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Simulation Analysis of Debris Flow Formation in Weak Cemented Aquifer Development Roadway
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Qia ZHAO1, 2, 3
Mining Research and Development | 2025, 45(4) : 120 - 127
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Mining Research and Development | 2025, 45(4): 120-127
Simulation Analysis of Debris Flow Formation in Weak Cemented Aquifer Development Roadway
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Qia ZHAO1, 2, 3
Affiliations
  • 1.State Key Laboratory of Comprehensive Utilization of Low-grade Refractory Gold Ores, Shanghang, Fujian 364204, China
  • 2.Zijin Mining Group Co., Ltd., Shanghang, Fujian 364200, China
  • 3.Zijin(Changsha) Engineering Technology Co., Ltd., Changsha, Hunan 410036, China
Published: 2025-04-25
Outline
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In order to study the mechanism of debris flow in the underground development project of weak cemented aquifer, the weak cemented sandstone of a mine in Xinjiang was taken as the research object, and its cementation characteristics and water characteristics were analyzed. The mathematical models of porosity, expansion rate and permeability were used to obtain the permeability of weak cemented aquifer under different expansion rates. On this basis, the fluid-solid coupling model was used to analyze the changes of surrounding plastic zone and seepage field in the process of water expansion of surrounding rock of roadway loose circle under different buried depth conditions.The research shows that the water expansion of surrounding rock will increase the permeability of aquifer and improve its permeability. When the expansion rate of surrounding rock increases to 30%, the unit water inflow after roadway excavation will increase by 1.5 to 2.0 times, and with the increase of development depth, the unit water inflow will increase greatly, which will provide sufficient water source for the occurrence of underground debris flow. The strength of weak cemented siltstone is low, and it is easy to form a plastic failure zone on the tunnel face of the development project. With the increase of the development depth, the plastic failure of the tunnel face is greater, and it is easy to collapse and decompose into a source under the condition of groundwater erosion and scour. The stability of surrounding rock in the underground fracture development area is poor, the groundwater seepage channel is smooth and the supply is sufficient. It is easy to expand, collapse and decompose under the action of groundwater, and it is carried by groundwater to form debris flow, which is the key area of underground debris flow. The research results are helpful to further reveal the formation mechanism of debris flow in the underground development project of weak cemented aquifer.

Weak cemented aquifer  /  Underground debris flow  /  Expansion rate  /  Permeability  /  Unit water inflow
赵恰. 弱胶结含水层开拓巷道泥石流形成模拟分析. 矿业研究与开发, 2025 , 45 (4) : 120 -127 .
Qia ZHAO. Simulation Analysis of Debris Flow Formation in Weak Cemented Aquifer Development Roadway[J]. Mining Research and Development, 2025 , 45 (4) : 120 -127 .
Year 2025 volume 45 Issue 4
54
28
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Article Info
  • Receive Date:2024-07-25
  • Online Date:2026-10-30
  • Published:2025-04-25
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  • Received:2024-07-25
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Affiliations
    1.State Key Laboratory of Comprehensive Utilization of Low-grade Refractory Gold Ores, Shanghang, Fujian 364204, China
    2.Zijin Mining Group Co., Ltd., Shanghang, Fujian 364200, China
    3.Zijin(Changsha) Engineering Technology Co., Ltd., Changsha, Hunan 410036, China
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表12种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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