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作 者:向佳卉 邹声华[1] 李文菁[2] Xiang Jiahui;Zou Shenghua;Li Wenjing(College of Civil Engineering,Hunan University of Science and Technology,Xiangtan 411201,China;College of Architecture and Engineering,Hunan Institute of Engineering,Xiangtan 411104,China)
机构地区:[1]湖南科技大学土木工程学院,湘潭411201 [2]湖南工程学院建筑工程学院,湘潭411104
出 处:《太阳能学报》2023年第4期371-376,共6页Acta Energiae Solaris Sinica
基 金:国家自然科学基金(51134005);湖南省联合基金(2020JJ6028)。
摘 要:该文以湖南科技大学应用水源热泵系统的水体——月湖为对象,通过调查分析湖水源热泵系统运行时对湖水水温造成的影响及景观水体构建对湖体得热与散热的影响,得出结论:基于麦凯尔方程计算水气之间对流换热叠加飞散水滴换热量,形成新的公式用于瀑布散热量计算的误差为4.3%,景观水体对湖水降温起到了有效作用;通过观测分析,确定湖水变温层的厚度,并用湖水净得热量在湖水变温层内计算的理论温差值与实际测量温差值的误差为2%。Taking Yue Lake water body in Hunan University of Science and Technology as the research object,which is applied ub the water-source heat pump system,the influence of the lake-water-source heat pump system on the lake water temperature and the influence of the construction of the landscape water on the heat gain and heat dissipation of the lake body are analyzed through experiments.The result shows that the convective heat transfer between water and air is calculated based on the Mckell equation and the heat transfer of flying water droplets is superimposed,and a new formula is formed for the calculation of waterfall heat dissipation with the error is 4.3%,and the landscape water plays an effective role in cooling the lake.The thickness of the variable temperature layer of the lake water is determined through observation and analysis,and the error between the theoretical temperature difference and the actual measured temperature difference is 2% when the net heat gain of the lake water is calculated within the variable temperature layer.
分 类 号:TU83[建筑科学—供热、供燃气、通风及空调工程]
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