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EFFECTS OF NAVIGATION ON SEDIMENTATION

机译:导航对沉积的影响

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An issue that has become of environmental concern is the possibility that navigationrntraffic can incorporate into the water column a considerable amount of material fromrnsediment beds. This material will deposit shortly thereafter or will remain inrnsuspension for some time depending on its size. Entrainment of pollutants attachedrnto the bed sediment, degradation of fish spawning areas and sedimentation of finernmaterial in backwater zones are some of the related problems.rnComputation of the amount and vertical distribution of suspended sediment requiresrna reference concentration near the bed or entrainment function, and considerablernresearch effort has been dedicated to obtain such formulae. Several entrainmentrnfunctions are available in the literature, but all of them have been developed forrnsteady, uniform flow conditions. The ability of such relationships to predictrnentrainment rates in unsteady flows has not been demonstrated, nor has there beenrnany attempt to develop a general formulation that works for both steady andrnunsteady flow conditions. The traditional approach relates the entrainment ofrnsediment to the wall shear stress associated with skin friction in a deterministic way,rnproviding only a relation between mean values. The approach presented hereinrnconsiders both the shear stress and the entrainment as stochastic turbulentrnquantities and expresses them in terms of their probability density functions (PDFs).rnThe resulting relation is valid for both steady and unsteady flow, since the effects ofrnunsteadiness are captured by the statistics.rnThis formulation was used to compute the amount and location of sedimentrnentrainment induced by the passage of tow barges. The wall shear stress informationrnused was gathered in a 1/25 Froude scale model of a tow barge. Total entrainmentrnand the associated scour produced by the passage of the tow barge were computedrnfor two uniform sediment sizes, namely 0.5 and 0.1 mm. The results show that highrnamounts of sediment are being entrained in both cases. However, the totalrnentrainment values for the two different sizes are not substantially different. Thernsediment size does become important when analyzing the effects on the bed, with arnmuch larger scour produced in the case of the finer sediment.
机译:引起环境关注的一个问题是,交通流量可能会将来自沉淀物床的大量物质纳入水柱。此材料此后不久将沉积,或将保持悬浮状态一段时间,具体取决于其尺寸。与此相关的一些问题是夹带在底泥上的污染物的夹带,鱼产卵区的退化和细料的沉淀。悬浮泥沙的数量和垂直分布的计算需要在底面附近具有参考浓度或夹带作用,并且需要大量的研究工作一直致力于获得这样的公式。文献中有几种夹带功能,但它们都是为稳定,均匀的流动条件而开发的。尚未证明这种关系能够预测不稳定流量中的夹带率,也没有进行任何尝试来开发适用于稳定流量和不稳定流量条件的通用公式的尝试。传统的方法是将确定的夹带关系与与皮肤摩擦相关的壁剪应力确定性地联系起来,只提供平均值之间的关系。本文提出的方法将剪切应力和夹带均视为随机湍流量,并用其概率密度函数(PDFs)表示。结果关系对于稳态和非稳态流动均有效,因为统计数据可以捕获非稳态的影响。该公式用于计算拖船通过引起的泥沙夹带的数量和位置。所使用的墙剪应力信息以拖船的1/25 Froude比例模型收集。对于两种均匀的沉积物尺寸,即0.5和0.1 mm,计算了拖带通过时的总夹带量和相关冲刷。结果表明,两种情况都夹带了大量的沉积物。但是,两个不同大小的总夹带值并没有实质性的不同。当分析对河床的影响时,沉积物的大小确实很重要,如果沉积物较细,则产生的冲刷量会更大。

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