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金沙江流域水土流失现状与河道泥沙分析
引用本文:刘邵权,陈治谏,陈国阶,杨定国. 金沙江流域水土流失现状与河道泥沙分析[J]. 长江流域资源与环境, 1999, 0(4)
作者姓名:刘邵权  陈治谏  陈国阶  杨定国
作者单位:中国科学院水利部成都山地灾害与环境研究所!成都610041
摘    要:
对金沙江流域水土流失、河道泥沙及主要影响因素系统作了分析,认为地质、地貌及气候因子是影响水土流失的主要因素,人为活动加剧水土流失的发生发展。河道泥沙主要来自金沙江下游,特别是下游干流河谷区间,流域的地面侵蚀与河道泥沙的空间关系不密切,影响输沙量的主要因素为年径流量和清水区年径流量,以及滑坡、泥石流等重力侵蚀,尽管水土流失治理对于流域的河道泥沙减沙效应显著,但短期内对流域干支流输沙量影响甚微。今后一段时间内金沙江流域河道泥沙不会有显著的变化

关 键 词:金沙江流域  水土流失  河道泥沙

SURFACE EROSION AND FLUVIAL SILT IN THE JINSHA RIVER WATERSHED
LIU Shao quan,CHEN Zhi jian,CHEN Guo jie,YANG Ding guo. SURFACE EROSION AND FLUVIAL SILT IN THE JINSHA RIVER WATERSHED[J]. Resources and Environment in the Yangtza Basin, 1999, 0(4)
Authors:LIU Shao quan  CHEN Zhi jian  CHEN Guo jie  YANG Ding guo
Abstract:
Based on the analysis of major influence elements of the surface erosion and fluvial silt in the Jinsha River Watershed,the authors confirm that the conditions of geology, landform and climate are the major factors effceting the surface erosion,and the injudicious social economic activities intensified the occurrence and development of soil and water loss.The fluvial silt is chiefly produced in the lower reaches of the River,especially in the main river valley of the lower reaches.The surface erosion of the watershed is not closely related to the flvial silt in space,the major elements which in fluence the amount of water borne silt are the runoff volume in the watershed and in the clear water are of the watershed.Although the effect of the control of soil and water loss is remarkable in the reduction of fluvial silt in small warershed,yet is scarcely in fluences the amount of water borne silt in the mainstream and tributaries of the River.The fluvial silt of Jinsha River Watershed will not be notably reduced in short times.
Keywords:Jinsha River Watershed  surface erosion  fluvial silt
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