[1]林雪平,游勇,柳金峰,等.动床条件下粘性泥石流沟道淤积实验研究[J].山地学报,2013,(03):327.
 LIN Xueping,YOU Yong,LIU Jinfeng,et al.Experimental Study on Channel Deposition of Viscous Debris Flow over Erodible Beds[J].Mountain Research,2013,(03):327.
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动床条件下粘性泥石流沟道淤积实验研究()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2013年03期
页码:
327
栏目:
山地灾害
出版日期:
2013-01-01

文章信息/Info

Title:
Experimental Study on Channel Deposition of Viscous Debris Flow over Erodible Beds
作者:
林雪平;游勇;柳金峰;赵彦波;刘曙亮;
1.中国科学院山地灾害与地表过程重点实验室,四川 成都610041;
2.中国科学院水利部成都山地灾害与环境研究所,四川 成都610041;
3.中国科学院大学,北京100049
Author(s):
LIN XuepingYOU YongLIU JinfengZHAO YanboLIU Shuliang
1. Institute of Mountain Hazards and Environment,Chinese Academy of Sciences & Ministry of Water Conservancy,Chengdu 610041,China;
2. University of Chinese Academy of Sciences,Beijing 100049,China
关键词:
粘性泥石流动床沟道淤积厚度实验研究
Keywords:
viscous debris flowchannel depositionexperimental studydeposition thicknesserodible beds
分类号:
P642.23
文献标志码:
A
摘要:
泥石流淤积是危害建筑物的主要方式之一。为了探讨动床条件下泥石流沟道淤积规律,开展了不同泥石流重度、不同沟床物质重度、不同沟道坡度以及不同泥石流总量共4组单次淤积实验和1组不同沟道坡度下的泥石流连续淤积实验。实验结果表明,单次淤积时,泥石流淤积厚度随着沟道坡度的增加而减小,随着泥石流重度的增大而增大,随泥石流总量的增大而增大,受沟床物质重度变化的影响较小;连续淤积时,随着沟道坡度的增加,第2次淤积相对于第1次淤积结果依次表现为完全淤积、冲淤交替以及完全冲刷,且冲刷始于沟道前缘,逐渐向后缘发展。在分析泥石流淤积厚度的影响因素基础上,通过回归分析建立了动床条件下粘性泥石流沟道淤积厚度的经验预测公式:...
Abstract:
Debris flow deposition is one of the main hazards for buildings. In order to explore the law of debris flow deposition over erodible beds,we carried out 4 groups single siltation experiment and 1 group successive siltation experiment. The single deposition experimental result shows that deposition thickness increases with the increase of channel slope debris,the increase of debris flow density and the increase of the total amount of debris flow. The bed material density has a small effect on the deposition thickness. By continuous sedimentation,along with the increase of channel slope,the second experiment in turn presented as complete cholestasis,half deposition and half erosion and scouring silting completely,and erosion began at the leading edge,gradually backward to edge of development. On the basis of analyzing of the factors of debris flow deposition thickness,this article established the prediction formula of viscous debris flow single siltation thickness through regression analysis: H=0.005x+(1.63E-11)erc-0.003ln(sinθ)+0.22V-0.02.

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备注/Memo

备注/Memo:
收稿日期(Received date):2012-12-10;改回日期(Accepted) : 2013-03-07。
基金项目(Foundation item):国家科技支撑计划(2011BAK12B03)和国家基金委中俄国际合作项目(41211120178)资助。[Supported by National Key Technologies R & D Program of China (Grant No. 2011BAK12B03) and the NSFC-RFBR project of the National Natural Science Foundation of China (Grant No. 41211120178).]
作者简介(Biography):林雪平(1987-),男,四川广安人,硕士,主要从事泥石流模拟实验与防治工程研究。[Lin Xueping(1987-),male,master,engaged in the experiment and mitigation research of mountain hazards.] *通信作者(Corresponding author):游勇(1964-),男,四川乐山人,研究员,主要从事山地灾害实验与防治工程研究。[You Yong(1964-),male,professor,engaged in mitigation research of mountain hazards.] E-mail:yyong@imde.ac.cn
更新日期/Last Update: 1900-01-01