摘要
近几十年来,汉江下游皇庄、沙洋、仙桃河段水沙量时有不平衡现象出现,水量时大时小,输沙量沿程增大。此现象已越来越受到各界的关注,此文的初步分析对于研究汉江下游皇沙仙段水沙不平衡现象有一定意义。
In recent years,there has been imbalance of water and sediment yield on the lower reaches of Hangjiang in Huangzhuang,Shayang and Xiantao.Water yield varies and sediment yield increases along the way.Such phenomena receive more amd more attention of the whole society.This preliminary analysis is of certain significance to the research of imbalance of water and sediment yield on the lower reaches of Hanjiang in Huangzhuang,Shayang and Xiantao.
出处
《长江工程职业技术学院学报》
CAS
2011年第1期23-24,共2页
Journal of Changjiang Institute of Technology
关键词
水量
沙量
不平衡
原因分析
汉江
water yield
sediment yield
imbalance
analysis of causes
Hanjiang River
