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黄河水量明显减少对下游河流地貌的影响
引用本文:李有利,傅建利,杨景春,倪晋仁.黄河水量明显减少对下游河流地貌的影响[J].水土保持研究,2001,8(2):7-12.
作者姓名:李有利  傅建利  杨景春  倪晋仁
作者单位:1. 北京大学城市与环境学系,
2. 北京大学环境科学中心,
基金项目:国家重点基础研究发展规划项目(G1999043603)和国家自然科学基金项目(40071016)资助。
摘    要:分析了黄河下游河床和河口区侵蚀及淤积的变化与黄河水沙变化的关系,黄河水量减少,包括总水量和洪峰水量的减少,会引起下游河床淤积,河口地区淤积减弱,甚至侵蚀后退,也会影响河口以外海岸带泥沙的供给情况,造成黄河三角洲海岸的侵蚀后退。

关 键 词:水量  侵蚀  堆积  河道  河口  黄河  淤积
文章编号:1005-3409(2001)02-0007-06

Geomorphological Effect of Discharge Reduction on the Lower Reaches of the Yellow River
LI You-li,FU jian-li,YANG Jing-chun,NI Jin-ren.Geomorphological Effect of Discharge Reduction on the Lower Reaches of the Yellow River[J].Research of Soil and Water Conservation,2001,8(2):7-12.
Authors:LI You-li  FU jian-li  YANG Jing-chun  NI Jin-ren
Abstract:Based on the study the relationship of the erosion/deposition in the lower reaches of the Yellow River and the variation of river discharge, it is concluded that the decrease of the discharge can induce the deposition in the river channel, and sedimentary reduction even retreat of the river mouth. The reduction of sand supply of the Yellow River also can induce erosion along the coasts of the Yellow River delta and retreat of the delta.
Keywords:
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