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A case study on the characteristics of footwall ground deformation and movement and their mechanisms
Xia, Kaizong1,2; Chen, Congxin1,2; Yang, Kuoyu1,2; Zhang, Haina1,2; Pang, Hansong1,2
刊名NATURAL HAZARDS
2020-08-10
页码39
关键词Metal mine Underground orebody excavation Ground movement Break angle Discontinuity
ISSN号0921-030X
DOI10.1007/s11069-020-04204-4
英文摘要The characteristics of ground deformation induced by the excavation of underground orebodies are summarized based on an analysis of over 10 years of deformation data recorded in the eastern mining area of the Chengchao mine in China. These data are combined with laws governing the development of ground-surface cracking and collapse to study the corresponding failure mechanism. The results indicate that the ground deformation in most mining-affected areas increases at a low rate of acceleration. Furthermore, the displacement-time curves are exponential in nature (that is, the relationship between displacement and time can be expressed using an exponent). Curves representing the ratio of the horizontal: vertical displacement over time show different behaviors including convergence, fluctuation, increase, fall-back, exponential, and linear trends. The originally designed scope of the ground movement is significantly smaller than the scope of the actual ground movement suggested by the in situ deformation data (the difference in movement angle amounts to 18 degrees; the difference in break angle to 20 degrees). After rapidly decreasing in the initial mining stage, the break angle remained constant (similar to 50 degrees) for a long period of time. The surrounding rock mass conformed to a failure model in which the rock mass topples toward the mined-out area leading to failure surfaces being formed in the deep parts of the rock mass. The inclination angles of these failure surfaces are different in different excavation-affected areas. The excavation-affected area in which the failure surfaces occur can be viewed as a large-scale surface-cracking zone. Outside this zone, small-scale surface cracking can be observed and this area can be viewed as a small-scale surface-cracking zone. In the area investigated, the occurrence of ground movement that is significantly larger than predicted is attributed to the combined effect of engineering-geological conditions, hydrogeological conditions, and the burial depth and geometric configuration of the underground orebodies of the mine. More specifically, the surrounding rock mass is continuously subjected to large-scale unloading during the process of karst collapse (during the construction stage) and ground collapse (during the mining stage) of the mine. Then, the surrounding rock mass progressively undergoes toppling failure and becomes unstable, making the region subjected to ground movement progressively extend outwards.
资助项目Young Scholar Fund of National Natural Science Foundation of China[11602284] ; Young Scholar Fund of National Natural Science Foundation of China[41602325]
WOS研究方向Geology ; Meteorology & Atmospheric Sciences ; Water Resources
语种英语
出版者SPRINGER
WOS记录号WOS:000558136800003
内容类型期刊论文
源URL[http://119.78.100.198/handle/2S6PX9GI/24682]  
专题中科院武汉岩土力学所
通讯作者Xia, Kaizong; Yang, Kuoyu
作者单位1.Chinese Acad Sci, State Key Lab Geomech & Geotech Engn, Inst Rock & Soil Mech, Wuhan 430071, Hubei, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Xia, Kaizong,Chen, Congxin,Yang, Kuoyu,et al. A case study on the characteristics of footwall ground deformation and movement and their mechanisms[J]. NATURAL HAZARDS,2020:39.
APA Xia, Kaizong,Chen, Congxin,Yang, Kuoyu,Zhang, Haina,&Pang, Hansong.(2020).A case study on the characteristics of footwall ground deformation and movement and their mechanisms.NATURAL HAZARDS,39.
MLA Xia, Kaizong,et al."A case study on the characteristics of footwall ground deformation and movement and their mechanisms".NATURAL HAZARDS (2020):39.
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