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Experimental study on heat and moisture transfer in soil during soil heat charging for solar-soil source heat pump compound system

机译:太阳能-土壤源热泵复合系统土壤供热过程中土壤热湿传递的实验研究

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摘要

Due to the imbalance of heating and cooling demand, the soil temperature decreases after several years' operation for soil source heat pump system, and consequently the coefficient of performance (COP) decreases. Soil heat charging with solar energy was proposed for solar-soil source heat pump compound system. Many studies have been carried out to investigate the heat and moisture transfer in soil for soil heat charging, but they failed to provide a clear description and explanation of the coupled and mutual effect between heat and moisture transfer. This paper presents an experimental study on the heat and moisture transfer in soil heat charging. The simplified testing rig was constructed to investigate the coupled and mutual effect of one-dimension horizontal heat and moisture transfer in soil heat charging. The results show that, peak volumetric water content (VWC) occurs firstly at the position near heat source and moves towards the other cold end of the tested soil pillar, but it is limited in an area near heat source. The time consumption and value for peak VWC increase with the increasing heat source temperature at the same initial VWC and increase with the increasing initial VWC at the same heat source temperature as well. The heat source temperature is a main factor affecting the peak soil temperature and peak VWC, while the initial VWC has little impact on them.
机译:由于供热和制冷需求的不平衡,土壤源热泵系统运行几年后,土壤温度下降,因此性能系数(COP)下降。提出了利用土壤对太阳能进行热能充注的太阳能-土壤源热泵复合系统。已经进行了许多研究以调查土壤中的热量和水分传递,以补充土壤热量,但未能对热量和水分传递之间的耦合和相互作用产生清晰的描述和解释。本文对土壤热负荷中的热量和水分传递进行了实验研究。构造了简化的试验台,以研究一维水平传热和水分传递在土壤供热中的耦合和相互作用。结果表明,峰值体积水含量(VWC)首先出现在靠近热源的位置,并向被测土柱的另一冷端移动,但它仅限于靠近热源的区域。在相同的初始VWC处,峰值VWC的时间消耗和值随热源温度的升高而增加,并且在相同的热源温度下,随着初始VWC的增加而增加。热源温度是影响峰值土壤温度和峰值VWC的主要因素,而初始VWC对其影响不大。

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