河床侵蚀的实验研究  

An Experimental Research of River Bank Erosion

作　　者：李锋[1] 司振江 

机构地区：[1]黑龙江省水利水电勘测设计研究院,黑龙江省水利科学研究所

出　　处：《黑龙江大学工程学报》1995年第4期13-16,28,共5页Journal of Engineering of Heilongjiang University

摘　　要：自然河床的侵蚀（沉积）速度Ｅ可视为流速υ的二次函数：Ｅ＝αυ２＋βυ．此式统一了侵蚀和沉积过程。几种自然边坡的侵蚀试验结果支持了这种观点。The velocity(E) of erosion (sedimentation) of the natural river bank could be considered as a function of the water flowing velocity (V)with square power: E=αV2+βVThe process of erosion and sedimentation could be unified with it. Some test results oferosion in a few natural slopes could support the point of view.

关 键 词：河床侵蚀 沉积 自然植被 侵蚀试验 

分 类 号：TB143.5[一般工业技术]