SEDIMENT TRANSPORTED BY DEBRIS FLOWTO THE LOWER JINSHA RIVER

被引:21
作者
CUI Peng1
WEI Fangqiang2 and LI Yong3(1 Prof. Dongchuan Debris Flow Observation and Research Station. Institute of Mountain Hazards and Environment
机构
关键词
Debris flow; Sediment yield. Jinsha River;
D O I
暂无
中图分类号
TV148 [河口、港湾、海岸泥沙];
学科分类号
081502 ;
摘要
The lower Jinsha River is an area with the highest sediment yield in the upper Yangze basin. Itcovers only 9.27% of the total area of the basin but supplies about 40% of the total sediment recordedat the Yichang Hydrological Station. The present study shows that besides strong slope erosion andwaste discharge from engineering works, debris-flow transport is an important source of the sedimentload in the river. Based on field investigation and measurement, the annual sediment transport intothe lower Jinsha River basin was estimated at 1.54×10 to 67.07×10.
引用
收藏
页码:67 / 71
页数:5
相关论文
共 2 条
[1]  
995, Debris flow activity in the lower reaches of Jinsha River in Sichuan Province. Zhong D.L. et al. .
[2]  
984, Characteristics of glacial debris flows in Guxiang Gully, Tibet Autonomous Region. Wang W.H. et al. .