IMHE OpenIR  > 山地灾害与地表过程重点实验室
佳禾沟泥石流堆积物的粒度与强度关系分析
Alternative TitleAnalysis on Grain-size Characteristics and Shear Strength of the Deposit in Jiahe Gully
苟万春1,2,3; 李泳1,2; 王保亮1,2,3; 刘道川1,2,3
Corresponding Author李泳
2015-12-18
Source Publication科学技术与工程
ISSN1671-1815
Volume15Issue:35Pages:120-123+144
Other Abstract 佳禾沟位于云南省维西县中路乡佳禾村,历史上曾多次发生不同规模的泥石流,并造成了人员伤亡和财产损失。通过对沟道流域沿线不同位置取样,用泥石流颗粒标度分析法并结合强度实验,发现佳禾沟泥石流松散堆积物的颗分参数μ与P(D2)之间存在线性关系,这说明μ影响了泥石流的启动;物源区中的细颗粒的迁移、上游泥石流部分物质的随机性停歇和沟道支沟和主沟陡坡物质的随机性补给导致了颗分参数(μ,Dc)的波浪式发展。黏聚力c与μ之间的关系为线性关系,c随着μ的增加而增加。这说明细颗粒的组成控制了黏聚力c的大小,因此推断黏聚力受到细颗粒之间的胶结作用和静电作用等因素的影响。内摩擦角φ与Dc之间的关系为负线性相关,而φ随着Dc的增加而变小,粗颗粒决定了φ的发展。因此,在相同条件下,较大的μ和较小的Dc组合的土体,其强度较大;这从定量的角度上验证了颗粒级配与土体强度的关系。以上结论是否适用于其他流域需进一步验证。此外,还应结合颗粒形状,土动力学,渗透理论分析泥石流发生机理。 
; Jiahe gully is located in Weixi,Yunnan. Several different scale debris flows have happened here in history,which caused injuries,deaths and property loss. By sampling in different positions,then using scaling analysis and strength experiment,the grain size distribution parameter μ increases as P( D2 ) increases with a linear
way were found,which indicates that μ influences the debris flow startup. Fine-grained migration in provenance and debris flow material stochastic cease and random replenishment lead to the unordered variation of μ and Dc. Cohesive force c increases as μ augments,which manifests that the fine grains control c,so cementation and electrostatic interaction between fine grains determines c were deduced. The relationship between φ and Dc is linear,and φ becomes smaller with the increase of Dc
,so it shows coarse grains control the φ. Consequently,in the same other
conditions,the soil with the bigger μ and the smaller Dc owns higher shear strength. The conclusions above need more drainage basins to confirm and particle shape,soil dynamics and seepage theory shoul be combined to research
Keyword泥石流 颗分参数 粒度分析 强度参数
Subject AreaP642.23
Indexed By北大中文核心
Language英语
Funding Organization国家自然科学基金项目(40771010)
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/17211
Collection山地灾害与地表过程重点实验室
Affiliation1.中国科学院山地灾害与地表过程重点实验室
2.中国科学院水利部成都山地灾害与环境研究所
3.中国科学院大学
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
苟万春,李泳,王保亮,等. 佳禾沟泥石流堆积物的粒度与强度关系分析[J]. 科学技术与工程,2015,15(35):120-123+144.
APA 苟万春,李泳,王保亮,&刘道川.(2015).佳禾沟泥石流堆积物的粒度与强度关系分析.科学技术与工程,15(35),120-123+144.
MLA 苟万春,et al."佳禾沟泥石流堆积物的粒度与强度关系分析".科学技术与工程 15.35(2015):120-123+144.
Files in This Item:
File Name/Size DocType Version Access License
佳禾沟泥石流堆积物的粒度与强度关系分析_(447KB)期刊论文作者接受稿开放获取CC BY-NC-SAView Application Full Text
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[苟万春]'s Articles
[李泳]'s Articles
[王保亮]'s Articles
Baidu academic
Similar articles in Baidu academic
[苟万春]'s Articles
[李泳]'s Articles
[王保亮]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[苟万春]'s Articles
[李泳]'s Articles
[王保亮]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: 佳禾沟泥石流堆积物的粒度与强度关系分析_苟万春.pdf
Format: Adobe PDF
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.