ANALYSIS OF THE FLOW-SUSPENDED MATERIAL RELATIONSHIP DURING THE FLOODS IN THE OUED ISSER WATERSHED.
Keywords:
suspended sediment concentration, liquid flow, sediment flow, flood, hysteresis, wadi IsserAbstract
This work focuses on the study of the relationship between suspended sediment concentration C and liquid flow Q during floods, on one hand, and the quantification of sedimentary flow in the watershed of the Isser wadi, on the other hand. The analysis of 84 floods over a 30-years period (1971/2001) shows a seasonal dynamic of suspended sediment availability, which increases in summer (especially in August) and autumn and decreases in winter and spring when flow is high. An analysis of the events recorded on the Isser wadi is made from the appearance of the graphs representing C as a function of Q which draws four hysteresis models hourly, counterclockwise, linear plus loop and figure in eight. The total flood performance in terms of suspended solid transport is 5.07* 106 tonnes, which corresponds to a specific degradation of 1222 t.km-2.year-1. Suspended solid flux varies considerably from one flood to another depending on many factors such as seasonality and flood duration, and hourly and counterclockwise floods are the most frequent and produce 70% of total sediments. The analysis of seasonal yields has shown that winter contributes a great deal of sediment (49%).
References
Achite, M. Meddi, M. 2004. Estimation du transport solide dans le bassin versant de l’Oued Haddad (Nord-Ouest Algérien). Sécheresse, 15 (4), 367–373.
Achite, M., Ouillon, S., 2007. Suspended sediment transport in a semiarid watershed, Wadi Abd, Algeria (1973–1995). J. Hydrol. 343, 187–202.
Asselman, N.E.M., 1999. Suspended sediment dynamics in a large drainage basin: the River Rhine. Hydrol. Proc. 13, 1437–1450.
Baca, P., 2008. Hysteresis effect in suspended sediment concentration in the Rybárik basin, Slovakia. Hydrol. Sci. J. 53 (1), 224–235.
Battala, R. J. & Sala, M. 19 92 - Temporal variability of su spended sediment in a Mediterranean River, International Conference Canberra Australia, Interna tional Association of Hydrologi cal Sciences Publication 224, 229 -305.
Benkhaled, A., Remini, B., 2003a. Variabilité temporelle de la concentration en sédiments et phénomène d’hystérésis dans le bassin de l’Oued Wahrane (Algérie). J. Sci. Hydrol. 48 (2), 243–255.
Benkhaled, A., Remini, B., 2003b. Analyse de la relation de puissance: débit solide – débit liquide à l’échelle du bassin versant de l’Oued Wahrane (Algérie). Rev. Sci. Eau 16 (3), 333–356 .
Bouanani, A., 2004. Hydrologie, transport solide et modélisation. Etude de quelques sous bassins de la Tafna (NW–Algérie). Ph.D. Thesis, Tlemcen University, Algeria, 250p.
Bourouba, M., 1997. Les variations de la turbidité et leurs relations avec les précipitations et les débits des oueds semi-arides de l ’Algérie orientale. Bulletin de l’ORSTOM, 17, 345–360.
Elmahi, A., Meddi, M., & Bravard, J.P. 20 12 - Analyse du transport solide en suspension dans le bassin de l’oued el- Hammam (Algérie Nord). Hydrological Sciences Journal Volume 57, Issue 8 pp. 1642 -1661.
Ghenim, A., Seddini, A., Terfous, A., 2008. Variation temporelle de la dégradation spécifique du bassin versant de l’Oued Mouilah (nord-ouest Algérien). Hydrol. Sci. J. 53 (2), 448–456 .
Ghenim, A., Terfous, A., Seddini, A., 2007. Etude du transport solide en suspension dans les régions semi-arides méditerranéennes: cas du bassin versant de l’oued Sebdou (nord-ouest algérien). Sécheresse 18 (1), 39–44 .
Ghorbal, A., Claude, J., 1977 . Mesure de l’envasement dans les retenues de sept barrages en Tunisie: estimation des transports solides, vol. 122. IAHS Publication, pp. 219–232.
Heidel, S.G., 1956. The progressive lag of sediment concentration with flood waves. Trans. Am. Geophys. Union 37, 56–66 .
Hudson, P.F., 2003. Event sequence and sediment exhaustion in the lower Panuco basin, Mexico. Catena 52, 57–76 .
Jansson, M.B., 2002. Determining sediment source areas in a tropical river basin, Costa Rica. Catena 47, 63–84 .
Kassoul, M., Abdelgader, A., Belorgey, M., 1997. Caractérisation de la sédimentation des barrages en Algérie. Rev. Sci. Eau 3, 339–358 .
Khanchoul, K., Jansson, M.-B., 2008. Sediment rating curves developed on stage and seasonal means in discharge classes for the Mellah Wadi, Algeria. Geogr. Ann. 90A (3), 227–236 .
Klein, M., 1984. Anti clockwise hysteresis in suspended sediment concentration during individual storms: Holbeck catchment; Yorkshire, England. Catena 11, 251–257.
Lefrancois, J. Grimaldi, C. Gascuel, O. Gilliet, N. 200 3. Origins end dynamic sediment in small agricultural catchement. The Fourth In ter- Celtic colloquium on Hydrology, Guimares P ortu gal. July 11 -14, 1 -13.
Lefrançois, J., Grimaldi, C., Gascuel-Odoux, C. & Gilliet, N. (2007) Suspended sediment and discharge relationships to identify bank degradation as a main sediment source on small agricultural catchments. Hydrol. Processes 21, 2923–2933
Lenzi, M. A. & Marchi, L. (2000) Suspended sediment load during floods in a small stream of the Dolomites (northeastern Italy). Catena 39, 267–282.
Megnounif, A. Terfous, A. Ghenaim, A. Poulet, J.B., 2007. Key processes influencing erosion and sediment transport in a semi-arid Mediterranean area: the upper Tafna catchment, Algeria. Hydrol. Sci. J. 52 (6), 1271–1284.
Megnounif, A., Terfous, A. Ouillon, S. 2013. A Graphical method to study suspended sediment dynamics during flood events in the Wadi Sebdou. N.W (Algeria) (197 3 -2004). Journal of hydrology 497, 24 -36.
Picouet, C., Hingray, B., Olivry, J.C., 2001. Empirical and conceptual modelling of the suspended sediment dynamics in a large tropical African river: the upper Niger river basin. J. Hydrol. 250, 19–39.
Roose, E., Arabi, M., Chebbani, M., Mazour, M., Morsli, B., 1998. Les montagnes méditerranéennes d’Algérie. Impact de l’intensification de l’agriculture de montagne sur l’environnement et les revenues. ORSTOM Actualité Spécial Erosion 56, 26–27.
Seeger, M., Errea, M. P., Begueria, S., Arnaez, J., Marti, C. & Garcia-Ruiz, J. M. (2004) Catchment soil moisture and rainfall characteristics as determinant factors for discharge/suspended sediment hysteretic loops in a small headwater catchment in the Spanish Pyrenees. J. Hydrol. 288, 299–311.
Terfous, A., Megnounif, A., Bouanani, A., 2001. Study of the suspended load at the river Mouilah (north west Algeria). Rev. Sci. Eau 14 (2), 173–185.
Walling, D.E., Webb, B.W., 1981. The reliability of suspended load data. Erosion and Sediment Transport Measurement, vol. 133. IAHS Publication, pp. 177–194.
Walling, D.E., Webb, B.W., 1982. Sediment Availability and Prediction of Stormperiod Sediment Yields, vol. 13. IAHS Publication, pp. 327–337.
Williams, G.P., 1989. Sediment concentration versus water discharge during single hydrologic events in rivers. J. Hydrol. 111, 89–106.