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Visualized Experimental Study on the Frozen Seepage Flow Law Through Rock Fractures Under Low Temperature
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Xiaoliang YANG1, 2, Yunfeng WANG3, Jianlong SHENG1, 2, Xin ZHOU1, 2, Nan WANG4, Wen ZHOU5
Mining Research and Development | 2025, 45(7) : 218 - 226
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Mining Research and Development | 2025, 45(7): 218-226
Visualized Experimental Study on the Frozen Seepage Flow Law Through Rock Fractures Under Low Temperature
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Xiaoliang YANG1, 2, Yunfeng WANG3, Jianlong SHENG1, 2, Xin ZHOU1, 2, Nan WANG4, Wen ZHOU5
Affiliations
  • 1.School of Resources and Environmental Engineering, Wuhan University of Science and Technology, Wuhan, Hubei 430081, China
  • 2.Hubei Key Laboratory of Efficient Utilization and Blocking of Metallurgical Mineral Resources, Wuhan, Hubei 430081, China
  • 3.Pinghu Municipal Bureau of Water Resources, Pinghu, Zhejiang 314200, China
  • 4.Electric Power Research Institute, State Grid Hubei Electric Power Co., Ltd., Wuhan, Hubei 430077, China
  • 5.Huanglongtan Hydropower Plant, State Grid Hubei Electric Power Co.,Ltd., Shiyan, Hubei 442000, China
Published: 2025-07-25
Outline
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Both rock slope instability and tunnel collapse disasters in cold regions are related to the frozen seepage flow in rock fractures. In order to explore the evolution mechanism of the frozen seepage flow in rock fractures at low temperature, a visualized experiment platform for frozen seepage flow in rock fractures under low temperature conditions was developed, and experiments of low temperature frozen seepage flow in rock fractures under different flow conditions were carried out. Based on the image-processing technology, the dynamic development process of liquid-ice phase transition was quantified, then the relationships between the liquid-ice phase transition and the frozen seepage flow properties were analyzed. The results show that due to the difference in heat exchange intensity between liquid phase and fracture surfaces, the liquid phase is frozen firstly in the upper and lower regions of fracture outlet in the frozen seepage flow process. With the development of frozen seepage flow, the areas of ice phase increase gradually, and the seepage channel decreases accordingly, which results in the increase of liquid phase velocity and an intensification of thermal convection intensity under constant flow conditions, so that the ablation phenomenon occurs at the convex places of the ice phase on both sides of the fracture. When the frozen seepage flow reaches a steady state, the Reynolds number of liquid phase flow is obviously greater than its initial value, and the pressure gradient is roughly linear with the flow. Furthermore, the larger flow has an obvious inhibitory effect on the freezing rate of the ice phase.

Frozen seepage flow  /  Visualized experiment  /  Liquid-ice phase transition  /  Ablation phenomenon  /  Cold region engineering
杨晓亮, 汪云峰, 盛建龙, 周新, 王楠, 周文. 低温作用下岩体裂隙冻结渗流规律可视化试验研究. 矿业研究与开发, 2025 , 45 (7) : 218 -226 .
Xiaoliang YANG, Yunfeng WANG, Jianlong SHENG, Xin ZHOU, Nan WANG, Wen ZHOU. Visualized Experimental Study on the Frozen Seepage Flow Law Through Rock Fractures Under Low Temperature[J]. Mining Research and Development, 2025 , 45 (7) : 218 -226 .
Year 2025 volume 45 Issue 7
58
22
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Article Info
  • Receive Date:2024-09-12
  • Online Date:2026-10-28
  • Published:2025-07-25
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History
  • Received:2024-09-12
Funding
Affiliations
    1.School of Resources and Environmental Engineering, Wuhan University of Science and Technology, Wuhan, Hubei 430081, China
    2.Hubei Key Laboratory of Efficient Utilization and Blocking of Metallurgical Mineral Resources, Wuhan, Hubei 430081, China
    3.Pinghu Municipal Bureau of Water Resources, Pinghu, Zhejiang 314200, China
    4.Electric Power Research Institute, State Grid Hubei Electric Power Co., Ltd., Wuhan, Hubei 430077, China
    5.Huanglongtan Hydropower Plant, State Grid Hubei Electric Power Co.,Ltd., Shiyan, Hubei 442000, 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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