长江上游主要支流水沙特性及其影响因素分析  

Analysis of water and sediment characteristics in the main tributaries of the Yangtze River and their associated influence factors

作　　者：王正成[1] 毛海涛[1,2] 申纪伟[1] 唐鑫 陈相[1] WANG Zhengcheng;MAO Haitao;SHEN Jiwei;TANG Xin;CHEN Xiang(College of Civil Engineering,Chongqing Three Gorges University,Chongqing 404100,China;Institute of Water Conservancy and Hydroelectric Power,Wuhan University,Wuhan 430072,China)

机构地区：[1]重庆三峡学院土木工程学院,重庆404100 [2]武汉大学水利水电学院,武汉430072

出　　处：《华东师范大学学报（自然科学版）》2020年第1期126-138,共13页Journal of East China Normal University(Natural Science)

基　　金：国家自然科学基金(41602367);重庆市科委基础与前沿研究计划(cstc2018jcyjA,cstc2019jcyj-msxm1330);重庆市教委科学技术研究项目(KJQN201901209,KJQN201901209,KJQN201901240);重庆三峡学院土木工程学院院级青年科研项目(18QN006)

摘　　要：雅砻江、岷江、嘉陵江和乌江的水沙特性是决定长江泥沙变异的关键因素之一,关乎三峡水库的合理运行,关系着长江流域水资源的合理开发利用及水生态平衡.本文基于2002—2016年期间,长江主要支流设置的桐子林、高场、北碚、武隆4所重要控制性水文站水文泥沙监测资料,深入系统地探讨水文泥沙参量的变化特征及其影响因素,借助统计软件SPSS进一步分析水文泥沙参量的相关性.研究结果表明:在时序上,各支流年均含沙量、年输沙量、年输沙模数降低22.57%~91.54%,年径流量雅砻江、岷江和乌江增大3.28%~17.96%,嘉陵江降低1.58%;嘉陵江和乌江的中值粒径增大50%~80%.水电站的修建导致年均含沙量、年输沙量、中值粒径、年输沙模数降低5%~79.34%;强降雨、滑坡、塌方、泥石流、溃坝等自然灾害以及人为诱发滑坡和向河道倾倒土石体致使年均含沙量、年输沙量、年输沙模数增大20%~702.94%.参数间相关性由强到弱排序为年均含沙量和年输沙量/年输沙模数,年径流量和年均含沙量,年径流量和年输沙量/年输沙模数,年均含沙量和中值粒径,中值粒径和年输沙量/年输沙模数,以及年径流量和中值粒径.研究成果将为长江支流梯级电站的规划设计、三峡水库的合理运行提供理论支撑.Water and sediment characteristics of Yalong River,Minjiang River,Jialing River,and Wujiang River are one of the defining aspects of variation in Yangtze River sediment;they have influence on the operation of the Three Gorges Reservoir,which is related to utilization of water resources in the Yangtze River Valley and equilibrium of the water ecosystem.This article is based on hydrological and sediment monitoring data from 2002—2016 of four important hydrological control stations set up in the main tributaries of the Yangtze River,which are Tongzilin,Gaochang,Beibei,and Wulong.Variation characteristics of hydrology and sediment parameters and their associated influence factors were studied systematically;correlations between hydrological and sediment parameters were subsequently analyzed by SPSS.The results showed that over time:the annual average sediment concentration,annual sediment load,and modulus of sediment transport of the tributaries of the Yangtze River decreased 22.57%~91.54%;the annual runoff of Yalong River,Minjiang River,and Wujiang River increased 3.28%~17.96%,but that of Jialing River decreased 1.58%;and the median size of sediment of the Jialing and Wujiang Rivers increased 50%~80%.Furthermore,cascade hydro power stations were built,which led to annual average sediment concentration,annual sediment load,median size of sediment,and modulus of sediment transport to decrease by 5%~79.34%.Natural disasters such us heavy rainfall,landslide,collapse,debris flow,dambreak,landslide under artificial conditions,and dumping earth rock into a river lead to annual average sediment concentration,annual sediment load,and modulus of sediment transport to increase by 20%~702.94%.Correlations between the parameters ranked from strong to weak are:annual average sediment concentration and annual sediment load/annual average sediment transport modulus,annual runoff and annual average sediment concentration,annual runoff and annual sediment load/annual average sediment transport modulus,annual average sediment concen

关 键 词：长江支流 年径流量 年均含沙量 年输沙量 年输沙模量 中值粒径 

分 类 号：TU443[建筑科学—岩土工程]