Peloncillo Mountains, New Mexico. Soil Science Society of America Journal, 64.
- 10. Moret L. 1931. Geological research in the Atlas of Marrakech. Note and Mr. Serv. Mines and geol map. Morocco, 18, 262.
- 11. Namous M. 2012. Quaternary Evolution And Current Dynamics Of A Geomorphological System Of Active Chain Front: The Example Of The Ourika Watershed (Morocco). Thesis. Faculty of Sciences Semlalia Marrakech, Morocco.
- 12. O’Loughlin C., Xinbao Z. 1986. The influence of fast-growing conifer plantations on shallow landsliding and earthflow movement in New Zealand steeplands. 18th IUFRO World Congress, Ljubljana (Yugoslavia), IUFRO.
- 13. Sabir M., Roose E., Merzouk A., Nouri A. 1999. Traditional management techniques water and anticorrosive control in two terroirs of the western Rif, Morocco, ORSTO Bulletin, Rome, Italy, 139–147.
- 14. Saidi M., Daoudi L., Aresmouk M.E., Fniguire F., Foukrim S. 2010. The floods of the oued Ourika (High Atlas, Morocco): Extreme events in a semiarid mountain context. Comunicações Geológicas, t. 97, Lisbon, 113–128.
- 15. Saidi M.E. 1994. Genesis and spread of floods in a sub-arid environment: Example of the oued Souss (Morocco). Bulletin of the Association of French Geographers, 1, 94–111, Paris.
- 16. Ouhammou A. 1991. Overview on the staging of the vegetation of the Ourika basin (High Atlas of Marrakech, Morocco). Monthly bulletin of the Linnean Society of Lyon 60, 401–405. https://doi.org/10.3406/linly.1991-14131
- 17. Proust F. 1961. Stratigraphic, petrographic and structural study of the Block Oriental of the Ancient Massif of the High Atlas (Morocco).thesis, Montpellier, France, 272.
- 18. Proust F. 1973. Stratigraphic, petrographic and structural study of the Eastern Block of the Ancient High Atlas Massif. Morocco. Memo Note. Serv. Geol. Morocco, 254, 15–53.
- 19. Proust F., Petit J.P., Tapponnier P. 1977. The Tizi n’test accident and the role of stalling in the tectonics of the Western High Atlas (Morocco). Bulletin of the Geological Society of France 7, 541–551.
- 20. Van-Dijk P.M., Kwaad F.J.P.M., Klapwijk M. 1996. Retention of water and sediment by grass strips. Hydrological Processes, 10, 1069–1080.
- 21. Villard N., Schmitt M., Tacnet J.M. 2014. Torrential correction: design & feedback on an innovative cable dam. National Days of Geotechnics and Geology of the Engineer JNGG 2014 Ŕ Beauvais July 8–10.
- 22. Viles H.A. 1990. The agency of organic beings: a selective review of recent work in biogeomorphology. In Vegetation and erosion: processes and environments. Ed. J.B. Thornes. Chichester, John Wiley & Sons Ltd, 5–24.
- 23. Rey F. 2001. influence of the spatial distribution of vegetation on the sedimentary production of marl gullies in the Southern Alps. Doctoral thesis. Joseph Fournier University, Grenoble I. France, 183.
- 24. Mathys N. 2003. Erosion quantification in the small marly experimental catchments of Draix (Alpes de Haute Provence, France). Calibration of the ETC rainfall–runoff–erosion model, 01. https://doi.org/10.1016/S03418162(02)00122-4
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Bibliografia
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