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Variation in the temperature field of rocks overlying a high-temperature cavity during underground coal gasification 被引量:7

Variation in the temperature field of rocks overlying a high-temperature cavity during underground coal gasification
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摘要 High temperature affects rocks in a way that changes the physical and mechanical properties of them. The temperature field in rock overlying a high temperature zone has been estimated using experimental research on thermal conductivity of the overlying strata. Numerical analysis software was used to esti- mate rock thermal conductivity at different temperatures. These estimates were then used with COMSOL Multiphysics to perform a numerical analysis with the heat conduction model. The results show that rock thermal conductivity decreases as the temperature increases and that various lithologies show similar behavior. The thermal conductivity of each rock type differs from the others at a given temperature. Exact values for the temperature distribution in the overlying strata during the process of underground coal gasification are obtained from the numerical simulation. The temperature in the rock changes with the height and direction from the gasifier. Temperature gradients vary for different types of rock. This result provides an important reference for further study of the strength of overlying strata subject to the process of underground coal gasification. High temperature affects rocks in a way that changes the physical and mechanical properties of them. The temperature field in rock overlying a high temperature zone has been estimated using experimental research on thermal conductivity of the overlying strata. Numerical analysis software was used to estimate rock thermal conductivity at different temperatures. These estimates were then used with COMSOL Multiphysics to perform a numerical analysis with the heat conduction model. The results show that rock thermal conductivity decreases as the temperature increases and that various lithologies show similar behavior. The thermal conductivity of each rock type differs from the others at a given temperature. Exact values for the temperature distribution in the overlying strata during the process of underground coal gasification are obtained from the numerical simulation. The temperature in the rock changes with the height and direction from the gasifier. Temperature gradients vary for different types of rock. This result provides an important reference for further study of the strength of overlying strata subject to the process of underground coal gasification.
出处 《Mining Science and Technology》 EI CAS 2011年第5期709-713,共5页 矿业科学技术(英文版)
基金 support from the State Key Basic Research Program of China (No. 2010CB226805) the National Natural Science Foundation of China (No. 50874103) the Natural Science Foundation of Jiangsu Province (No. BK2008135) the StateKey Laboratory Program (No. SKLGDUEK0905) the Natural Science Fundsof the Education Department of Anhui Province (No.KJ2009B096Z) the Brain Gain Funds Program of Anhui University of Scienceand Technology (No. 2008yb011)
关键词 StratumThermal conductivityTemperatureSimulation 岩石热导率 温度场 气化温度 煤炭 上覆地层 数值分析 岩石类型 气化过程
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