Turbidity-Hysteretic Response in River Ose, Ondo State, Nigeria
June 24, 2023
June 23, 2023
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Concentration-Discharge relationships are a key tool for understanding the sources and transport of material from watersheds to fluvial networks. Turbidity based estimating of suspended sediment concentration is widely used for river studies due to its simply and cheap using. The relation between suspended sediment concentration (turbidity) and discharge is not normally homogenous and often producing hysteretic loop. Therefore, this work identified the hysteresis types of the turbidity-discharge relationships in river Ose. Data were collected at coordinates 7⁰ 18’ 35.5” N and 5⁰ 39’ 52.5” E for two-year period and analysis showed that counter-clockwise hysteresis loop pattern was dominant. This suggested that overland flow is much possible in the study area.
A. S., D. (2023). Turbidity-Hysteretic Response in River Ose, Ondo State, Nigeria. Engineering And Technology Journal, 8(6), 2350–2359. https://doi.org/10.47191/etj/v8i6.09
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13. Steegen, A., Govers, G., Nachtergaele, J., Takken, I., Beuselinck L., Poesen, J. (2000). Sediment export by waterfrom an agricultural catchment in the Loam Belt of Central Belgium. Geomorphology, 33:25-36.
14. Wood, P. (1977). Controls of variation in suspended sediment concentration in the River Rother, West Sussex,England. Sedimentogy, 24: 437-445.
2. Baca, P,. 2002. Temporal variability of suspended sediment availability during rainfall-runoff events in a small agricultural basin. ERB and Northern European FRIEND Project 5 Conference, Demanovska dolina, Slovakia.
3. DiCenzo, P. D., Luk, S. (1997). Gully erosion and sediment transport in a small subtropical catchment,Catena, 29: 161-176.
4. Doty, C. W., Carter, C. E. (1965). Rates and particles-size distribution of soil erosion from unit source areas. Trans. Am. Soc. Agric. Engrs., 8: 309-311.
5. Fellman, J. B., Hood, E., Edwards, R. T., and D’Amore, D. V. (2009). Changes in the concentration, biodegradability, and fluorescent properties of dissoved organic matter during stormflows in coastal temperate watersheds. J. Geophys. Res. Biogeo. 114:G01021. doi: 10.1029/2008JG000790
6. Inamdar, S. P., O’ Leary, N., Mitchell, M. J,. and Riley, J. T. (2006). The impact of storm events on solute exports from a glaciated forested watershed in western New York, USA. Hydrol process. 20, 3423-3439. Doi: 10.1002/hyp.6141
7. Klein, M. (1984). Anticlockwise hysteresis in suspended concentration during individual storms: Holbeck catchment, Yorkshire, England. Catena 11, pp 251-257.
8. Lefrancois, J., Grimaldi, C., Gascuel-ODoux, C., Gilliet, N. (2007). Suspended sediment and discharge relationships to identify bank degradation as a main source on small agricultural catchments. Hydrol. Process., 21:2923-2933.
9. Martin, S.E., Conklin, M.H., Bales, R.C. (2014). Seasonal Accumulation and Depletion of Local Sediment Stores of Four Headwater Catchments. Journal Water 6,2144-2163; doi: 10.3390/w607244
10. Rodrigueez-Blanco, M, L., Taboada-Castro, M. T., Oropeza Mota, J. L. Suspended sediment-discharge during rainfall events in a small headwater catchment in the NW Spain. Part of research of REN2003-08143 project PGIDIT05RAG10303PR, funded respectively by the Spanish Ministry of Education and Science (MEC) and the Xunta of Galicia.
11. Slattery, M. C., Gares, P. A., Philips, J. D. (2002). Slope-channel linkage and sediment delivery on North Carolin Coastal Plain cropland. Earth Surf. Process. Landforms, 27: 1377-1387
12. Soler, M., Latron, G., Gallart, F. (2008). Relationships between suspendend sediment concentrations and discharge in two small research basins in mountainous Mediterranean area (Vallcebre, Eastern Pyrenees). Geomorphology 98, 143-152.
13. Steegen, A., Govers, G., Nachtergaele, J., Takken, I., Beuselinck L., Poesen, J. (2000). Sediment export by waterfrom an agricultural catchment in the Loam Belt of Central Belgium. Geomorphology, 33:25-36.
14. Wood, P. (1977). Controls of variation in suspended sediment concentration in the River Rother, West Sussex,England. Sedimentogy, 24: 437-445.
