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Analysis for Suspended Load along the fluctuating backwater Region in Trial Impoundment of Three Gorges Reservoir

机译:三峡水库蓄水试验中变动回水区悬移质分析

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摘要

Three gorges hydropower, the biggest hydropower project in the world at present, is a backbone project for flood control and water power development of Yangtze river. From the flood season in 2008 with the beginning test impounding to 2012 has been implemented for five years, that water level has been continue to rise to 175m during 2010 to 2012. After the impoundment to normal water level, backwater is near Jiangjin during dry season with water level of 175m and is nearby Changshou in flood with water level of 145m, then Changshou upstream is the fluctuating backwater region. In this paper, based on a large amount of measured hydrologic data with Zhutuo, Cuntan, Qingxichang and Beibei, Wulong hydrological station on fluctuating backwater region, firstly suspended sediment inflow changes is analyzed, secondly suspended sediment characteristics is studied from the grouping sediment content and gradation change along the river in experimental impounding, then suspended sediment basic characteristics is gained about varying backwater region.
机译:三峡水电是目前世界上最大的水电工程,是长江防洪和水电开发的骨干工程。从2008年汛期开始试蓄水到2012年已经实施了五年,2010年至2012年水位一直持续上升到175m。蓄水至正常水位后,枯水期回水在江津附近,水位175m,洪水期回水在长寿附近,水位145m,长寿上游为变动回水区。本文根据朱坨、村滩、青西昌、北碚、武隆水文站在变动回水区的大量实测水文资料,首先分析了悬移质输沙量的变化,其次从试验蓄水过程中沿河的分组含沙量和级配变化研究了悬移质泥沙特性,得到了不同回水区的悬沙基本特征。

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