摘要
本文论证了冰期岸边流速系数α=0.7是合理的。根据有冰盖情况下垂线流速分市公式,证明了半深流速系数和冰底糙率与河床糙率比有关,并给出半深系数的近似值,可供无资料情况下使用。
In this paper,the reasonable value of velocity coefficient(α=0.7)near stream bankin ice period is given. On the basis of vertical velocity distribution with ice cover,it hasbeen proved that the semi-depth velocity coefficient is related to bed roughness and bottom ice roughness,and its approximant is given for practical use.
出处
《黑龙江大学工程学报》
1995年第2期43-48,53,共7页
Journal of Engineering of Heilongjiang University
关键词
冰期
岸边流速系数
半深流速系数
ice period, velocity coefficient near stream bank, semi-depth velocity coefficient