孙婉. 地下水渗流与地源热泵热量运移耦合模拟[J]. 太阳能学报, 2021, 42(5): 16-23. DOI: 10.19912/j.0254-0096.tynxb.2019-0019
引用本文: 孙婉. 地下水渗流与地源热泵热量运移耦合模拟[J]. 太阳能学报, 2021, 42(5): 16-23. DOI: 10.19912/j.0254-0096.tynxb.2019-0019
SUN Wan. COUPLING SIMULATION OF GROUNDWATER SEEPAGE AND HEAT TRANSFER OF GROUND SOURCE HEAT PUMP[J]. Acta Energiae Solaris Sinica, 2021, 42(5): 16-23. DOI: 10.19912/j.0254-0096.tynxb.2019-0019
Citation: SUN Wan. COUPLING SIMULATION OF GROUNDWATER SEEPAGE AND HEAT TRANSFER OF GROUND SOURCE HEAT PUMP[J]. Acta Energiae Solaris Sinica, 2021, 42(5): 16-23. DOI: 10.19912/j.0254-0096.tynxb.2019-0019

地下水渗流与地源热泵热量运移耦合模拟

COUPLING SIMULATION OF GROUNDWATER SEEPAGE AND HEAT TRANSFER OF GROUND SOURCE HEAT PUMP

  • 摘要: 为准确模拟不同地下水径流条件下地源热泵系统地埋管换热区地温场变化特征、系统换热性能变化规律以及由此而产生的热量堆积效应等问题,以同济大学生态园试验场地为研究对象,采用理论分析及数值模拟计算为主要手段,建立了水流、介质、热量三场耦合的数值模拟模型。结果表明:随着地下水渗流速度的增大,热量逐渐向地下水流动方向偏移,粉砂层扩散偏移幅度小于细砂层,细砂层小于粗砂层。0~80 m深度,土层热量堆积明显,处于含水层深度范围内的80~100 m深度土层热量堆积越少。随着地下水渗流流速的增大,地埋管换热器单位深度换热功率逐渐增大,两者为线型关系,地下水渗流流速为1.33×10-4、6.30×10-4及1.27×10-3m/d时地埋管换热器换热功率增幅分别为0.53%、1.31%及2.43%。

     

    Abstract: In order to accurately simulate the variation characteristics of geothermal field in heat exchange zone,variation of heat transfer performance of the system and heat accumulation effect of ground source heat pump under different groundwater seepage conditions,the experimental site of Tongji University Eco-Park was taken as the research object,a numerical simulation model of three fields coupled with water,medium and heat is established by the theoretical analysis and numerical simulation. The results show that with the increase of seepage velocity of groundwater,the heat gradually shifts to the direction of groundwater flow. The diffusion migration amplitude of silt layer is smaller than that of fine sand layer,and fine sand layer is smaller than that of coarse sand layer. At the depth of 0-80 m,the heat accumulation of soil layer is obvious,and the heat accumulation of soil layer at the depth of 80-100 m is less. With the increase of groundwater seepage velocity,the heat transfer power per unit depth of buried tube heat exchanger increases gradually,and the relationship between them is linear. The heat transfer power increases by 0.53%,1.31% and 2.43% respectively when the groundwater seepage velocity is 1.33×10-4,6.30×10-4 and 1.27×10-3 m/d.

     

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