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Erodibility of fine soil from the composite river bank of Brahmaputra in India

机译:印度布拉马普特拉复合河岸细土壤的可蚀性

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The erosion of a composite river bank critically depends on the erodibility of its fine soils, as the fine soil has higher resistancenagainst erosion. Therefore, for the estimation of the bank erosion in the case of a composite river bank, it is important tondetermine the critical shear stress and erodibility coefficients of the bank soil and their spatial distribution. In the present study,nerodibility parameters of the river bank of Brahmaputra in India have been estimated through 58 in situ submerged jet tests.nThe significance of spatial and layer-wise distribution of the erodibility parameters was tested through analysis of variancen(ANOVA). Results indicate that the spatial variation of erodibility parameters is highly significant, but layer-wise variationsnof the erodibility parameters are not significant. Therefore, the erodibility of the riverbank depends on the particular location,nwhereas layer-wise average erodibility parameters can be lumped for the estimation of the bank erosion for the specific site.nUsing the measured erodibility parameters, yearly river bank erosions at the study locations were computed and found to fallnwithin the reported range of the bank erosion in the Brahmaputra River. Copyright  2010 John Wiley & Sons, Ltd.
机译:复合河岸的侵蚀严重取决于其细土的易蚀性,因为细土对侵蚀的抵抗力更高。因此,对于估算复合河岸情况下的河岸侵蚀,重要的是确定河岸土壤的临界剪切应力和侵蚀性系数及其空间分布。在本研究中,印度的布拉马普特拉河沿岸的侵蚀力参数通过58次原位水下射流试验进行了估算。n通过方差分析(ANOVA)检验了侵蚀性参数在空间和分层上的意义。结果表明,可蚀性参数的空间变化非常显着,但可蚀性参数的逐层变化并不显着。因此,河岸的可蚀性取决于特定的位置,而可以将分层平均可蚀性参数集总起来以估算特定地点的河岸侵蚀。通过使用测得的可蚀性参数,研究地点的年河岸侵蚀量为计算并发现其落在Brahmaputra河的河岸侵蚀报告范围之内。版权所有©2010 John Wiley&Sons,Ltd.

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