中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Evolution mechanism study of flow slide catastrophes in large waste dumps at the Nanfen iron mine

文献类型:期刊论文

作者Wang, Hai-bin1; Yan, Fei1; Li, Xiao-chun1; Mi, Zi-jun2; Li, Xiang-ming4; Wang, Shao-quan3
刊名BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT
出版日期2020-06-18
页码15
关键词Single-high terrace waste dump Chair-shaped gully foundation Retrogressive landslide Freeze-thaw cycle Soil particle transfer effect Lubrication effect with sluggish water
ISSN号1435-9529
DOI10.1007/s10064-020-01881-0
英文摘要In this study, we applied historical matching and self-analogism methods, as well as laboratory physical-mechanics tests, to study the evolution mechanism of the collapse-slide-flow slide at the waste dump on the slope of the chair-shaped gully, as well as the evolution mechanism of the subsequent debris flow. Our analyses indicate that (1) an excessive fine particle content results in a relatively large specific surface area and further enhances water retention performance, (2) rainfall infiltration was concentrated at the contact surface between chair-shaped valley and bottom of the bulk, and (3) with high-intensity continuous rock discharge during the snow and ice period, a mixed frozen body of ice waste stone particles forms, such that ice melting in the spring leads to a sudden change in the shear strength near the contact interface between the waste rock pile foundation and the bulk. Dual effects, essential internal factors, i.e., shear strength and water retention, induced external factors, i.e., ice-freezing skeleton-melting structure collapse, and the chimney effect drive the slope toe of the waste dump. The weak interface of the Quaternary base gradually penetrates the interior of the dumping body, beginning to form from a single-stage traction landslide and evolving into a multi-stage rotary landslide. The sliding surface is characterized by the shear outlet at the front edge of the slope toe, quaternary base interface, and nearly vertical and steep trailing edge. During this movement, gasification on the sliding surface and particle rotation lead to long run-out sliding, which magnifies the scope of disaster.
资助项目National Natural Science Foundation of China[51674238]
WOS研究方向Engineering ; Geology
语种英语
WOS记录号WOS:000543628500002
出版者SPRINGER HEIDELBERG
源URL[http://119.78.100.198/handle/2S6PX9GI/24435]  
专题中科院武汉岩土力学所
通讯作者Yan, Fei
作者单位1.Chinese Acad Sci, State Key Lab Geomech & Geotech Engn, Inst Rock & Soil Mech, Wuhan 430071, Peoples R China
2.Min Co, Taiyuan Iron & Steel Grp Co Ltd, Taiyuan 030027, Peoples R China
3.Northern Engn & Technol Corp, MCC, Dalian 114009, Peoples R China
4.Min Co, Benxi Iron & Steel Grp Co Ltd, Benxi 030027, Peoples R China
推荐引用方式
GB/T 7714
Wang, Hai-bin,Yan, Fei,Li, Xiao-chun,et al. Evolution mechanism study of flow slide catastrophes in large waste dumps at the Nanfen iron mine[J]. BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT,2020:15.
APA Wang, Hai-bin,Yan, Fei,Li, Xiao-chun,Mi, Zi-jun,Li, Xiang-ming,&Wang, Shao-quan.(2020).Evolution mechanism study of flow slide catastrophes in large waste dumps at the Nanfen iron mine.BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT,15.
MLA Wang, Hai-bin,et al."Evolution mechanism study of flow slide catastrophes in large waste dumps at the Nanfen iron mine".BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT (2020):15.

入库方式: OAI收割

来源:武汉岩土力学研究所

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