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Modelling of Sediment Transport Capacities of Ogbese and Owena Rivers in S.W. Nigeria

机译:S.W中ogbese和Ogena Rivers沉积物运输能力的建模。尼日利亚

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The movement of sediment such as sand, silt or gravel by flowing water is of interest to a wide range of engineering disciplines. This study is aimed at developing models, which can be used to predict the magnitude and levels of sediment concentration in Ogbese and Owena Rivers in Ondo State S.W. Nigeria for engineering design purposes. Data were collected from field investigations conducted at the respective sampling stations on the two rivers. The live bed concept used was derived from Liu - Hwang (1954) resistance equations and that of Einstein-Brown (1981) sediment transport concept. The problem was reduced to that of a power law relationship. These data ere fitted into the power relationship to obtain the predicted model of the form: F~1Q = k_Φ~(k1), where the parameters F~1Q is the dimensionless sediment discharge, Φ is the dimensionless bed shear stress, k_1 and k_2 are sediments transport coefficients. Calibrating the models yielded the values of k_1 and k_2 for Ogbese river as 0.592 and 0.865 and for Owena river as 0.335 and 1.197 respectively. When tested the predicted models for Ogbese and Owena rivers performed well in comparison with the established models such as Ackers and White (1973), Engleund and Hansen (1967), Yang (1973) and Karim (1998). It is concluded that the models developed would be useful for engineering design purposes for Ogbese and Owena rivers.
机译:通过流动水的沙子,淤泥或砾石等沉积物的运动对广泛的工程学科感兴趣。本研究旨在开发模型,可用于预测ONDO州S.W的OGBESE和OWENA RIVERS中沉积物浓度的大小和水平。尼日利亚工程设计目的。从两条河流上的各个采样站进行的现场调查中收集数据。使用的直播床概念来自刘明(1954)电阻方程和爱因斯坦 - 棕色(1981)沉积物运输概念。问题减少到权力法关系的问题。这些数据被拟合到电力关系中,以获得形式的预测模型:f〜1q =k_φ〜(k1),其中参数f〜1q是无量纲沉积物放电,φ是无量纲床剪切应力,k_1和k_2是沉积物运输系数。校准模型将ogbese河河的K_1和K_2的值产生为0.592和0.865,以及Owena河分别为0.335和1.197。当测试ogbese和Owena Rivers的预测模型与Ackers and White(1973),Engleund和Hansen(1967),yang(1973)A 和Karim(1998)相比表现良好。结论是,开发的模型对于Ogbese和Owena Rivers的工程设计目的是有用的。

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