中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
“东川型”排导槽结构对泥石流流速影响的实验研究

文献类型:期刊论文

作者黄海 ; 马东涛 ; 王显林
刊名山地学报
出版日期2009-09-15
卷号27期号:5页码:551-556
关键词“东川型”排导槽 泥石流 流速 肋槛 纵比降
其他题名Experimental Study on the Relationships between the Velocity of Debris Flow and Structure of the Dongchuan Debris Flow Channel
通讯作者马东涛
中文摘要消能肋槛和排导槽纵比降是控制"东川型"泥石流排导槽内流体运动的两个关键因素。泥石流流速是反映排导槽工程输移力及对排导槽的冲刷淤积破坏的重要参数之一。通过实验,对固定配比的泥石流流体在不同的肋槛组合下的排导槽中的流速进行了研究,结果表明:(1)肋槛间距从40cm增加至60cm时,泥石流流速先增加后减少,在间距50cm时达到最大值;(2)肋槛高度对泥石流流速的影响非常复杂,在不同的肋槛间距和纵比降下表现不同的相关关系;(3)纵比降对排导槽内的泥石流流体基本呈正相关;(4)得到了肋槛间距与肋槛高度之比值N与泥石流流速V之间关系的数学表达式:V=0.0341N+C,其中C为常量。
英文摘要The debris flow velocity is one of important parameters on describe the transport capacity,deposition and erosion damage of debris flow channel.The Dongchuan debris flow channel is the most wide used type of channel with the characteristic of soft foundation energy dissipation in China,which is created by pre-scholars in the long time practice of debris flow mitigation.For the Dongchuan Channel,the threshold and gradient are two key factors to control the movement of debris flow in channel.By using a dynamic experimental system of debris flow,a series of indoor model tests on debris flow passing through channel with diffident threshold parameters are carried out.The follow test results are drawn:(1)When the spacing of threshold increase from 40 cm to 60 cm,the velocity is increased first and then reduced,it reaches maximum when the spacing of threshold is 50 cm;(2)The relationship between the height of threshold and velocity is very complex.When the threshold spacing and gradient change,the relationship would change too;(3)The relationship between the gradient and the velocity of debris flow is in positive correlation;(4)One formula has derived to express the relationship between the ratio of the threshold spacing and height N and the velocity of debris flow V from testing,which is V=0.0341N+C,where C is a constant number,which is varying in 1.01-1.41 and confined by gradient of the debris flow channel
分类号P642.23
收录类别CSCD
资助信息地质灾害防治与地质环境保护国家重点实验室开放基金资助项目
语种中文
CSCD记录号CSCD:3670147
公开日期2010-09-08
源URL[http://ir.imde.ac.cn/handle/131551/1866]  
专题成都山地灾害与环境研究所_成都山地所知识仓储(2009年以前)
推荐引用方式
GB/T 7714
黄海,马东涛,王显林. “东川型”排导槽结构对泥石流流速影响的实验研究[J]. 山地学报,2009,27(5):551-556.
APA 黄海,马东涛,&王显林.(2009).“东川型”排导槽结构对泥石流流速影响的实验研究.山地学报,27(5),551-556.
MLA 黄海,et al."“东川型”排导槽结构对泥石流流速影响的实验研究".山地学报 27.5(2009):551-556.

入库方式: OAI收割

来源:成都山地灾害与环境研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。