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首页> 外文期刊>Energies >Factors Affecting the Installation Potential of Ground Source Heat Pump Systems: A Comparative Study for the Sendai Plain and Aizu Basin, Japan
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Factors Affecting the Installation Potential of Ground Source Heat Pump Systems: A Comparative Study for the Sendai Plain and Aizu Basin, Japan

机译:影响地源热泵系统安装潜力的因素:日本仙台平原和会津盆地的比较研究

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摘要

Evaluating the installation potential of ground source heat pump (GSHP) systems based on the hydrogeological condition of an area is important for the installation and sustainable use of the system. This work is the first to have compared the distributions of heat exchange rate in the Sendai Plain and Aizu Basin (Japan) in terms of topographical and hydrogeological conditions. A regional groundwater flow and heat transport model was constructed for the Sendai Plain. Suitability assessment was conducted for an identical closed-loop system by preparing the distribution maps of heat exchange rate for space heating for the plain and basin. For both locations, the upstream area showed a higher heat exchange rate than the downstream area. Multiple regression analysis was conducted using heat exchange rate as a response variable. Average groundwater flow velocity and average subsurface temperature were considered as explanatory variables. The heat exchange rate for the plain, whose Péclet number ranged from 3.5 × 10 ?3 –7.3 × 10 ?2 , was affected by groundwater flow velocity and subsurface temperature. The exchange rate for the basin, whose Péclet number ranged from 8.5 × 10 ?2 –5.8 × 10 ?1 , was affected by groundwater flow velocity. Inland basins are likely to be more suitable for GSHP system installation utilizing groundwater flow than coastal plains in terms of inclination of slope. This study showed that multiple regression analysis can reveal factors affecting the heat exchange rate as well as the degree to which they affect it.
机译:根据某个地区的水文地质条件评估地源热泵(GSHP)系统的安装潜力对于系统的安装和可持续使用非常重要。这项工作是首次根据地形和水文地质条件比较了仙台平原和会津盆地(日本)的热交换率分布。为仙台平原建立了区域地下水流动和热传输模型。通过准备平原和盆地空间供热的热交换率分布图,对相同的闭环系统进行了适用性评估。对于两个位置,上游区域的热交换率均高于下游区域。使用热交换率作为响应变量进行多元回归分析。平均地下水流速和平均地下温度被认为是解释变量。平原的热交换速率(Péclet数在3.5×10?3 –7.3×10?2之间)受地下水流速和地下温度的影响。该盆地的佩克莱特数在8.5×10?2 –5.8×10?1之间的交换速率受地下水流速的影响。就坡度而言,内陆盆地可能比沿海平原更适合利用地下水流动的GSHP系统安装。这项研究表明,多元回归分析可以揭示影响热交换率的因素以及它们影响热交换率的程度。

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