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A study of sedimentation rate in the lower Yellow Riverbased on cross section measurement data

机译:基于断面测量数据的黄河下游沉积率研究

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Using cross section measurement data, the sedimentation rate of the lower Yel-low River was determined. There are two methods to determine channel sedimentation rate, the method of sediment budget using data of suspended sediment loads, and the method using data of cross-section measurement. The latter has the advantage of avoiding the error that may be resulted from sediment load measurement, which is incapable of measuring the near-bot-tom suspended sediment and bed-load. Moreover, in so-doing, when relating annual channel sedimentation rate to the incoming sediment load, the demand of independence between the independent and dependent variables can be satisfied. Based on annual data from the period 1952-1999, correlations between channel sedimentation rate and a number of flow and sedi-ment indices have been established, all significant at a level of p < 0.01. Then, some multiple equations have been established, which can be used to estimate channel sedimentation rate based on a number of influencing variables including suspended sediment load and its grain size compositing, water discharge and, hyperconcentration flow frequency. These equations may provide some useful information for better environment management in general, and for sediment management in particular, in the Yellow River basin.
机译:使用横截面测量数据,确定下耶洛河的沉积速率。确定河道沉降速率的方法有两种,一种是使用悬浮泥沙负荷数据的泥沙预算方法,另一种是使用横截面测量数据的方法。后者的优点是避免了因沉积物负荷测量而导致的误差,而该误差是无法测量接近底部的悬浮沉积物和床层负荷的。此外,这样做时,将年度河道沉降速率与入泥沙量相关联,就可以满足自变量和因变量之间的独立性要求。根据1952-1999年期间的年度数据,已建立了河道沉积速率与许多流量和泥沙指数之间的相关性,所有这些均在p <0.01的水平上具有显着性。然后,建立了多个方程,可以根据包括泥沙悬浮量及其粒度组成,排水量和高浓度流动频率在内的许多影响变量来估算河道的沉积速率。这些方程式可能为总体上更好的环境管理,尤其是黄河流域的沉积物管理提供一些有用的信息。

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