近 60 年长江上游泥沙变化特征及主要影响因素的统计研究

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Lvze Duan , Yiman Tian , Shuanghu Zhang , Xingbo Wang , Chong Li , Min Chen
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引用次数: 0

摘要

过去 60 年间,长江上游的沉积物发生了显著变化。在即将开始的长江流域综合治理阶段,必须确定这些沉积物变化的特征和原因。本研究基于 1960 年至 2020 年的沉积物观测数据,研究了长江上游主流及其重要支流沉积物的变化趋势和突变。量化了降水变化和各种人类活动对泥沙负荷变化的相对贡献。建立了泥沙变化与大型水坝工程建设、水土保持措施和地震灾害之间的关系。结果表明,泥沙负荷出现了显著下降,主要变化发生在 1985 年代和 2010 年代前后。多重双质量曲线用于量化降水变化和人类活动对泥沙负荷变化的相对贡献。大坝对泥沙量减少的相对贡献率从 53% 到 74% 不等。降水变化在观测到的变化中发挥了重要作用,占 10% 到 27%。水土保持措施需要一段时间才能显示出对减少泥沙量的影响。这些措施通过稳定土壤和改善水文条件发挥作用。平均而言,这些措施对减少沉积物的作用在 7% 到 20% 之间。近来,嘉陵江和岷江等河流的泥沙量明显增加。这种意外增加可能与地震、强降水和局部泥沙冲刷等多种因素有关。这项研究的结果为了解河流泥沙负荷的变化提供了宝贵的见解,有助于改善水资源和大型水坝泥沙的管理。这些发现为大坝管理提供了有益的启示。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Statistical studies of the characteristics and key influencing factors of sediment changes in the upper Yangtze River over the past 60 years

Sediments in the upper Yangtze River have significantly changed over the past 60 years. The characteristics and causes of these sediment changes must be determined in the upcoming phases of the comprehensive management of the Yangtze River Basin. Based on sediment observation data from 1960 to 2020, this study examined the trends and sudden changes in the sediments in the mainstream and its significant tributaries in the upper Yangtze River. The relative contributions of precipitation change and various human activities to sediment load changes are quantified. The relationships between sediment variations and the construction and large dam projects, soil and water conservation measures, and earthquake disasters are established. The results indicate that there was a significant decline in sediment load with main changes occurring around the 1985s and 2010s. Multiple double mass curves are used to quantify the relative contributions of precipitation change and human activities to sediment load changes. The relative contribution of dams to the decrease in sediment load ranges from 53 % to 74 %. Precipitation change serves a significant role in the observed changes, accounting for a range of 10 % to 27 %. Soil conservation measures take some time to show their impact on sediment reduction. These measures work by stabilizing the soil and improving hydrological conditions. On average, they contribute between 7 % and 20 % towards reducing sediment. In recent times, there has been a noticeable rise in sediment load in rivers like the Jialing and Min Rivers. This unexpected increase could potentially be linked to a combination of factors including earthquakes, heavy precipitation, and localized sediment scouring. The results of this study offer valuable insights into the variations in river sediment load, aiding in the improved management of water resources and sediment in large dams. These findings provide helpful insights for dam management.

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来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
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