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首页> 外文期刊>Open Journal of Civil Engineering >Experimental Study of Runoff Coefficients for Different Hill Slope Soil Profiles
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Experimental Study of Runoff Coefficients for Different Hill Slope Soil Profiles

机译:不同坡面土壤剖面径流系数的试验研究

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The estimation of peak discharge from a catchment due to intense rainfall is a difficult task that may occur in a return period. If cannot be estimated accurately, it may lead to serious problem in hydraulic structure design like bridge, culvert across a river and drainage system. The main parameter which affects the peak flow is runoff coefficient of the catchment which directly depends on the soil type, its slope and land use pattern with vegetation covers. For the purpose, this study was carried out to estimate maximum runoff coefficients for different land profiles and soil types in hill slope model developed in 10 degree with the horizontal to the rainfall simulator rig (Basic Hydrology system-S12) experimentally which can give more reliable value than the real field test method as it is easier than field test especially in hill slope. The soil slope preparation was made of sand, silt and clay separately and the experiments were carried out in a controlled system. The slope prepared represented a small catchment on a plot of 2.02 meter length, 1 meter wide and 0.15 m depth soil plots (at the slope of 10 ° to the horizontal plane). From the experiment in different soil plots, the rainfall runoff coefficients were observed as 0.428 - 0.53 for sand soil slope, 0.46 - 0.55 for silt soil slope and 0.42 - 0.51 for clay soil slope under uniform rainfall rate of 4 lpm to 13 lpm in each soil slope. Rainfall runoff correlation equation was found with the values of R above 90% in each soil slope. The value observed is within the range of rational value of 0.05 to 0.95 as standard which concluded that the performance of simulator was found good to deal with rational values. And the runoff coefficients for these soil types can be taken within the range obtained to estimate peak discharge in any small catchment area depending on the soil types.
机译:估算由于强降雨造成的流域洪峰排放是一项艰巨的任务,可能会在返回期间发生。如果无法准确估算,可能会导致水工结构设计中出现严重问题,例如桥梁,涵洞和排水系统。影响洪峰流量的主要参数是流域的径流系数,径流系数直接取决于土壤类型,坡度和植被覆盖的土地利用方式。为此,本研究在水平方向上与降雨模拟器架(Basic Hydrology system-S12)一起以10度开发的山坡模型中,估算了不同坡度和土壤类型的最大径流系数,从而可以提供更可靠的结果。比实地测试方法更有价值,因为它比实地测试更容易,尤其是在山坡上。土壤边坡制备分别由沙子,粉砂和粘土制成,并在受控系统中进行实验。所准备的坡度代表了一个小集水区,其长度为2.02米,宽为1米,深度为0.15 m(与水平面成10°的坡度)。通过在不同土壤样地上的试验,在4 lpm至13 lpm的均匀降雨率下,沙土坡的降雨径流系数分别为0.428-0.53,粉砂土坡的0.46- 0.55和黏土坡的0.42- 0.51。土壤坡度。在每个土壤坡度中,降雨径流相关方程的R值均大于90%。观察到的值在0.05到0.95的有理值范围内作为标准,这得出结论,发现模拟器的性能很好地处理了有理值。这些土壤类型的径流系数可以在获得的范围内取,以根据土壤类型估算任何小集水区的峰值流量。

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