中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The influence of temporal and spatial variations on phase separation in debris flow deposition

文献类型:期刊论文

作者Wang, Fei1; Wang, Jiading1; Chen, Xiaoqing2; Chen, Jiangang2
刊名LANDSLIDES
出版日期2019-03-01
卷号16期号:3页码:497-514
关键词Debris flow Peak discharge Flow density Experimental analysis Deceleration baffles
ISSN号1612-510X
DOI10.1007/s10346-018-1119-5
通讯作者Wang, Jiading(wangjd@nwu.edu.cn)
英文摘要The phase separation mechanism in a natural debris flow as a solid-liquid mixture is an important aspect in its movement and deposition. In this paper, the relationship between debris flow discharges and densities is studied based on the field observations of the Jiangjia Gully, China. A number of experiments are conducted to study the phase separation mechanism of debris flows, and the characteristics of their depositions over deceleration baffles with varying flow density and bottom slopes. The phase separation mechanism of natural debris flows is analyzed based on the mentioned experimental and field observations. During the decreasing debris flow, the flow density reduces with reduction of the flow discharge, indicating the important role of the flow discharge in changing the flow density as a driving factor. Temporal variations of the debris flow density can have two chronological orders: (a) dilute-viscous-dilute debris flow and (b) viscous-dilute debris flow. The variation order of the flow density has an important influence on the phase separation mechanism and the final deposition morphology. The experimental results show that the bottom slope and the flow density have opposite effects on the phase separation mechanism. Increasing the flow density increases the viscosity of the debris flow, decreasing the phase separation of the solid-liquid mixture. Increasing the bottom slope promotes phase separation by increasing the shear rate inside the debris flow. As a result, the phase separation mechanism of natural debris flow is mostly related to the temporal and spatial variations of the flow pattern and the flow density.
WOS关键词LABORATORY ANALYSIS ; FIELD ; MITIGATION ; VELOCITY ; CHANNEL ; RUNOUT ; SEGREGATION ; MECHANISMS ; INITIATION ; DOLOMITES
资助项目National Natural Science Foundation of China[41630639] ; National Natural Science Foundation of China[41807252] ; National Key Research and Development Plan[2018YFC1504703] ; International Cooperation and Exchange of the National Science Foundation of China[41661144028] ; China Postdoctoral Science Foundation[2018M633558]
WOS研究方向Engineering ; Geology
语种英语
WOS记录号WOS:000461573100004
出版者SPRINGER HEIDELBERG
资助机构National Natural Science Foundation of China ; National Key Research and Development Plan ; International Cooperation and Exchange of the National Science Foundation of China ; China Postdoctoral Science Foundation
源URL[http://ir.imde.ac.cn/handle/131551/25303]  
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Wang, Jiading
作者单位1.Northwest Univ, State Key Lab Continental Dynam, Dept Geol, Xian 710069, Shaanxi, Peoples R China
2.Chinese Acad Sci, CAS Key Lab Mt Hazards & Earth Surface Proc, Inst Mt Hazards & Environm, Chengdu 610041, Sichuan, Peoples R China
推荐引用方式
GB/T 7714
Wang, Fei,Wang, Jiading,Chen, Xiaoqing,et al. The influence of temporal and spatial variations on phase separation in debris flow deposition[J]. LANDSLIDES,2019,16(3):497-514.
APA Wang, Fei,Wang, Jiading,Chen, Xiaoqing,&Chen, Jiangang.(2019).The influence of temporal and spatial variations on phase separation in debris flow deposition.LANDSLIDES,16(3),497-514.
MLA Wang, Fei,et al."The influence of temporal and spatial variations on phase separation in debris flow deposition".LANDSLIDES 16.3(2019):497-514.

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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