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古洪水行洪断面面积的估算
引用本文:谢悦波,张素亭,毕东生.古洪水行洪断面面积的估算[J].河海大学学报(自然科学版),1999,27(5):8-11.
作者姓名:谢悦波  张素亭  毕东生
作者单位:1. 河海大学水文水资源及环境学院,南京,210098
2. 水利部海河水利委员会水情处,天津,300170
3. 山东黄河河务局水情处,济南,250013
基金项目:国家自然科学基金,国土资源部地质开放研究实验室资助
摘    要:根据中国四大江河(长江、黄河、海河、淮河)古洪水研究的成果,提出了在冲淤变化型河床上进行古洪水行洪断面面积估算的方法,即将估算的断面面积分为三个部分;现代均衡断面面积、古洪水均衡断面面积和次洪水冲刷断面面积。应用结果表明,次洪水冲刷断面面积往往占总过水断面面积的比重较大,不可忽略。

关 键 词:古洪水  行洪断面  新构造运动  冲淤变化
修稿时间:2004/11/11 0:00:00

Palaeoflood Channel Cross Section Area Estimates
Xie Yuebo,Zhang Suting,Bi Dongsheng.Palaeoflood Channel Cross Section Area Estimates[J].Journal of Hohai University (Natural Sciences ),1999,27(5):8-11.
Authors:Xie Yuebo  Zhang Suting  Bi Dongsheng
Abstract:To obtain a palaeoflood discharge based on the pinch outs of its slackwater deposits,the palaeoflood channel cross section area is required.Overseas palaeoflood research is limited in valley type rivers.After the research work on the four largest rivers(Yangtze River,Yellow River,Haihe River,Huai River)in China,a method is present for the estimation of the cross sectional area of the allavial stream.The area is divided into three parts:the present mean cross sectional area,the difference between the present cross sectional area and the sectional area for the year of occurence of the palaeoflood,and the difference between the present mean cross sectional area and the maximum area of the erosion section.The conclusion is drawn that the third part is larger than the second part.
Keywords:palaeoflood  palaeochannel  alluvial stream  tectonic movement
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