摘要
进入洞庭湖的洪峰流量超过４００００ｍ￣３／ｓ时，称为大洪水年；城陵机水位达３３．０ｍ（冻结）以上时，本文中称为大洪灾年．将两个序列按大小顺序排列后发现，除第１及第５位分别同是１９５４年和１９６９年外，其余均不对应．本文对产生该现象的原因进行了系统分析．并在洪峰影响因素与最高洪水位间进行回归分析，得出经验方程式．
The time when the flood flow of Dongting Lake is over 40000m￣3/s is called thegreat flood water year and when the water stage at Chenglinji is over 33.0m (freezing) iscalled the great flood disaster year. After arranging these two series in accordance with sizeorder, it is discovered that with the exception of all the 1st and 5th places being respectively1954 and 1969 in these two series, all the rest places are not correspondent. The causes ofproducing this phenomenon are systematically analyzed in this paper. Analysis is also madebetween the causes influenced by flood peak and the highest flood stage. Finally, the relatedexperiential equation is obtained.
出处
《武汉水利电力大学学报》
CSCD
1995年第1期28-33,共6页
Engineering Journal of Wuhan University
关键词
洞庭湖
洪峰
流量
水位
顶托壅阻
flood peak discharge
water levels
lake regions
crest-lifting choke
