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土壤蓄热-放热过程中地埋管周围土壤温度特性模拟
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  • 英文篇名:Simulation on temperature variation characteristics of soil around buried pipe in process of heat storage and release
  • 作者:吴晅 ; 刘卫 ; 路子业 ; 梁盼龙 ; 金光
  • 英文作者:Wu Xuan;Liu Wei;Lu Ziye;Liang Panlong;Jin Guang;School of Energy and Environment, Inner Mongolia University of Science and Technology;
  • 关键词:土壤 ; 温度 ; 热泵系统 ; 地埋管 ; 热作用半径 ; 运行模式 ; 土壤热平衡
  • 英文关键词:soils;;temperature;;heat pump systems;;buried pipe;;thermal influencing radius;;operation mode;;ground heat balance
  • 中文刊名:NYGU
  • 英文刊名:Transactions of the Chinese Society of Agricultural Engineering
  • 机构:内蒙古科技大学能源与环境学院;
  • 出版日期:2017-02-08
  • 出版单位:农业工程学报
  • 年:2017
  • 期:v.33;No.305
  • 基金:内蒙古自治区自然科学基金资助项目(2014MS0530)
  • 语种:中文;
  • 页:NYGU201703028
  • 页数:10
  • CN:03
  • ISSN:11-2047/S
  • 分类号:212-221
摘要
为探索内蒙中部地区地源热泵蓄热-放热过程中地埋管周围土壤温度变化特性,以垂直U型地埋管周围土壤为研究对象,基于有限元分析法建立了二维非稳态传热物理数学模型。在与试验结果进行验证的基础上,对土壤蓄热、放热和蓄热-放热耦合过程进行模拟研究。分析了热作用半径、单位管长换热量和土壤温度随热泵运行时间及运行模式的变化规律;单一条件下的蓄热、放热以及蓄热-放热耦合模式下土壤热平衡问题,探讨了流体入口流速、温度、土壤类型和热泵运行模式等因素对土壤温度场的影响。研究结果表明:热作用半径随蓄热时间的增加而增大且逐渐趋于平缓,热泵运行25和28 d后,热作用半径分别为3.3和3.4 m;流体入口温度对热作用半径及单位管长换热量影响较大但流体流速影响较小,流体入口温度和速度分别为40、60℃和0.6、1.2 m/s时,对应热作用半径分别为3.7、4.5和3.5、3.6 m。合理的间歇运行模式对换热量及埋管周围土壤温度的恢复均有改善;土壤导热系数越大土壤温度恢复时间与效果越佳,土壤导热系数为3.1 W/(m?K)时恢复后温度为9.3℃(土壤初温9.5℃)。此外,蓄热-放热耦合模式下换热量不等对土壤热平衡具有较大影响。试验验证表明,所建模型具有一定的准确性其相对最大误差为5.35%。
        Ground source heat pump(GSHP)has been very popular for space heating and cooling due to its high energy efficiency and low operating cost and thus it is still a very important research subject.Ground heat exchanger is a key component of GSHP.The comprehensive understanding about the heat transfer characteristic of the ground heat exchangers and the soil temperature distribution around the ground heat exchangers is crucial to the performance of GSHP and a large number of researches were carried out,because the operating conditions of GSHP were related closely to the soil temperature field around the ground heat exchangers.Besides,the heat imbalance of GSHP has been become a serious problem,because the amount of heat extracted from and rejected to the soil is usually not equal.It is an especially obvious problem for heating-dominated buildings in the cold and severely cold regions.So,the temperature recovery ability of soil has attracted wide attention.This paper presents the study of the temperature variation characteristics of soil around the ground heat exchangers in the process of heat storage and release of GSHP in the center of Inner Mongolia,China.Based on the finite element method,two-dimensional physical and mathematical models of transient heat transfer were established for the soil around the vertical U-tube ground heat exchanger.The heat storage,heat release and the coupling process were studied on the basis of experimental verification.The variation laws of thermal influencing radius,heat exchange of unit pipe and soil temperature with the operation time and operation mode of GSHP were revealed.The soil heat equilibrium problems in the heat storage,heat release and the coupling process were discussed.The influence of fluid inlet velocity,inlet temperature,soil types and GSHP operation model on the soil temperature field were explored.The results indicated that the thermal influencing radius increased with the increase of operation time and became gentle eventually.With the 25 and 28 days running-time of GSHP,thermal influencing radius is 3.3 and 3.4 m,respectively.The fluid inlet temperature has a great influence on the thermal influencing radius and heat flux of unit pipe,while the fluid inlet velocity has a small impact on these.The fluid inlet temperature and inlet velocity are40,60℃and 0.6,1.2 m/s,respectively.And the corresponding thermal influencing radius is 3.7,4.5 and 3.5,3.6 m.The proper intermittent operation mode could improve the heat transfer rate and the temperature recovery ability of soil around the ground heat exchanger.The recovery time and recovery effect of soil temperature were better with the increase of the thermal conductivity of soil.With the running time of 84 h(heat rejection of 12 hour and recovery of 72 hour),the soil temperature is 9.3℃with a thermal conductivity of 3.1 W/(m?K)(the initial temperature of soil is 9.5℃).In addition,the unequal heat transfer had a great influence on the soil heat balance in the coupling mode of heat storage and release.The experimental validation indicated that enough accuracy could be achieved using the model developed in this study with a maximum difference of 5.35%.
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