中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
ANALYSIS OF THE CORRELATION BETWEEN FRACTAL DIMENSION OF GRAVELLY SOIL AND DEBRIS-FLOW INITIATION THROUGH IN-SITU EXPERIMENTS

文献类型:期刊论文

作者Zhong, W.1,2; He, N.3; Cosgrove, T.4; Zhu, Y. J.3; Fu, L.3
刊名APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH
出版日期2019
卷号17期号:4页码:7573-7589
ISSN号1589-1623
关键词debris flow fractal theory particle size distribution initiation mechanism in-situ experiments disaster mitigation
DOI10.15666/aeer/1704_75737589
通讯作者He, N.(hn61886@163.com)
英文摘要Particle size distribution of the gravelly soil in debris flow source area has a great impact on the formation mechanism of debris-flow. In order to explore the relationship between particle composition and debris flow initiation, we collected 182 soil samples from debris flow source areas. Sieving tests have been conducted in the laboratory to acquire the fundamental particle size distribution data. Subsequently, the fractal theory was employed to compute the fractal dimension of each soil sample, analyzing the results of calculation we found that the gravelly soil in debris flow source area is mainly concentrated in one fractal dimension, the value of which ranges from about 2.250 to 2.798. Comparing the results of calculation and sieving experimentation, the underlying relationship between particle composition and fractal dimension can be revealed: the particle compositions of the gravelly soil tend to remain uniform as the fractal dimension increases. On the basis of the calculation results, the in-situ artificial rainfall experiments can be designed and performed. Analyzing the phenomenon during the processes of the experiments, the initiation mechanism with different fractal dimensions can be preliminarily identified: The gravelly soil which can mobilise into debris flows exhibits significant criticality feature, and the gravelly soil with fractal dimension ranges from 2.4 to 2.6 are more susceptible to mobilise into debris flow, and the scale of the debris flow is relatively larger. For slopes with fractal dimension < 2.4, the possibility of mobilisation into debris flow is extremely low. When fractal dimension ranges from about 2.6 to 2.7, the density of the formed debris flow is relatively lower, under which the formation of debris flows exhibits significant intermittent characteristics.
WOS关键词RAINFALL THRESHOLDS ; MODEL ; SIZE ; RUNOFF ; LANDSLIDE ; CLASSIFICATION ; MAGNITUDE ; DELIVERY ; SLOPE ; BASIN
资助项目National Key R&D Program of China[2018YFC1505205] ; National Natural Science Foundation of China[41302284] ; National Natural Science Foundation of China[41661144028] ; Henan Polytechnic University[B2015-58] ; Henan Postdoctoral Foundation[19030069]
WOS研究方向Environmental Sciences & Ecology
语种英语
出版者CORVINUS UNIV BUDAPEST
WOS记录号WOS:000478066700026
资助机构National Key R&D Program of China ; National Natural Science Foundation of China ; Henan Polytechnic University ; Henan Postdoctoral Foundation
源URL[http://ir.imde.ac.cn/handle/131551/26781]  
专题成都山地灾害与环境研究所_山地灾害与地表过程重点实验室
通讯作者He, N.
作者单位1.Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Sichuan, Peoples R China
2.Chinese Acad Sci, Key Lab Mt Hazards & Surface Proc, Chengdu 610041, Sichuan, Peoples R China
3.Henan Polytech Univ, Sch Civil Engn, Jiaozuo 454003, Henan, Peoples R China
4.Univ Limerick, Dept Civil Engn & Mat Sci, Limerick, Ireland
推荐引用方式
GB/T 7714
Zhong, W.,He, N.,Cosgrove, T.,et al. ANALYSIS OF THE CORRELATION BETWEEN FRACTAL DIMENSION OF GRAVELLY SOIL AND DEBRIS-FLOW INITIATION THROUGH IN-SITU EXPERIMENTS[J]. APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH,2019,17(4):7573-7589.
APA Zhong, W.,He, N.,Cosgrove, T.,Zhu, Y. J.,&Fu, L..(2019).ANALYSIS OF THE CORRELATION BETWEEN FRACTAL DIMENSION OF GRAVELLY SOIL AND DEBRIS-FLOW INITIATION THROUGH IN-SITU EXPERIMENTS.APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH,17(4),7573-7589.
MLA Zhong, W.,et al."ANALYSIS OF THE CORRELATION BETWEEN FRACTAL DIMENSION OF GRAVELLY SOIL AND DEBRIS-FLOW INITIATION THROUGH IN-SITU EXPERIMENTS".APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH 17.4(2019):7573-7589.

入库方式: OAI收割

来源:成都山地灾害与环境研究所

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