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THE INFLUENCE OF GRASS AND POROUS BARRIER STRIPS ON RUNOFF HYDROLOGY AND SEDIMENT TRANSPORT

机译:草和多孔障碍带对径流水文和泥沙输送的影响

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A series of experiments was conducted in a large tilting flume to investigate the effects of buffer strips on flow hydrology and sediment transport/deposition in and around the strips. Changes in flow depth caused by buffer strips of either nails or grass were recorded, photographed, and measured with a high degree of accuracy. Flow retardation took place at some distance ahead of the strips, causing the water level to rise. This distance is dependent upon flume slope and strip density for any given flow rate. With any increase in flume slope, the point at which water depth increased moved closer to the strip, entering it at around 6% slope. An exponential relationship exists between flume slope and backwater length. Backwater length is also dependent on strip density, and the relationship between these two factors is linear. Under our experimental conditions, sediment deposition did not take place within the strips, but before and after it. The lack of deposition inside the strips appears to be contrary to the common expectation from this technique. The bulk of sediment load in the sediment-laden flow approaching the strips was deposited ahead of the strips, commencing at the point where flow depth started to rise. The finer fraction of sediment load that entered the strip with the flow emerged from the other end unchanged. Some deposition took place as fans downstream of the strips, an indication of resistive flow velocity being slower before and after the strips than within them. When the soil or sand were not consolidated, significant erosion took place inside the strips, creating a head fall at the exit end of the strips, which moved upslope within the strips as experiments continued. For the range of slopes and strip widths studied, the efficiency of the grass or nail strips in slowing down the flow and unloading its sediment in the backwater region was independent of the width of strips in the flow direction. Grass strips thus appear to behave more like "grass barriers" or "grass buffers" than "filter strips," as they are referred to in some literature. The process interpretation of these results is discussed in this article
机译:在一个大的倾斜水槽中进行了一系列实验,以研究缓冲带对带内及其周围的流动水文和沉积物迁移/沉积的影响。记录,照相和测量由指甲或草的缓冲带引起的流动深度变化,并具有较高的准确度。滞流发生在钢带前面一定距离处,导致水位上升。对于任何给定的流速,该距离取决于水槽斜率和带材密度。随着水槽坡度的增加,水深增加的点将更靠近钢带,以6%的坡度进入钢带。水槽斜率与回水长度之间存在指数关系。回水长度也取决于带材密度,这两个因素之间的关系是线性的。在我们的实验条件下,沉积物的沉积不是在带内发生,而是在沉积之前和之后。条带内部缺乏沉积似乎与该技术的普遍预期相反。接近条带的充满泥沙的流动中的大部分泥沙载荷从条带开始沉积,开始于流动深度开始上升的位置。进入水流带的细颗粒泥沙部分从另一端流出而没有变化。在条带的下游以风扇的形式发生了一些沉积,表明在条带之前和之后的阻力流速比在条带内的阻力流速慢。当土壤或沙子没有固结时,条带内部会发生明显的侵蚀,从而在条带的出口端造成压倒,随着实验的进行,条带内的坡度向上移动。在研究的坡度和宽度范围内,草或钉条在回水区减缓流速并释放泥沙的效率与条带在流动方向上的宽度无关。因此,草条的表现更像是“草栅栏”或“草缓冲区”,而不是“过滤条”,正如它们在某些文献中提到的那样。本文讨论了这些结果的过程解释

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