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Study on the Effective Thermal Conductivity Model of Fractured Rock Mass Under Normal Stress
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Jianlong SHENG1, 2, Bing WU1, 2, Nan WANG3, Xiaoliang YANG1, 2, Yihong YANG1, 2
Mining Research and Development | 2026, 46(1) : 150 - 158
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Mining Research and Development | 2026, 46(1): 150-158
Study on the Effective Thermal Conductivity Model of Fractured Rock Mass Under Normal Stress
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Jianlong SHENG1, 2, Bing WU1, 2, Nan WANG3, Xiaoliang YANG1, 2, Yihong YANG1, 2
Affiliations
  • 1.College of Resources and Environmental Engineering, Wuhan University of Science and Technology, Wuhan, Hubei 430081, China
  • 2.Hubei Key Laboratory of Efficient Utilization and Agglomeration of Metallurgical Mineral Resources, Wuhan, Hubei 430081, China
  • 3.Electric Power Research Institute of State Grid Hubei Electric Power Co., Ltd., Wuhan, Hubei 430077, China
Published: 2026-01-25
Outline
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The temperature field of deep tunnels and the development of deep mineral resources involve the thermal conductivity of rock mass. For the nonlinear change rule of effective thermal conductivity of fractured rock mass under normal stress, based on the two-part Hooke's model and effective thermal conductivity series-parallel theory, a theoretical model of effective thermal conductivity of fractured rock mass under normal stress was established, and the influences of model parameters on the effective thermal conductivity of fractured rock mass under stress were analyzed. Through the numerical simulation results of the change of temperature field in Nigel Tunnel, the reliability in engineering application of the model was verified. The results show that, the theoretical model prediction results are in good agreement with the test data. The effective thermal conductivity of the fractured rock mass in the low stress stage is mainly affected by the soft part of the pore-slit closure, and increases nonlinearly with the increase of the stress. While the effective thermal conductivity of the fractured rock mass in the high stress stage is mainly affected by the hard part of the pore-slit closure, and increases slowly in an approximately linear manner with the increase of the stress. The larger the angle between the fracture surface and the direction of heat transfer, the smaller the effective thermal conductivity of the rock at the same stress, and the higher the degree of non-linearity with the stress change. Comparing the numerical simulation results with the measured data, the thermal conductivity of the intact rock mass is on the large side, the effective thermal conductivity obtained by the stress-independent effective thermal conductivity model is on the small side, and the coupling model of normal stress and thermal conductivity is more in line with the actual measured values.

Fractured rock mass  /  Effective thermal conductivity  /  Two-part Hooke's model  /  Stress  /  Temperature field  /  Numerical simulation
盛建龙, 吴兵, 王楠, 杨晓亮, 杨一宏. 法向应力下的裂隙岩体有效导热系数模型研究. 矿业研究与开发, 2026 , 46 (1) : 150 -158 .
Jianlong SHENG, Bing WU, Nan WANG, Xiaoliang YANG, Yihong YANG. Study on the Effective Thermal Conductivity Model of Fractured Rock Mass Under Normal Stress[J]. Mining Research and Development, 2026 , 46 (1) : 150 -158 .
Year 2026 volume 46 Issue 1
36
11
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Article Info
  • Receive Date:2024-12-24
  • Online Date:2026-10-29
  • Published:2026-01-25
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  • Received:2024-12-24
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Affiliations
    1.College of Resources and Environmental Engineering, Wuhan University of Science and Technology, Wuhan, Hubei 430081, China
    2.Hubei Key Laboratory of Efficient Utilization and Agglomeration of Metallurgical Mineral Resources, Wuhan, Hubei 430081, China
    3.Electric Power Research Institute of State Grid Hubei Electric Power Co., Ltd., Wuhan, Hubei 430077, 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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