首页 | 本学科首页   官方微博 | 高级检索  
     检索      

室内小流域降雨产流过程试验
引用本文:屈丽琴,雷廷武,赵 军,余新晓,高佩玲,闫丽娟.室内小流域降雨产流过程试验[J].农业工程学报,2008,24(12):25-30.
作者姓名:屈丽琴  雷廷武  赵 军  余新晓  高佩玲  闫丽娟
作者单位:1. 中国农业大学水利与土木工程学院,北京,100083
2. 中国农业大学水利与土木工程学院,北京100083;中科院、水利部水土保持研究所土壤侵蚀与旱地农业国家重点实验室,杨凌7121001
3. 中科院、水利部水土保持研究所土壤侵蚀与旱地农业国家重点实验室,杨凌,7121001
4. 北京林业大学水土保持学院水土保持与荒漠化防治教育部重点实验室,北京,100083
5. 山东理工大学资源与环境工程学院,淄博,255049
基金项目:国家自然科学基金资助项目(40635027)
摘    要:该研究采用新型的小水流流量自动观测系统,在室内小流域模型上进行了不变雨强和变雨强模拟降雨试验,实时观测了模型流域各沟道的产流过程。试验进行了不同降雨强度(25、50、75、120mm/h)和不同降雨历时(5、10、15min)组合的12次降雨试验,同时进行了30-70mm/h和70-30-70mm/h的变雨强降雨试验。在不变雨强的条件下,仪器与人工测量所得稳定流量的最大平均相对误差仅为2.02%。测量得到的流量过程线呈现出起流、稳定和退水3个明显的阶段。其中,起流和退水过程涨落的剧烈程度、稳定阶段的流量大小随雨强增大而增大,稳定阶段的持续时间与降雨历时成正比。空间上,主沟出口的产流过程明显滞后于支沟出口的产流过程,且其两者之间具有一致的流量过程。在变雨强的情况下,流量过程线没有稳定的阶段,流量随雨强变化而变化。该研究对于深入理解流域产流过程具有重要意义,可为相关的模型研究提供可靠的试验支持。

关 键 词:产流  过程  小流域  自动测量系统  人工降雨
收稿时间:7/6/2007 12:00:00 AM
修稿时间:2008/10/1 0:00:00

Laboratory experiments of runoff processes in small watershed under simulated rainfall
Qu Liqin,Lei Tingwu,Zhao Jun,Yu Xinxiao,Gao Peiling and Yan Lijuan.Laboratory experiments of runoff processes in small watershed under simulated rainfall[J].Transactions of the Chinese Society of Agricultural Engineering,2008,24(12):25-30.
Authors:Qu Liqin  Lei Tingwu  Zhao Jun  Yu Xinxiao  Gao Peiling and Yan Lijuan
Institution:Qu Liqin1,Lei Tingwu 1,2,Zhao Jun 2,Yu Xinxiao 3,Gao Peiling 4,Yan Lijuan 1
Abstract:A new automatic measurement system of flow was applied.Simulated rainfall experiments were conducted under constant and variable rainfall intensity in small watershed in the laboratory.Runoff processes of the watershed branches were monitored realtimely.Under the constant rainfall intensity,12 rainfall experiments were conducted involving a complete combination of four kinds of rainfall intensity(25,50,75,120 mm/h)and three kinds of rainfall duration(5,10,15 min).The experiments of variable rainfall intensity were conducted at 30-70 mm/h and 70-30-70 mm/h rainfall events.Under the constant rainfall intensity,the maximum averaged relative error of the measured values of stable flow between the automatic system measurement and the manual measurement is only 2.02%.The runoff diagrams had three obvious stages of initial runoff,stable flow and recession flow.The severe degrees of fluctuation in the processes of initial runoff and recession flow and the flow of stable flow were increased with the increasing of rainfall intensity while the duration of the stable crest segment was directly proportion to rainfall duration.The runoff processes at the watershed outlets delayed to those at the branches,but the processes no matter at the outlets or branches of the watershed were identical in shape.Under the variable rainfall intensity,the runoff processes had no stable segment and the flow changed with the rainfall intensity.The results are significantly meaningful for understanding the runoff process.The results also can provide reliable experimental support for related model research.
Keywords:runoff  process  small watershed  automatic measurement  simulated rainfall
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《农业工程学报》浏览原始摘要信息
点击此处可从《农业工程学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号