Jingjing Wang , Juntao Deng , Jianguo Zheng , Yongtang Yu , Jianmin Zhu , Xin Huang
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引用次数: 0
Abstract
Effectively describing the heat transfer process of ground heat exchangers is crucial for fully utilizing geothermal energy. The current progress in heat transfer analysis models is to divide the soil into several non-isothermal soil layers based on the assumption of uniform borehole wall temperature and heat flux in traditional models, but the temperature and heat flux inside the layers are uniform. Rarely consider the non-uniformity of heat flux within the layer and the boundary problem of vertical heat flux at the ground level. This article adopts a composite medium method to modify the segmented model, considering the heat transfer problem between soil layers. The assumption of uniform temperature of the borehole wall was removed to improve the fluid analysis model. Afterwards, analyze the impact of the heat transfer process inside and outside the borehole on the heat flux of the borehole wall. Using the segmented trial-and-error technique to couple the fluid and soil heat transfer models, a new comprehensive model of the U-shaped grounded heat exchanger was established. Conducted initial underground soil temperature distribution and thermal response tests in different geomorphic units in Guanzhong, Shaanxi, and verified the model's reliability based on experimental data. Analyze three influencing factors, namely fluid mass flow rate, initial underground soil temperature considering variable temperature layer, and temperature difference between average initial underground soil temperature and inlet fluid temperature, to evaluate system performance. The results indicate that the recommended range of fluid mass flow rate in the Guanzhong region is 0.32–0.42 kg/s. It was found that the heat transfer capacity of the heat exchanger will be underestimated if it ignores the influence of the variable temperature layer. Furthermore, the determination of the heat extraction result is not due to the high inlet fluid temperature but rather to the high difference between the inlet fluid temperature and the initial underground soil temperature. This study can promote better system design and achieve higher system performance.
有效描述地热交换器的传热过程对于充分利用地热能至关重要。目前传热分析模型的研究进展是在传统模型中基于钻孔壁温度和热通量均匀的假设,将土壤划分为多个非等温土壤层,但各层内部的温度和热通量是均匀的。很少考虑层内热通量的不均匀性和地层垂直热通量的边界问题。本文采用复合介质法修改分段模型,考虑了土层间的传热问题。取消了井壁温度均匀的假设,改进了流体分析模型。然后,分析钻孔内外传热过程对孔壁热通量的影响。利用分段试错技术将流体和土壤传热模型耦合,建立了新的 U 型接地换热器综合模型。在陕西关中不同地貌单元进行了地下土壤初始温度分布和热响应试验,并根据试验数据验证了模型的可靠性。分析流体质量流量、考虑变温层的地下土壤初始温度、地下土壤平均初始温度与入口流体温度之间的温差三个影响因素,评价系统性能。结果表明,关中地区流体质量流量的推荐范围为 0.32-0.42 kg/s。研究发现,如果忽略变温层的影响,换热器的传热能力将被低估。此外,热量提取结果的确定并非由于入口流体温度过高,而是由于入口流体温度与地下土壤初始温度之间的差异过大。这项研究可以促进更好的系统设计,实现更高的系统性能。
期刊介绍:
Geothermics is an international journal devoted to the research and development of geothermal energy. The International Board of Editors of Geothermics, which comprises specialists in the various aspects of geothermal resources, exploration and development, guarantees the balanced, comprehensive view of scientific and technological developments in this promising energy field.
It promulgates the state of the art and science of geothermal energy, its exploration and exploitation through a regular exchange of information from all parts of the world. The journal publishes articles dealing with the theory, exploration techniques and all aspects of the utilization of geothermal resources. Geothermics serves as the scientific house, or exchange medium, through which the growing community of geothermal specialists can provide and receive information.