穆玄,裴鹏,周鑫,等. 岩溶构造对地埋管群换热效率影响数值模拟研究[J]. 煤田地质与勘探,2022,50(10):131−139. DOI: 10.12363/issn.1001-1986.21.09.0513
引用本文: 穆玄,裴鹏,周鑫,等. 岩溶构造对地埋管群换热效率影响数值模拟研究[J]. 煤田地质与勘探,2022,50(10):131−139. DOI: 10.12363/issn.1001-1986.21.09.0513
MU Xuan,PEI Peng,ZHOU Xin,et al. Numerical simulation of the influence of karst structure on heat transfer efficiency of buried pipeline group[J]. Coal Geology & Exploration,2022,50(10):131−139. DOI: 10.12363/issn.1001-1986.21.09.0513
Citation: MU Xuan,PEI Peng,ZHOU Xin,et al. Numerical simulation of the influence of karst structure on heat transfer efficiency of buried pipeline group[J]. Coal Geology & Exploration,2022,50(10):131−139. DOI: 10.12363/issn.1001-1986.21.09.0513

岩溶构造对地埋管群换热效率影响数值模拟研究

Numerical simulation of the influence of karst structure on heat transfer efficiency of buried pipeline group

  • 摘要: 地埋管是岩体热泵系统与地层直接交换冷热量的部分。岩溶地区含水构造复杂多样,对地埋管群换热储热有明显影响。对27根垂直地埋管群在无岩溶构造、岩溶裂隙构造、岩溶管道构造以及混合岩溶构造4种地质构造类型中的换热过程进行了模拟,并对比了岩体内温度场、埋管出口水温、热泵机组制冷系数(COP)以及单位井深换热量等参数的变化。结果表明:在制冷工况下,不同模型温度场中,岩体中存在岩溶裂隙构造或岩溶管道构造时,地下水流动对岩体热堆积有明显缓解作用;岩溶导水构造与地埋管的距离也是重要影响因素。模型运行到第1个制冷周期末期时,含岩溶裂隙构造岩体和含岩溶管道构造岩体的进出口水温差比混合岩溶构造岩体的分别升高了0.87、4.00 K;无岩溶构造岩体进出口水温差比混合岩溶构造岩体的下降了1.16 K。无岩溶构造岩体、岩溶裂隙构造岩体、岩溶管道构造岩体和混合岩溶构造岩体的COP分别为7.2、7.4、7.8和7.3;单位井深换热量分别为64.1、90.3、130.7和79.1 W/m。研究结果表明,岩溶导水构造明显增强了地埋管群的换热效率,不同的地质构造类型对地埋管换热效率的影响也不一样。

     

    Abstract: The buried pipeline is the part where the rock mass heat pump system performs direct heat transfer with the ground. The water-bearing structure in the karst area is complex and diverse, which has a significant impact on the heat transfer and storage of the buried pipeline group. Herein, the heat transfer process of a group of 27 vertical buried pipelines in four geological structure types was simulated, including the non-karst structure, fractured karst structure, karst conduit structure and mixed karst structure. Meanwhile, comparison was made for the change of parameters, such as the temperature field in the rock mass, the outlet water temperature of buried pipeline, the coefficient of performance (COP) of heat pump unit, and the heat change in unit well depth. The results show that the flow of groundwater can significantly relieve the heat build-up in the rock mass where fractured karst structure and karst conduit structure exist in different model temperature fields under the refrigeration conditions, and the distance between the karst water-conducting structure and the buried pipeline is also an important influencing factor. When the model operates to the end of the first refrigeration cycle, the temperature difference between the inlet and outlet of rock mass in fractured karst structure and karst conduit structure is 0.87 K and 4.00 K higher than that in mixed karst structure respectively, while the temperature difference between the inlet and outlet of rock mass in non-karst structure is 1.16 K lower than that in mixed karst structure. The COPs of rock mass in non-karst structure, fractured karst structure, karst conduit structure, and mixed karst structure are 7.2, 7.4, 7.8 and 7.3 respectively. Besides, the heat transfer per well depth is 64.1, 90.3, 130.7 and 79.1 W/m respectively. The research results show that the karst water-conducting structure significantly enhances the heat transfer efficiency of the buried pipeline group, and different geological structure types have different effects on the heat transfer efficiency of the buried pipeline.

     

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