中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Variations in Sedimentation Rate and Corresponding Adjustments of Longitudinal Gradient in the Cascade Reservoirs of the Lower Jinsha River

文献类型:期刊论文

作者Wang, Suiji1,2
刊名WATER
出版日期2025
卷号17期号:2页码:262
关键词sedimentation rate channel gradient channel width-depth ratio heterogeneity cascade reservoirs lower Jinsha River
DOI10.3390/w17020262
产权排序1
文献子类Article
英文摘要The Xiangjiaba and Xiluodu reservoirs, as important components of the large cascade reservoirs in the lower Jinsha River, and the interactive changes in sediment trapping amounts, the differences in sedimentation dynamics, and the potential mutual influence mechanisms among them are scientific issues worthy of attention. Based on the multiple observed data of thalweg elevation before and after the completion of the dam construction, this study calculated the average sedimentation rates of all 20 km segments of the above-mentioned reservoirs in different periods. Meanwhile, the local mean gradients between adjacent segments and the regional mean gradients from the segments to the dam in the corresponding periods were calculated. The results show that the maximum and average sedimentation rates of the Xiangjiaba Reservoir, which was built earliest and is located downstream, were as high as 19.62 m yr-1 and 8.88 m yr-1, respectively, in the first half year after the dam closure. After the completion of the Xiluodu Reservoir, an adjacent cascade reservoir upstream, the average sedimentation rate of the Xiangjiaba Reservoir in the following seven years dropped to 0.67 m yr-1. The maximum and average sedimentation rates of the Xiluodu Reservoir were 9.07 m yr-1 and 4.15 m yr-1, respectively, within one year after the dam closure, and its average sedimentation rate in the following six years was 2.51 m yr-1. The spatial variations of sedimentation rates in these two reservoirs follow different changing patterns. There is an obvious correlation between the change in mean gradient and the change in sedimentation rate. The sequence of dam construction, the relative positions of the reservoirs, the differences in sediment trapping amounts, and operation modes are the key factors controlling the changes in sedimentation rate and gradient in the reservoir area. This study reveals the interactive changes in sedimentation rates among cascade reservoirs and the response mechanism of river channel morphology, and has a guiding role for the formulation of effective measures for the sustainable utilization of cascade reservoirs.
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WOS关键词DAMS
WOS研究方向Environmental Sciences & Ecology ; Water Resources
语种英语
WOS记录号WOS:001404807300001
出版者MDPI
源URL[http://ir.igsnrr.ac.cn/handle/311030/211357]  
专题陆地水循环及地表过程院重点实验室_外文论文
通讯作者Wang, Suiji
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China;
2.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Wang, Suiji. Variations in Sedimentation Rate and Corresponding Adjustments of Longitudinal Gradient in the Cascade Reservoirs of the Lower Jinsha River[J]. WATER,2025,17(2):262.
APA Wang, Suiji.(2025).Variations in Sedimentation Rate and Corresponding Adjustments of Longitudinal Gradient in the Cascade Reservoirs of the Lower Jinsha River.WATER,17(2),262.
MLA Wang, Suiji."Variations in Sedimentation Rate and Corresponding Adjustments of Longitudinal Gradient in the Cascade Reservoirs of the Lower Jinsha River".WATER 17.2(2025):262.

入库方式: OAI收割

来源:地理科学与资源研究所

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