Spatial evolution mechanism of landslide in loess gully basement dump

External dump is the inevitable outcome of surface mining. Because of the special landform, some open-pit coal mines in the middle and west of China build their dump sites on the loess base with gully development, forming the loess gully base dump with weak basement and extremely complex morphology....

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Main Authors: WANG Dong, ZHANG Yan, LI Guanghe, XING Xiaoyu
Format: Article
Language:zho
Published: Editorial Department of Coal Science and Technology 2023-03-01
Series:Meitan kexue jishu
Subjects:
Online Access:http://www.mtkxjs.com.cn/article/doi/10.13199/j.cnki.cst.2021-0749
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author WANG Dong
ZHANG Yan
LI Guanghe
XING Xiaoyu
author_facet WANG Dong
ZHANG Yan
LI Guanghe
XING Xiaoyu
author_sort WANG Dong
collection DOAJ
description External dump is the inevitable outcome of surface mining. Because of the special landform, some open-pit coal mines in the middle and west of China build their dump sites on the loess base with gully development, forming the loess gully base dump with weak basement and extremely complex morphology. Its stability will become an important factor affecting the safe and efficient production of opencast coal mine. As a result, to study in Loess Gully basal dump deformation destruction of spatial evolution, in Heidaigou dump as an engineering background, based on discontinuous structural plane theory and strength reduction theory, considering the gnawing and climbing effect of undulating structural plane, the failure mechanism of loess gully basement dump was analyzed. Using FLAC3D numerical simulation method, the spatial evolution process of the deformation and failure of the dump was studied, the landslide mode and landslide area of the loess gully basement dump were determined by analyzing the maximum displacement cloud map of each section and the position of the deformation zone during critical instability. The results show that the loess gully basement can be regarded as an undulation and unfilled structural plane, and the gnawing and climbing effect will be formed under the loading and shear of the dump, that is, the irregular surface landslide of the raised shear part will occur in the dump. T Under the dual influence of the dumping load and the morphology of the gully base, the upper rock mass of the slope deforms first, and then the middle and lower rock mass deforms under the extrusion. The deformation zones located on both sides of the north-south central axis extend to the Northern Slope bottom, forming a quasi-ellipsoid deformation zone, and finally evolves into a push landslide. The research results can provide technical reference for landslide warning and slope treatment of Heidaigou dump, and provide reference for slope stability study of similar dump.
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spelling doaj.art-8ed97880e64840129e2d38bf2f71f30a2023-05-30T08:54:35ZzhoEditorial Department of Coal Science and TechnologyMeitan kexue jishu0253-23362023-03-01513778410.13199/j.cnki.cst.2021-07492021-0749Spatial evolution mechanism of landslide in loess gully basement dumpWANG DongZHANG YanLI GuangheXING XiaoyuExternal dump is the inevitable outcome of surface mining. Because of the special landform, some open-pit coal mines in the middle and west of China build their dump sites on the loess base with gully development, forming the loess gully base dump with weak basement and extremely complex morphology. Its stability will become an important factor affecting the safe and efficient production of opencast coal mine. As a result, to study in Loess Gully basal dump deformation destruction of spatial evolution, in Heidaigou dump as an engineering background, based on discontinuous structural plane theory and strength reduction theory, considering the gnawing and climbing effect of undulating structural plane, the failure mechanism of loess gully basement dump was analyzed. Using FLAC3D numerical simulation method, the spatial evolution process of the deformation and failure of the dump was studied, the landslide mode and landslide area of the loess gully basement dump were determined by analyzing the maximum displacement cloud map of each section and the position of the deformation zone during critical instability. The results show that the loess gully basement can be regarded as an undulation and unfilled structural plane, and the gnawing and climbing effect will be formed under the loading and shear of the dump, that is, the irregular surface landslide of the raised shear part will occur in the dump. T Under the dual influence of the dumping load and the morphology of the gully base, the upper rock mass of the slope deforms first, and then the middle and lower rock mass deforms under the extrusion. The deformation zones located on both sides of the north-south central axis extend to the Northern Slope bottom, forming a quasi-ellipsoid deformation zone, and finally evolves into a push landslide. The research results can provide technical reference for landslide warning and slope treatment of Heidaigou dump, and provide reference for slope stability study of similar dump.http://www.mtkxjs.com.cn/article/doi/10.13199/j.cnki.cst.2021-0749open pit coal mineloess gullydumpslope stabilitymechanism of spatial evolution
spellingShingle WANG Dong
ZHANG Yan
LI Guanghe
XING Xiaoyu
Spatial evolution mechanism of landslide in loess gully basement dump
Meitan kexue jishu
open pit coal mine
loess gully
dump
slope stability
mechanism of spatial evolution
title Spatial evolution mechanism of landslide in loess gully basement dump
title_full Spatial evolution mechanism of landslide in loess gully basement dump
title_fullStr Spatial evolution mechanism of landslide in loess gully basement dump
title_full_unstemmed Spatial evolution mechanism of landslide in loess gully basement dump
title_short Spatial evolution mechanism of landslide in loess gully basement dump
title_sort spatial evolution mechanism of landslide in loess gully basement dump
topic open pit coal mine
loess gully
dump
slope stability
mechanism of spatial evolution
url http://www.mtkxjs.com.cn/article/doi/10.13199/j.cnki.cst.2021-0749
work_keys_str_mv AT wangdong spatialevolutionmechanismoflandslideinloessgullybasementdump
AT zhangyan spatialevolutionmechanismoflandslideinloessgullybasementdump
AT liguanghe spatialevolutionmechanismoflandslideinloessgullybasementdump
AT xingxiaoyu spatialevolutionmechanismoflandslideinloessgullybasementdump