CIESC Journal ›› 2021, Vol. 72 ›› Issue (8): 4134-4145.DOI: 10.11949/0438-1157.20201651

• Fluid dynamics and transport phenomena • Previous Articles     Next Articles

Heat transfer characteristics of coaxial tubes type deep borehole heat exchanger in water-rich geothermal reservoir

Jiuchen MA1,2,3(),Feiyu YI1,3,Qiuli ZHANG1,3,Yu WANG1,2,3   

  1. 1.School of Energy and Safety Engineering, Tianjin Chengjian University, Tianjin 300384, China
    2.Key Laboratory for Efficient Use of Low and Medium Grade Energy, Ministry of Education, Tianjin University, Tianjin 300072, China
    3.Research Center for Efficient Utilization Technology of Geothermal Energy, Tianjin Chengjian University, Tianjin 300384, China
  • Received:2020-11-16 Revised:2021-02-12 Online:2021-08-05 Published:2021-08-05
  • Contact: Jiuchen MA

富水型热储层深井套管式换热器传热特性研究

马玖辰1,2,3(),易飞羽1,3,张秋丽1,3,王宇1,2,3   

  1. 1.天津城建大学能源与安全工程学院,天津 300384
    2.天津大学中低温热能高效利用教育部重点实验室,天津 300072
    3.天津城建大学地热高效利用技术研究中心,天津 300384
  • 通讯作者: 马玖辰
  • 作者简介:马玖辰(1980—),男,博士,副教授,thermaltju@163.com
  • 基金资助:
    国家自然科学基金项目(41402228);天津市自然科学基金项目(19JCTPJC48100);国家级大学生创新项目(202010792003)

Abstract:

According to the operation principle of the coaxial tubes type deep borehole heat exchanger (DBHE), a three-dimensional unsteady state heat transfer model coupled inside and outside of the borehole was established, based upon hydrogeological conditions of water-rich hot reservoirs with the buried depth of 1000—3000 m in Bohai Basin. The transient analytical solutions were obtained by applying Laplace and Fourier transform methods to calculate the vertical temperature profiles in the inlet (outlet) pipe and the grout of the DBHE and the excess temperature in aquifers. The mathematical model and the analytical solutions were validated by the experimental data determined from a demonstration project and the numerical simulation of the finite volume method (FVM). Based on the dual-continuum spatial coupling approach, the influence was performed to examine the seepage process of underground water on the heat transfer performance of the DBHE in water-rich hot reservoirs. The simulated calculation indicates that the average heat exchange capacity increment of the DBHE is up to 55 kW, when the quantity of the circulating water is stable at 30 m3/h and the Darcy velocity of underground water increases from 0 to 5×10-6 m/s in water-rich hot reservoirs. However, the average heat exchange capacity increases 34 kW meanwhile the circulating pump power consumption increases 20.6 kW, ignoring the seepage process, when the quantity of the circulating water is enhanced from 30 m3/h to 60 m3/h. Studies have shown that as the seepage velocity increases, the heat transfer mechanism in the thermal reservoir changes, thereby enhancing the heat transfer process of the deep well heat exchanger; at the same time, it reduces the influence of the circulating water flow on the heat transfer performance of the deep well heat exchanger.

Key words: deep borehole heat exchanger, water-rich geothermal reservoir, heat transfer, numerical analysis, computer simulation, seepage process

摘要:

基于所建立的深井套管式换热器井孔内、外非稳态传热模型,推导得到富水型热储层地下水渗流作用下深井换热器进(出)水管、固井水泥温度以及热储层过余温度的瞬态解析解。以示范工程现场监测数据与有限体积法数值计算结果为验证依据,探究热储层中渗流过程对于深井换热器传热特性的影响。计算得到,当深井换热器循环水量稳定在30 m3/h时,热储层中达西流速由0提高到5×10-6 m/s时,平均换热量增大55 kW。然而在忽略热储层中渗流过程时,循环水量由30 m3/h提高到60 m3/h,平均换热量增大34 kW,循环水泵耗功提高20.6 kW。研究表明:随着渗流速度的增大,热储层中的传热机制发生改变,从而强化深井换热器的传热过程;同时降低了循环水流量对于深井换热器换热性能的影响程度。

关键词: 深井换热器, 富水型热储层, 传热, 数值分析, 计算机模拟, 渗流过程

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