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为了研究地埋管换热器在变负荷下连续运行与间歇运行的换热性能,基于有限长线热源渗流模型建立竖直地埋管钻孔外准三维非稳态传热模型,应用叠加原理计算钻孔群中钻孔壁温度场及地埋管内流体温度场。在存在地下水水平渗流的情况下,研究了变负荷连续运行模式下不同渗流速度、不同运行工况及不同钻孔位置对地埋管换热器的换热性能的影响。结果表明,在连续运行模式下,边缘位置的钻孔及较大的渗流速度能够增强地埋管换热器的换热性能;在间歇运行模式下,地埋管换热器的运行份额越小,其制冷效果越好,反之,制冷效果越差;在间歇运行工况下,土壤温度能在系统间歇期内得到一定程度的恢复,从而更好地提高地热能的利用率。 相似文献
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介绍了土壤源热泵竖直埋管换热器钻孔外的传统的无限长线热源模型,无限长圆柱模型,有限长线热源模型以及改进后的热湿传递的线热源模型,变热流的线热源模型,土壤分层的线热源模型。分析了各种模型之间的联系、区别以及优缺点。提出了完善土壤源热泵竖直埋管换热器钻孔外传热模型需进一步研究的内容。 相似文献
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地下水运动对地埋管换热器具有重要的影响,通过对比分析渗流无限长与有限长线热源模型,指出考虑轴向传热的有限长线热源更为合理。基于温度场的叠加原理,建立渗流有限长线热源的管群换热模型,并通过耦合管内流体流动,构建管群换热的优化模型。采用位置布置优化措施后,18孔梅花布置比16孔正方形布置的面积利用率提高12.5%,承担相同的负荷其系统的COP值提高7%-10%;16孔管群采用负荷分配优化策略后,其管群的土壤温度场不平衡率大大降低,管群平均温度约降低7.6%,COP提高约10%。 相似文献
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以埋设在均匀渗流介质中的螺旋埋管为研究对象,结合地源热泵工程应用背景,将地下螺旋埋管简化为连续的螺旋线热源,通过移动线热源理论与格林函数法,建立二维和三维非稳态的导热与对流联合作用的渗流传热问题的传热模型;求得无限长及有限长螺旋热源形态下渗流问题的温度响应的解析解。通过与纯导热模型的对比可知,地下水渗流会在一定程度上影响地下温度场的分布及传热达到稳态所需的时间。指出渗流速度是体现地下水流动对换热过程影响程度的重要参数,且渗流对整个螺旋管群的换热影响也被分析讨论。 相似文献
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为了确定渗流对竖直地埋管换热器换热性能的影响,基于多孔介质传热理论与Darcy定律,利用多物理场耦合软件COMSOL建立了三维热渗耦合模型,模拟了有无渗流条件下竖直地埋管换热器周围土壤温度场的变化。结果表明,地下水渗流有助于竖直地埋管换热器换热,且渗流速度越大,竖直地埋管换热器换热效果越明显;平行于渗流方向处温度场偏向下游,垂直于渗流方向处温度场始终保持对称分布,渗流速度由0m/s增大到1.0×10-5 m/s时,对应热作用半径由0.42m减小到0.32m。 相似文献
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为研究不同工况砾砂回填条件下土壤源热泵地理管换热器周围温度场的变化规律,通过自主设计的可模拟地下水渗流的砂箱试验台,以砾砂为回填材料,测试了多种工况下地埋管换热器周围的温度场,并利用Surfer软件绘制等温线。结果表明,饱和无渗流条件下,温度场呈圆形对称分布,随着热负荷的增加,温度场达到稳定的时间延长;稳定后的温度变化量增加;温度变化明显区域的范围增大。饱和有渗流条件下,温度场沿渗流方向向下偏移,随着渗流速度的增加,温度场达到稳定的时间缩短;上游各点达到稳定后的温度变化量减小,温度变化明显区域的范围缩小;下游各点达到稳定后的温度变化量先增大后减小,温度变化明显区域的范围扩大。研究成果提供了一种温度场测试的新方法。 相似文献
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为准确预测地埋管换热器在分层岩土中的传热特征,采用分离变量法和格林函数法,基于单个圆环热源基本传热单元问题的解答,建立考虑岩土结构分层和横观各项同性特征的地埋管传热解析模型。该模型适用于工程中常见的垂直钻孔和桩基埋管换热器分层传热问题,具有较好的普适性。以2层岩土为例,利用模型解答对分层岩土中地埋管的传热特征以及分层参数对其影响规律进行研究。结果表明:均匀介质假设计算误差随作用时间的增加而逐渐增大,在靠近热源处误差更加明显,预测地埋管长时间温度响应时,应采用分层传热模型;在临界区域范围内,可用均质假设模型预测地埋管的传热特性,均质等效热物性参数取为对应岩土分层的热物性参数值;分层岩土导热系数对地埋管传热性能影响较大,岩土平衡温度随分层导热系数比的增大而明显降低;地埋管长度和直径的比值对地埋管传热性能有所影响,岩土平衡温度随长径比的增大而升高,且其影响程度随分层导热系数比的减小而增强。 相似文献
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Nelson Molina-Giraldo Philipp Blum Ke Zhu Peter Bayer Zhaohong Fang 《International Journal of Thermal Sciences》2011,50(12):2506-2513
Available analytical models for the thermal analysis of ground source heat pumps (GSHPs) either neglect groundwater flow or axial effects. In the present study a new analytical approach which considers both effects is developed. Comparison with existing analytical solutions based on the finite and infinite line source theory is carried out. This study shows that in general the heat transfer at the borehole heat exchanger (BHE) is affected by groundwater flow and axial effects. The latter is even more important for long simulation times and short borehole lengths. At the borehole wall the influence of the axial effect is restricted to Peclet numbers lower than 10, assuming the BHE length as characteristic length. Moreover, the influence of groundwater flow is negligible for Peclet numbers lower than 1.2. As a result for Peclet numbers between 1.2 and 10 the combined effect of groundwater flow and axial effects has to be accounted for when evaluating the temperature response of a BHE at the borehole wall and thus the use of the moving finite line source model is required. 相似文献
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Nairen Diao Qinyun Li Zhaohong Fang 《International Journal of Thermal Sciences》2004,43(12):1223-1211
In order to estimate the impact of groundwater flow on performance of geothermal heat exchangers in ground source heat pump systems, an equation of conduction–advection is established for heat transfer in porous media, and an analytical transient solution is obtained for a line heat source in an infinite medium by means of the Green function analysis. An explicit expression has also been derived of the mean temperature on circles around the heat source. Dimensionless criteria that dictate the process are summarized, and influence of the groundwater advection on the heat transfer is discussed accordingly. Computations show that water advection in the porous medium may alter significantly the conductive temperature distribution, result in lower temperature rises and lead to a steady condition eventually. The hydraulic and thermal properties of soils and rocks influencing the advection heat transfer are briefly summarized. The analytical solution has provided a theoretical basis and practical tool for design and performance simulation of the ground heat exchangers. 相似文献
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The ground-coupled heat pump (GCHP) systems have been identified as one of the best sustainable energy technologies for space heating and cooling in residential and commercial buildings. In this paper, research on and development of the GCHP technology in China are summarized. New models are presented for efficient thermal analysis of ground heat exchangers, of which one- and two-dimensional solid cylindrical source models and their analytical solutions are devised to deal with pile ground heat exchangers. Analytical solutions are also derived for vertical and inclined finite line source models as well as for a groundwater advection model. Explicit solutions of a quasi-three-dimensional model can be used to better evaluate the thermal resistance inside boreholes. Studies on hybrid GCHP systems and the thermal response test in China are also commented. 相似文献
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In ground-coupled heat pump systems, accurate prediction of transient ground heat transfer is important to establish the required borehole length and to determine precisely the resulting fluid temperature. Three analytical solutions to transient heat transfer in the vicinity of geothermal boreholes are presented. These solutions are referred to as the infinite line source (ILS), the infinite cylindrical source (ICS) and the finite line source (FLS) models, which vary in complexity and are based on simplifications of the borehole geometry. The results of these models are compared and their validity domains are determined. 相似文献
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Computer simulation of borehole ground heat exchangers for geothermal heat pump systems 总被引:6,自引:0,他引:6
Computer simulation of borehole ground heat exchangers used in geothermal heat pump systems was conducted using three-dimensional implicit finite difference method with rectangular coordinate system. Each borehole was approximated by a square column circumscribed by the borehole radius. Borehole loading profile calculated numerically based on the prescribed borehole temperature profile under quasi-steady state conditions was used to determine the ground temperature and the borehole temperature profile. The two coupled solutions were solved iteratively at each time step. The simulated ground temperature was calibrated using a cylindrical source model by adjusting the grid spacing and adopting a load factor of 1.047 in the difference equation. With constant load applied to a single borehole, neither the borehole temperature nor the borehole loading was constant along the borehole. The ground temperature profiles were not similar at different distances from the borehole. This meant that a single finite difference scheme was not sufficient to estimate the performance of a borefield by superposition. The entire borefield should be discretized simultaneously. Comparison was made between the present method and the finite line source model with superposition. The discrepancies between the results from the two methods increased with the scale of borefield. The introduction of time schedule revealed a discrepancy between the load applied to the ground heat exchanger and that transferred from the borehole to the ground, which was usually assumed to be the same when using analytical models. Hence, in designing a large borefield, the present method should give more precise results in dynamic simulation. 相似文献
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为探究常温注水井对水源热泵热贯通现象的影响,利用FlowHeat1.0软件模拟了3组情景下含水层渗流场、温度场时空分布特征,并分析了常温注水井对含水层热贯通的影响机理和抽水井水温变化规律。结果表明,常温注水井通过减小回灌井、常温注水井之间的水力坡度和延长地下水渗透途径的方式达到缓解热贯通的效果;回灌井、常温注水井流量比相同时,常温注水井在抽灌井连线的位置对含水层热贯通的影响小;抽灌量不变时,常温注水井与回灌井的流量比越大,常温注水井缓解热贯通的效果越明显;在有利地下水回灌的水源热泵系统中,布设常温注水井能有效地降低含水层热贯通程度。 相似文献
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以南方岩溶地区地下水丰富为前提,利用多含水层渗流提高地埋管的换热能力。该文利用有限元软件建立三维单U型换热孔数值模型,利用相关指标分析有无含水层时地源热泵系统的换热效果研究。结果表明:蓄能岩土体内有无含水层多种情况时,U型管出水口平均温度呈现N1>A1>A2>AF1>AF2;AF2、AF1、A2和A1情况下的平均延米换热量分别比N1高49.87%、44.06%、39.51%、31.93%;AF2、AF1、A2和A1情况下的平均COP分别比N1高4.35%、3.93%、3.52%、2.67%。在地下水丰富区域应合理布置换热孔,提升热泵系统运行效率,对实际工程项目可提供一定的指导。 相似文献