辽宁石油化工大学学报

辽宁石油化工大学学报 ›› 2010, Vol. 30 ›› Issue (1): 51-54.DOI: 10.3696/j.issn.1672-6952.2010.01.015

• 化工机械 • 上一篇    下一篇

土壤源热泵单U 型埋管换热器短期运行换热分析

李小玲,马贵阳*   

  1. 辽宁石油化工大学储运与建筑工程学院,辽宁抚顺113001
  • 收稿日期:2009-03-11 出版日期:2010-03-25 发布日期:2017-07-05
  • 作者简介:李小玲(1982-),女,青海西宁市,讲师,硕士。

 
Short-Term Operation Analysis of Heat Exchange on Single U-Tube Heat Exchanger of Ground Coupled Heat Pump

 

LI Xiao-ling,MA Gui-yang*
  

  1. School of Storage and Architecture Engineering, Liaoning Shihua University,Fushun Liaoning 113001,P.R. China
  • Received:2009-03-11 Published:2010-03-25 Online:2017-07-05

摘要: 单U 型管是当前土壤源热泵系统广泛使用的地下换热器形式,而地下换热器是地源热泵系统的重要
组成部分。考虑U 型管的实际形状,借助数学方法和数值分析软件,建立了地下垂直埋管换热器传热模型,并通过
编程求解数学模型,得到了系统短期运行不同工况下埋管周围土壤的温度场分布情况。通过分析得出土壤导热系
数、土壤比热、钻孔回填材料导热系数以及U 型管间距的大小对埋管的换热性能具有直接影响。得出的结果可为合
理设计地下埋管换热器提供参考。

关键词: 单U 型管 , 地源热泵 , 数值分析 , 传热模型 , 温度场

Abstract: A single U-tube is the most common type of ground heat exchange in Ground Coupled Heat Pump(GCHP)system, and ground heat exchanger is an important component of the GCHP system. The real shape of U-tube was considered, and heat transfer model of underground vertical buried tube heat exchanger was built with math methods and numerical analysis software. The soil temperature distributions around the buried tube under different working conditions were solved by programming. The analysis shows that the thermal conductivity and specific heat of soil, the thermal conductivity of backfilled material in drilling and the distance between U-tubes have direct effect on the heat transfer performance of buried tubes. The results may provide guidance in the design of GCHP systems.

Key words: Single U-tube ,  Ground coupled heat pump ,  Numerical analysis ,  Heat transfer model ,  Temperature distribution

引用本文

李小玲,马贵阳. 土壤源热泵单U 型埋管换热器短期运行换热分析[J]. 辽宁石油化工大学学报, 2010, 30(1): 51-54.

LI Xiao-ling,MA Gui-yang.  

Short-Term Operation Analysis of Heat Exchange on Single U-Tube Heat Exchanger of Ground Coupled Heat Pump
[J]. Journal of Liaoning Petrochemical University, 2010, 30(1): 51-54.

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