The Failure Mechanism and Stability of the End Slope of Inclined Composite Coal Seam

In view of the inclined occurrence of coal seam in Heishan open-pit coal mine, in the longitudinal exploitation process of the first mining area, the height of the slope at the west end is increasing, and the occurrence of weak interlayer in the slope is in production. The failure mechanism and stab...

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Autores principales: Haoran Li, Han Du, Runcai Bai, Guangwei Liu, Mingyuan Zhao, Rongzheng Liu
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Publicado: Hindawi Limited 2021
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spelling oai:doaj.org-article:783ab9862cea4ca897e4028cc03c405e2021-11-08T02:35:26ZThe Failure Mechanism and Stability of the End Slope of Inclined Composite Coal Seam1563-514710.1155/2021/2830717https://doaj.org/article/783ab9862cea4ca897e4028cc03c405e2021-01-01T00:00:00Zhttp://dx.doi.org/10.1155/2021/2830717https://doaj.org/toc/1563-5147In view of the inclined occurrence of coal seam in Heishan open-pit coal mine, in the longitudinal exploitation process of the first mining area, the height of the slope at the west end is increasing, and the occurrence of weak interlayer in the slope is in production. The failure mechanism and stability of the end slope of the inclined composite coal seam, which is typical of the West end slope of Heishan open-pit mine, are studied by means of field investigation, theoretical analysis, limit equilibrium analysis, and numerical simulation. The factors affecting the stability of the western side slope and the potential landslide mode are analyzed. The residual thrust method and simplified Bishop method were used to study the stability of two potential landslide modes on the western slope, and the landslide mode, final slope angle, and slope morphology were determined. FLAC3D was used to simulate the western end of the slope, reveal its landslide mechanism, and clarify the evolution law of the slope rock mass displacement. The results show that the landslide mode at the west end of the first mining area is the combined sliding mode of “cutting and bedding.” With the decrease of longitudinal mining depth, the final slope angle functions from 40° to 37°. The stress and strain are concentrated at the weak layer of the coal floor of the western side slope 13-2 and at the foot of the slope. Meanwhile, the failure also occurs inside the slope. The internal cracks connect through the weak layer of the coal floor and slide along the weak layer of the coal floor 13-2. The displacement evolution law of the slope monitoring point shows that the deformation of the slope is mainly horizontal displacement, the maximum displacement deformation is at the foot of the slope, and the degree of displacement deformation of the slope surface is obviously greater than that of the inside of the slope.Haoran LiHan DuRuncai BaiGuangwei LiuMingyuan ZhaoRongzheng LiuHindawi LimitedarticleEngineering (General). Civil engineering (General)TA1-2040MathematicsQA1-939ENMathematical Problems in Engineering, Vol 2021 (2021)
institution DOAJ
collection DOAJ
language EN
topic Engineering (General). Civil engineering (General)
TA1-2040
Mathematics
QA1-939
spellingShingle Engineering (General). Civil engineering (General)
TA1-2040
Mathematics
QA1-939
Haoran Li
Han Du
Runcai Bai
Guangwei Liu
Mingyuan Zhao
Rongzheng Liu
The Failure Mechanism and Stability of the End Slope of Inclined Composite Coal Seam
description In view of the inclined occurrence of coal seam in Heishan open-pit coal mine, in the longitudinal exploitation process of the first mining area, the height of the slope at the west end is increasing, and the occurrence of weak interlayer in the slope is in production. The failure mechanism and stability of the end slope of the inclined composite coal seam, which is typical of the West end slope of Heishan open-pit mine, are studied by means of field investigation, theoretical analysis, limit equilibrium analysis, and numerical simulation. The factors affecting the stability of the western side slope and the potential landslide mode are analyzed. The residual thrust method and simplified Bishop method were used to study the stability of two potential landslide modes on the western slope, and the landslide mode, final slope angle, and slope morphology were determined. FLAC3D was used to simulate the western end of the slope, reveal its landslide mechanism, and clarify the evolution law of the slope rock mass displacement. The results show that the landslide mode at the west end of the first mining area is the combined sliding mode of “cutting and bedding.” With the decrease of longitudinal mining depth, the final slope angle functions from 40° to 37°. The stress and strain are concentrated at the weak layer of the coal floor of the western side slope 13-2 and at the foot of the slope. Meanwhile, the failure also occurs inside the slope. The internal cracks connect through the weak layer of the coal floor and slide along the weak layer of the coal floor 13-2. The displacement evolution law of the slope monitoring point shows that the deformation of the slope is mainly horizontal displacement, the maximum displacement deformation is at the foot of the slope, and the degree of displacement deformation of the slope surface is obviously greater than that of the inside of the slope.
format article
author Haoran Li
Han Du
Runcai Bai
Guangwei Liu
Mingyuan Zhao
Rongzheng Liu
author_facet Haoran Li
Han Du
Runcai Bai
Guangwei Liu
Mingyuan Zhao
Rongzheng Liu
author_sort Haoran Li
title The Failure Mechanism and Stability of the End Slope of Inclined Composite Coal Seam
title_short The Failure Mechanism and Stability of the End Slope of Inclined Composite Coal Seam
title_full The Failure Mechanism and Stability of the End Slope of Inclined Composite Coal Seam
title_fullStr The Failure Mechanism and Stability of the End Slope of Inclined Composite Coal Seam
title_full_unstemmed The Failure Mechanism and Stability of the End Slope of Inclined Composite Coal Seam
title_sort failure mechanism and stability of the end slope of inclined composite coal seam
publisher Hindawi Limited
publishDate 2021
url https://doaj.org/article/783ab9862cea4ca897e4028cc03c405e
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