Trends in suspended sediment grain size in the upper Yangtze River and its tributaries, as influenced by human activities
文献类型:EI期刊论文
作者 | Xu Jiongxin |
发表日期 | 2007 |
关键词 | Grain size and shape Reservoirs (water) Sediments Soil conservation |
英文摘要 | Based on data from five hydrometric stations, Pingshan station on the Jinshajiang River, Gaochang station on the Minjiang River, Wulong station on the Wujiang River, Wusheng station on the Jialingjiang River and Yichang station on the Yangtze River, a study has been made of the temporal variation in grain size of suspended sediment load in the upper Yangtze River. The results show that in the past 40 years, the grain size of the suspended sediment load in the main stem and major tributaries of the upper Yangtze River has had a decreasing trend, that can be explained by the effect of reservoir construction and implementation of soil conservation measures. The reservoirs in the upper Yangtze River Basin, all used for water storage for hydro-electric generation and/or irrigation, have trapped coarse sediment from the drainage area above the dam and, thus, the sediment released now is much finer than before the construction of the reservoirs. The downstream channels are all gravel-bedded or even in bedrock, with little fine sediment, and thus, the released flow can hardly get a supply of fine sediment through eroding the bed. Then, after the downstream adjustment, the grain size of suspended sediment is still fine. Large-scale soil conservation measures have significantly reduced sediment yield in some major sediment source areas. The relatively coarse sediment is trapped and, thus, the sediment delivered to the river becomes finer. Copyright © 2007 IAHS Press. |
出处 | Hydrological Sciences Journal |
卷 | 52期:4页:777-792 |
收录类别 | EI |
语种 | 英语 |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/24473] |
专题 | 地理科学与资源研究所_历年回溯文献 |
推荐引用方式 GB/T 7714 | Xu Jiongxin. Trends in suspended sediment grain size in the upper Yangtze River and its tributaries, as influenced by human activities. 2007. |
入库方式: OAI收割
来源:地理科学与资源研究所
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