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北京市泥石流灾害临界雨量研究
引用本文:白利平,南赟,孙佳丽.北京市泥石流灾害临界雨量研究[J].中国地质灾害与防治学报,2007,18(2):34-36,41.
作者姓名:白利平  南赟  孙佳丽
作者单位:北京市地质研究所,北京,100011
基金项目:北京市跨世纪优秀人才培养计划
摘    要:降雨是泥石流灾害的主要诱发因素。文章根据北京市历史上泥石流灾害发生时的前期雨量与当日激发雨量,建立了临界雨量判别模型。通过对北京地区泥石流灾害与降雨频率的分析,计算了不同时段的临界雨量;经验证明,计算结果是可信的。基于灾害与降雨频率分析来确定北京地区泥石流发生的临界雨量是一种新的尝试。该方法可用于计算不同泥石流沟道发生泥石流的临界雨量。

关 键 词:泥石流  灾害  临界雨量判别模型  北京市
文章编号:1003-8035(2007)02-0034-03
收稿时间:2006-08-14
修稿时间:2006-08-142006-09-28

Research on critical rainfall of debris flows in Beijing
BAI Li-ping,NAN Yun,SUN Jia-li.Research on critical rainfall of debris flows in Beijing[J].The Chinese Journal of Geological Hazard and Control,2007,18(2):34-36,41.
Authors:BAI Li-ping  NAN Yun  SUN Jia-li
Institution:Beijing Institute of Geology, Beijing 100011, China
Abstract:Precipitation is the main factor of begetting the debris flow,and the mostly used method of computing the critical rainfall in debris flow is the discriminance of critical precipitation,which is based on the statistical data.Based on the data of rainfall in Beijing,the model of computing the critical rainfall for debris flow was established.The frequency of precipitation and debris flow was also analyzed in this paper,and the critical rainfall for debris flow of different periods of time(the maximum 10 minutes,the maximum 30 minutes,the maximum 60 minutes,the maximum 360 minutes,the maximum 24 hours and the maximum 3 days) were computed.Computing the critical rainfall through this way is a new method,which can be used in computing the critical precipitation of different channels in Beijing.
Keywords:debris flow  hazard  critical rainfall  computing model  Beijing City
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