The Seepage Evolution Mechanism of Variable Mass of Broken Rock in Karst Collapse Column under the Influence of Mining Stress

When the collapse column of overburden is disturbed by the working face, the grain loss in the karst collapse column occurs by the dissolution and corrosion of groundwater, thereby inducing the water inrush disaster. The test samples are prepared based on the fractal theory and the Talbol grading th...

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Main Authors: Li Xiao-Lei, Li Xin-Lei, Wang Yue, Peng Wei-Hang, Fan Xuan, Cao Zheng-Zheng, Liu Rui-Fu
Format: Article
Language:English
Published: Wiley 2023-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2023/7256937
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author Li Xiao-Lei
Li Xin-Lei
Wang Yue
Peng Wei-Hang
Fan Xuan
Cao Zheng-Zheng
Liu Rui-Fu
author_facet Li Xiao-Lei
Li Xin-Lei
Wang Yue
Peng Wei-Hang
Fan Xuan
Cao Zheng-Zheng
Liu Rui-Fu
author_sort Li Xiao-Lei
collection DOAJ
description When the collapse column of overburden is disturbed by the working face, the grain loss in the karst collapse column occurs by the dissolution and corrosion of groundwater, thereby inducing the water inrush disaster. The test samples are prepared based on the fractal theory and the Talbol grading theory, and the seepage evolution law of fractured rock in collapse column under triaxial stress is studied, by employing the triaxial seepage test equipment. Besides, the seepage mechanics model of broken rock is established and calculated in the COMSOL Multiphysics, and the water-conducting channel under mass loss condition in the collapse column is further elucidated. The research results indicate that the loss ratio of mass is inversely proportional to the Talbol power index, and grain mass loss rate increases with the decrease of the Talbol power index. During the infiltration process, the evolution of pore structure is related with grain size distribution. With the increase of the Talbol power index, the overall porosity increases. Grain loss is an internal factor in seepage loss stability. Flow speed is accelerating, and seepage pathways are communicated with each other to induce the water inrush disaster.
format Article
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institution Kabale University
issn 1468-8123
language English
publishDate 2023-01-01
publisher Wiley
record_format Article
series Geofluids
spelling doaj-art-5d04dcc81b6c4eccabefeec1332eb8382025-02-03T06:47:16ZengWileyGeofluids1468-81232023-01-01202310.1155/2023/7256937The Seepage Evolution Mechanism of Variable Mass of Broken Rock in Karst Collapse Column under the Influence of Mining StressLi Xiao-Lei0Li Xin-Lei1Wang Yue2Peng Wei-Hang3Fan Xuan4Cao Zheng-Zheng5Liu Rui-Fu6Zhaogu No.2 MineZhaogu No.2 MineHenan Key Laboratory of Underground Engineering and Disaster PreventionSchool of Physics & Electronic Information EngineeringHenan Key Laboratory of Underground Engineering and Disaster PreventionHenan Key Laboratory of Underground Engineering and Disaster PreventionStructural and Fire Safety EngineeringWhen the collapse column of overburden is disturbed by the working face, the grain loss in the karst collapse column occurs by the dissolution and corrosion of groundwater, thereby inducing the water inrush disaster. The test samples are prepared based on the fractal theory and the Talbol grading theory, and the seepage evolution law of fractured rock in collapse column under triaxial stress is studied, by employing the triaxial seepage test equipment. Besides, the seepage mechanics model of broken rock is established and calculated in the COMSOL Multiphysics, and the water-conducting channel under mass loss condition in the collapse column is further elucidated. The research results indicate that the loss ratio of mass is inversely proportional to the Talbol power index, and grain mass loss rate increases with the decrease of the Talbol power index. During the infiltration process, the evolution of pore structure is related with grain size distribution. With the increase of the Talbol power index, the overall porosity increases. Grain loss is an internal factor in seepage loss stability. Flow speed is accelerating, and seepage pathways are communicated with each other to induce the water inrush disaster.http://dx.doi.org/10.1155/2023/7256937
spellingShingle Li Xiao-Lei
Li Xin-Lei
Wang Yue
Peng Wei-Hang
Fan Xuan
Cao Zheng-Zheng
Liu Rui-Fu
The Seepage Evolution Mechanism of Variable Mass of Broken Rock in Karst Collapse Column under the Influence of Mining Stress
Geofluids
title The Seepage Evolution Mechanism of Variable Mass of Broken Rock in Karst Collapse Column under the Influence of Mining Stress
title_full The Seepage Evolution Mechanism of Variable Mass of Broken Rock in Karst Collapse Column under the Influence of Mining Stress
title_fullStr The Seepage Evolution Mechanism of Variable Mass of Broken Rock in Karst Collapse Column under the Influence of Mining Stress
title_full_unstemmed The Seepage Evolution Mechanism of Variable Mass of Broken Rock in Karst Collapse Column under the Influence of Mining Stress
title_short The Seepage Evolution Mechanism of Variable Mass of Broken Rock in Karst Collapse Column under the Influence of Mining Stress
title_sort seepage evolution mechanism of variable mass of broken rock in karst collapse column under the influence of mining stress
url http://dx.doi.org/10.1155/2023/7256937
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