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A model of groundwater seepage and heat transfer for single-well ground source heat pump systems

机译:单井地源热泵系统的地下水渗流与传热模型

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摘要

In China, for the limitation of land, many buildings intending to utilize ground source heat pump systems install "single-well" systems, which drill only one well for both the pumping and reinjection of the groundwater. A model of groundwater seepage and heat transfer for single-well ground source heat pump systems has been established and validated against the experiment conducted in Denmark. In a unitary homogenous confined aquifer, the analytic seepage solution has been derived. Moreover, equations of steady drawdown, seepage velocity, quasi-steady time and hydraulic effective radius are achieved. Results show that groundwater seepage can achieve steady state quickly. In addition, the thermal performance of groundwater and aquifer on a case study in Beijing, China has been simulated. The simulation indicates that the large thermal effective radius (far to 40 m), which is much larger than that of ground-coupled heat pump, makes one single-well accommodate large space heating and cooling loads.
机译:在中国,由于土地的限制,许多打算利用地源热泵系统的建筑物都安装了“单井”系统,该系统仅钻一口井用于抽水和回注地下水。建立了单井地面源热泵系统的地下水渗流和传热模型,并根据丹麦进行的实验进行了验证。在单一的均质承压含水层中,已经得出了解析渗流解。此外,还获得了稳定降水,渗流速度,准稳定时间和水力有效半径的方程。结果表明,地下水渗流可以迅速达到稳态。此外,以中国北京为例,对地下水和含水层的热力性能进行了模拟。仿真表明,大的热有效半径(远至40 m)远大于地面耦合热泵的热有效半径,使一口单井可容纳较大的空间供热和制冷负荷。

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