大兴安岭地区岩土热物性特征及冷源对水源热泵影响研究
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摘要
开发利用浅层地热能资源在节能减排、保护环境等方面的效益非常显著。目前，包括辽宁、吉林、黑龙江、内蒙古在内，全国31个省、自治区、直辖市均有开发利用浅层地热能的项目。我国大兴安岭地区由于经济、自然条件等因素在该地区尚无浅层地热能资源评价及岩土热物性特征的相关研究。在国家自然科学基金项目《水源热泵地下THCB耦合运移机理研究》(NO.40972172)的支持下，以及九O四水文地质工程地质勘查院的大力配合下，通过对大兴安岭地区岩土体进行室内、外试验研究该地区岩土体的热物性特征，同时配合抽水试验和回灌试验获取准确的水文地质参数。提出并开展了地下冷源对地下水源热泵的影响进行研究，
本文通过对大兴安岭地区岩土体进行室内、外试验研究该地区岩土体的热物性特征以及地下温度场特征，同时配合抽水试验和回灌试验获取准确的水文地质参数。再与黑龙江庆安县的室内、外热物性试验结果进行对比分析。并且配合抽水试验和回灌试验获取准确的水文地质参数，最后建立岩土热物性数据库系统，对钻探资料、热物性试验资料、测温资料进行管理分析，并且赋予数据库能对数据进行添加、删除、修改、查询、空间分析、数据输出、成果图件成图、报表管理等基本功能以解决多源信息的的综合问题。
结合TOUGH软件模拟群井抽灌系统条件下，通过改变抽灌井在不同空间方位上的间距，不同水文地质条件以及地下水流动方向，回灌水温度等因素，对含水层温度场的影响演化进行研究，尤其针对含水层发生热短路以及井群发生干扰，地下天然冷源对水源热泵的影响等实际水源热泵工程中遇到的问题进行分析研究。
It is very significant that shallow geothermal energy resources is developed andutilized in the benefits of energy saving and environmental protection. At present，the wholecountry has to develop the use of shallow geothermal energy project，including Liaoning，Jilin，Heilongjiang，Neimenggu. For Daxinganling regions of our country，it does not havecorrelation study of the investigation of shallow geothermal energy and the characteristic ofrock and soil thermal properties since economy and natural conditions. With the support ofthe national natural science foundation project”water source heat pump underground THCBcoupled transport mechanism”(NO.40972172)，the paper studied the characteristic of rockand soil thermal properties and the influence of underground cold source to water sourceheat pump in the region through the indoor and field tests，at the same time with thepumping test and recharge tests acquiring accurate hydrogeological parameters.
This paper studied the thermal properties of the rock and soil mass，and obtainedhydrogeological parameters，then compared with the indoor and field test results of Qing`ancounty，Heilongjiang province and Shenyang city，Liaoning province and analyze theirdifference. What is more，under the condition of the TOUGH simulating group wellspumping and irrigating system，the paper analyzed and studied problems in the actual watersource heat pump project，such as，heat breakthrough in the aquifer，wells interference，and so on. Finally，this thesis established a database. The paper studied from followingthree-part：
The first part：the paper developed survey of shallow geothermal resources inDaxinganling Jiagedaqi region，and studied rock and soil thermal properties through theindoor thermal physical experiments and field thermal responsive tests，with the pumpingtest and recharge tests acquiring accurate hydrogeological parameters. At the same time，thepaper measured temperature of22investigation holes in the different locations and analyzedhorizontal and vertical temperature fields distribute conditions. Then，carrying on the indoorthermal physical experiments and field thermal responsive tests in Qing`an county，Heilongjiang province and Shenyang city，Liaoning province，this thesis researched thermalphysical properties of two regions and compared with it in Daxinganling.
The second part：the paper analyzed experimental data and inclusion of the first part，then under the condition of the TOUGH simulating group wells pumping and irrigatingsystem，studied change of aquifer temperature fields through changing the size of thepumping capacity of the aquifer，the interval of pumping and irrigating wells in the different spatial orientation，different hydrogeological conditions and groundwater flow direction，specially for problems in the actual water source heat pump project，such as，heatbreakthrough in the aquifer，wells interference，and so on.
The third part：the shallow geothermal database management system is a integrationand embodiment of the shallow geothermal survey. It has following merit：first，it canorganize a lot of data information systematically and realize structuring of data andinformation highly; Second, it can improve independence and sharing of data，reducingunnecessary data redundancy，saving storage space，and achieve sharing of data resourcesfully；Third，it can make data and information add，delete，modify and retrieve in a commonand controlled way，and service for a wide range of application. For the system mainlyfacilitates government decision-making departments to grasp of occurrence of shallowgeothermal energy resources rapidly and timely in the Jiagedaqi region and providesfoundation for planning，managing and guiding development and utilization of shallowgeothermal resources scientificaly and rationally，it faces the government persons ratherthan professional GIS researchers. Therefore，the system requires not only having a simple，good user interface，but also having a wealth of tips and user help function.
Finally， the paper summarized research results and limitations， and proposedrecommendations on development and utilization of shallow geothermal resources.
本文通过对大兴安岭地区岩土体进行室内、外试验研究该地区岩土体的热物性特征以及地下温度场特征，同时配合抽水试验和回灌试验获取准确的水文地质参数。再与黑龙江庆安县的室内、外热物性试验结果进行对比分析。并且配合抽水试验和回灌试验获取准确的水文地质参数，最后建立岩土热物性数据库系统，对钻探资料、热物性试验资料、测温资料进行管理分析，并且赋予数据库能对数据进行添加、删除、修改、查询、空间分析、数据输出、成果图件成图、报表管理等基本功能以解决多源信息的的综合问题。
结合TOUGH软件模拟群井抽灌系统条件下，通过改变抽灌井在不同空间方位上的间距，不同水文地质条件以及地下水流动方向，回灌水温度等因素，对含水层温度场的影响演化进行研究，尤其针对含水层发生热短路以及井群发生干扰，地下天然冷源对水源热泵的影响等实际水源热泵工程中遇到的问题进行分析研究。
It is very significant that shallow geothermal energy resources is developed andutilized in the benefits of energy saving and environmental protection. At present，the wholecountry has to develop the use of shallow geothermal energy project，including Liaoning，Jilin，Heilongjiang，Neimenggu. For Daxinganling regions of our country，it does not havecorrelation study of the investigation of shallow geothermal energy and the characteristic ofrock and soil thermal properties since economy and natural conditions. With the support ofthe national natural science foundation project”water source heat pump underground THCBcoupled transport mechanism”(NO.40972172)，the paper studied the characteristic of rockand soil thermal properties and the influence of underground cold source to water sourceheat pump in the region through the indoor and field tests，at the same time with thepumping test and recharge tests acquiring accurate hydrogeological parameters.
This paper studied the thermal properties of the rock and soil mass，and obtainedhydrogeological parameters，then compared with the indoor and field test results of Qing`ancounty，Heilongjiang province and Shenyang city，Liaoning province and analyze theirdifference. What is more，under the condition of the TOUGH simulating group wellspumping and irrigating system，the paper analyzed and studied problems in the actual watersource heat pump project，such as，heat breakthrough in the aquifer，wells interference，and so on. Finally，this thesis established a database. The paper studied from followingthree-part：
The first part：the paper developed survey of shallow geothermal resources inDaxinganling Jiagedaqi region，and studied rock and soil thermal properties through theindoor thermal physical experiments and field thermal responsive tests，with the pumpingtest and recharge tests acquiring accurate hydrogeological parameters. At the same time，thepaper measured temperature of22investigation holes in the different locations and analyzedhorizontal and vertical temperature fields distribute conditions. Then，carrying on the indoorthermal physical experiments and field thermal responsive tests in Qing`an county，Heilongjiang province and Shenyang city，Liaoning province，this thesis researched thermalphysical properties of two regions and compared with it in Daxinganling.
The second part：the paper analyzed experimental data and inclusion of the first part，then under the condition of the TOUGH simulating group wells pumping and irrigatingsystem，studied change of aquifer temperature fields through changing the size of thepumping capacity of the aquifer，the interval of pumping and irrigating wells in the different spatial orientation，different hydrogeological conditions and groundwater flow direction，specially for problems in the actual water source heat pump project，such as，heatbreakthrough in the aquifer，wells interference，and so on.
The third part：the shallow geothermal database management system is a integrationand embodiment of the shallow geothermal survey. It has following merit：first，it canorganize a lot of data information systematically and realize structuring of data andinformation highly; Second, it can improve independence and sharing of data，reducingunnecessary data redundancy，saving storage space，and achieve sharing of data resourcesfully；Third，it can make data and information add，delete，modify and retrieve in a commonand controlled way，and service for a wide range of application. For the system mainlyfacilitates government decision-making departments to grasp of occurrence of shallowgeothermal energy resources rapidly and timely in the Jiagedaqi region and providesfoundation for planning，managing and guiding development and utilization of shallowgeothermal resources scientificaly and rationally，it faces the government persons ratherthan professional GIS researchers. Therefore，the system requires not only having a simple，good user interface，but also having a wealth of tips and user help function.
Finally， the paper summarized research results and limitations， and proposedrecommendations on development and utilization of shallow geothermal resources.
引文
[1]中国建筑科学院主编，地源热泵系统工程技术规范[M]，2005，北京：中国建筑工业出版社，2005
[2][Cane R L D,Forgas D A.Modeling of Ground-SourceHeat Pump Performance.ASHRAE Transactions.1991
[3]Sulatisky M T,G van der Kamp.Ground-Source HeatPumps in the Canadian Prairies.ASHRAE Transactions.1991
[4]马最良，吕悦主编，地源热泵系统设计与应用[M]，北京：机械工业出版社，2007
[5]蒋能照，刘道平主编，水源、地源、水环热泵空调技术应用[M]，北京：机械工业出版社，2007
[6]韩再生，浅层地热能的属性和利用[J]，地温资源与地源热泵技术应用论文集（第二集）地质出版社：27~31
[7] Roland Wagner and Christoph Clauser, Evaluating thermal response tests usingparameter estimation for thermal conductivity and thermal capacity [J], J. Geophys.Eng.2(2005)349–356.
[8]吴刚，岩土材料导热系数及水源热泵室内模拟试验研究[M]，2009,吉林大学
[9] Kavanaugh S P.Simulation and experimental verification of vertical ground-coupledheat pump systems[D].Oklahoma State University,1985
[10]W.A.Austin.Development of aninsitu system for measuring groundthermal properties.Oklahoma State University,1995
[11]王秉陈，我国浅层地热能开发现状与发展趋势[J]，供热制冷，2011,12:50-51
[12] M. J. Hatten. Groundwater heat pumping: lessons learned in43years at one building[J]. ASHRAE Transactions,1992,98(1):1031-1037.
[13]龚宇烈,赵军,李新国等.地源热泵在美国工程应用及其发展[C].见:2001年全国热泵和空调技术交流会议论文集.北京:中国建筑工业出版社,2001,249-253.
[14] J. Donald Kroeker, Ray C. Chewing. Heat pump in an office building [J]. ASHRAETransactions,1948,54:221-238.
[15] E. C. Knipe, K. D. Raffery. Corrosion in low temperature geothermal application [J].ASHRAE Transactions,1985,91(2B-1):81-91.
[16] Kevin Raffery. A capital cost comparison of commercial ground-source heat pumpsystem [J]. ASHRAE Transactions,1995,101(2):1095-1100.
[17]张群力,王晋.地源热泵和地下水源热泵的研发现状及应用过程中的问题分析[J].流体机械,2003,5:50-54.
[18] John W. Lund. International course on geothermal heat pumps, Chapter2.4-Design ofclosed-loop geothermal heat exchangers in the U.S.. International summer school ondirect implication geothermal energy[M]:134-146.
[19] Carl D. Orio. A new England school&climate master geothermal heat pumps[C]. In:Hastings School Westborough MA, First Successful100%Geothermal School in NewEngland1997,1-16.
[20] Burkhard Sanner. Ground heat sources for heat pumps (classification, characteristics,advantages)[C]. In: International summer school on direct implication geothermalenergy,1997,1-8.
[21] Zum Boden. Geothermal heat pumps[J]. UbeG.1999,3:16-23.
[22]胡继华，地下水源热泵水力学机理及其对地下温度场影响研究[M]，2009，吉林大学
[23] Ladislaus Rybach, Burkhard Sanner. Ground-source heat pump systems the Europeanexperience [Z]. GHC BULLETIN,2000,(3):16-26.
[24]汪训昌.关于国外电热泵的发展道理及模型-兼谈洋为中用的几点借鉴[J].暖通空调,1994,24(2):22-26.
[25]张延军,王世辉,于子望,吴刚,胡继华.基于岩土工程的地源热泵研究热点及回顾[C].北京:地质出版社,2008.91-95.
[26]李元旦,张旭.土壤源热泵的国内外研究和应用现状及展望[J].制冷空调与电力机械,2002,23(1),4-7.
[27]李家伟,等.土壤源热泵的理论与实践研究[C].1995年暖通空调年会资料集，1995:408-410.
[28]高祖锟.用于供暖的土壤-水热泵系统[J].暖通空调,1995,(4)：9-12.
[29]张昆峰等.土壤热源与热泵联结运行冬季工况的实验研究[J].华中理工大学学报,1996,24(1):23-26.
[30]刘宪英,王勇,胡鸣明,魏唐棣.地源热泵地下垂直埋管换热器的试验研究[J].重庆建筑大学学报,1999,21(5):22-26.
[31]刘冬生,孙友宏.浅层地能利用新技术-地源热泵技术[J].岩土工程技术，2003,(1):57-59.
[32]殷平.地源热泵在中国[J].现代空调,2001,(8):1-10.
[33] http://baike.baidu.com/view/97115.htm
[34] http://baike.baidu.com/view/107252.htm
[35]杨世铭.传热学[M].北京:高等教育出版社,1965.
[36] HAMMERSCHMIDT U.A quasi-steady state technique to measure thethermalconductivity[J].International Journal of Thermophysics,2003,24(5):1291-1312.
[37] American Society for Testing and Materials.Thermal conductivity of materials bymeans of a guarded hot plate,ASTM Specifications, C177-63,1963[C].
[38] KERSTEN M S.Thermal properties of soils.University of Minnesota,Engineering Experiment Station.Bulletin No.28,1949[C].
[39] MOCHLINSKI K.Some industrial measurements of thermal properties ofsoils.International Study Group on Soils[C],Cambridge,England,July12-26,1964:168-178.
[40] SCOTT R F,Sanger F J.Heat exchange at the ground surface.Cold RegionsScience andEngineering.Monograph II-A1,AD0449434,1964[R]. Hanover,NH:Cold RegionsResearch and Engineering Lab.
[41]王庆华，浅层岩土体热物理性质原位测试仪的研制及传热数值模拟[M],2009,吉林大学
[42]张汝惠，谢毅真，利杏荣.QTM导热仪测试条件的研究[J]，地震地质，1986,8(2):26-32
[43] HOOPER F C,LEPPER F R.Transient heat flow apparatus for the determonation ofthermal conductivity[J].Journal of American Society of Heating and VentilatingEngineers,1950(56),309-322.
[44] DE VRIES D A,PECK A J.On the cylindrical probe method of measuring ther-malconductivity with special reference to soils[J].Australian Journal ofPhysics,1958,11:255-271.
[45] SLEGEL D L,DAVIS L R.Transient heat and mass transfer in soils in the vicinity ofheated porous pipes[J].Journal of Heat Transfer,1977,79:541-621.
[46] RAO M V,SINGH D N.Soil thermal resistivity[J].Geotechnical EngineeringBulletin,1999,7(3):179-199.
[47] MANTHENA K C,SINGH D N.Measuring soil thermal resistivity in a geotechnicalcentrifuge[J].International Journal of Physical Modelling inGeotechnics,2001,1(4):29-34.
[48] American Society for Testing and Materials.Standard test method for determination ofthermal conductivity of soil and soft rock by thermal needle probeprocedure.1992[C],ASTM D5334:346-348.
[49]张延军,于子望,黄锐，吴刚等.岩土热导率测量和温度影响研究[J].岩土工程学报,2009,31(2)：213-217.
[50]彭担任,赵全富等.煤与岩石的导热系数研究[J].矿业安全与环保。2000，27(6):16-18
[51]侯方卓.用探针法测定材料的导热系数[J].石油大学学报.1994,18(5):94-98.
[52]孟凡凤,李香龙等.利用探针法测定土壤的导热系数[J].绝缘材料。2006，39(6):65-70.
[52]冯健美,高晓兵等,土壤热源热泵地下换热性能分析[J].太阳能学报。2002,6(3):349-353.
[53]张旭,高晓兵.华东地区土壤及土沙混合物导热系数的实验研究[J].暖通空调.2004,34(5):83-89.
[54]张旭,高晓兵等.土壤及其与黄沙混合物导热系数的实验研究.全国暖通空调制冷2000年学术年会论文集.2000[C],478-481.
[55]苏天明,刘彤等.南京地区土体热物理性质测试与分析[J].岩石力学与工程学报。2006,25(6):1278-1283.
[57] L.A. Salomone L. Aetal. Thermal Performance of Fine-Grained Soils. Journal ofGeotechnical Engineering, Vol.110, No.3, March1984, pp.359-374.
[58]徐学祖，王家澄,张立新.冻土物理学[M].北京:科学出版社,2001.
[59] MOGESEN P.Fluid to duct wall heat transfer in duct system heatstorages[C].Proc.Inc.Conf.On Subsurface Heat Storage in Theory andPractice,Stockholm,Sweden,June6-8,1983:652-657.
[60] EKLOF C,GEHLIN S.A mobile equipment for thermal response test-testing andevaluation[D].Lulea:Lule?University of Technology,1996.
[61] AUSTIN W A.Development of an in situ system for measuring ground thermalproperties[D].Stillwater,Oklahoma:Oklahoma State University,1998.
[62] Sanner B,Hellstr?m G,Spitler J.Thermal response test-current status and world-wideapplication[C].Proceedings World Geothermal Congress,Antalya, Turkey,April2005:24-29.
[63] SANNER B,REUSS M,Thermal response test-experiences in Germany. Proceedings ofTerrastock2000[C],Stuttgart,Germany,August28-Sepertemper1,2000:177-182.
[64] GEHLIN S.Thermal response test-method development and evaluation[D].LuleaUniversity of Technology,2002.
[65]李晓东,于明志等.基于地源热泵的便携式岩土热物性测试仪的研制与应用[J].电子技术应用,2004(5):28-29.
[66]于明志,方肇洪.现场测试地下岩土平均热物性参数方法[J].热能动力工程,2002,17(101):489-492.
[67]于明志,方肇洪.现场测量深层岩土热物性方法[J].工程热物理学，2002，23(3):354-356.
[68]于明志,彭晓峰等.基于线热源模型的地下岩土热物性测试方法[J].太阳能学报，2006,27(3):279-283.
[69]张汝惠，谢毅真，利杏荣.QTM导热仪测试条件的研究[J]，地震地质，1986,8(2):26-32
[70]蔡长录，黄贤龙，等.加格达奇地区浅层土热物性研究[J].中国水运，2011，11（3）：173-175.
[71] Gehlin S. Thermal Response Test-in Situ Measurements of Thermal Properties in HardRock[D].Sweden: Lunea University of Technology,1998.
[72] Witte H,G van Gelder,J Spitler.In-situ thermal conductiv-eity test: a Dutchperspective[J].ASHRAE Transactions,108(1):2002.
[73]王成，群井抽灌地下TH耦合模型及影响因素研究[M],2010,吉林大学
[74] Yu-Shu Wu,Karsten Pruess. A3-D hydrodynamic dispersion model for modelingtracer transport inGeothermal Reservoirs[J]. Lawrence Berkeley NationalLaboratory,1998:1-12.
[75] Pruess, K. TOUGH-A General Purpose Numerical Simulator for Multiphase Fluid andHeat Flow, Lawrence Berkeley Laboratory Report LBL-29400, Lawrence BerkeleyLaboratory, Berkeley, CA,May1991.
[76]施晓清，张可霓，吴吉春，TOUGH发展及应用[J]，工程勘察，2009,10:29~34
[77] Pruess, K, C. Oldenburg and G. Moridis. TOUGH User`s Guide Version2.0[M].Lawrence Berkeley National Laboratory Report LBNL243134, Berkeley, CA,November1999.
[78] Zhang Keni, Yu2Shu Wu, G. S. Bodvarsson and Hui Hai Liu. FlowFocusing inUnsaturated Fracture Networks2A NumericalInvestigation [J]. Vadose Zone Journal,2004,3:624-633.
[79]铁道部第三勘察设计院编著.岩土工程[S].1994，北京：中国铁道出版社
[80]王小柯等编著，C#开发实战宝典[M]，清华大学出版社，2010
[81]王新娟李玲等，浅层地温能数据库基础信息管理系统建设[J]，城市地质，2009-02-15
[82]刘力赟，基于SharpMap的世界地图连续漫游研究与实现，中国科技论文在线http://www.paper.edu.cn/index.php/default/releasepaper/content/200812-345
[83]晏可奇,王宏.沈阳市地下水源热泵系统应用问题分析[C].地温资源与地源热泵技术应用论文集（第二集）,2008,10
[2][Cane R L D,Forgas D A.Modeling of Ground-SourceHeat Pump Performance.ASHRAE Transactions.1991
[3]Sulatisky M T,G van der Kamp.Ground-Source HeatPumps in the Canadian Prairies.ASHRAE Transactions.1991
[4]马最良，吕悦主编，地源热泵系统设计与应用[M]，北京：机械工业出版社，2007
[5]蒋能照，刘道平主编，水源、地源、水环热泵空调技术应用[M]，北京：机械工业出版社，2007
[6]韩再生，浅层地热能的属性和利用[J]，地温资源与地源热泵技术应用论文集（第二集）地质出版社：27~31
[7] Roland Wagner and Christoph Clauser, Evaluating thermal response tests usingparameter estimation for thermal conductivity and thermal capacity [J], J. Geophys.Eng.2(2005)349–356.
[8]吴刚，岩土材料导热系数及水源热泵室内模拟试验研究[M]，2009,吉林大学
[9] Kavanaugh S P.Simulation and experimental verification of vertical ground-coupledheat pump systems[D].Oklahoma State University,1985
[10]W.A.Austin.Development of aninsitu system for measuring groundthermal properties.Oklahoma State University,1995
[11]王秉陈，我国浅层地热能开发现状与发展趋势[J]，供热制冷，2011,12:50-51
[12] M. J. Hatten. Groundwater heat pumping: lessons learned in43years at one building[J]. ASHRAE Transactions,1992,98(1):1031-1037.
[13]龚宇烈,赵军,李新国等.地源热泵在美国工程应用及其发展[C].见:2001年全国热泵和空调技术交流会议论文集.北京:中国建筑工业出版社,2001,249-253.
[14] J. Donald Kroeker, Ray C. Chewing. Heat pump in an office building [J]. ASHRAETransactions,1948,54:221-238.
[15] E. C. Knipe, K. D. Raffery. Corrosion in low temperature geothermal application [J].ASHRAE Transactions,1985,91(2B-1):81-91.
[16] Kevin Raffery. A capital cost comparison of commercial ground-source heat pumpsystem [J]. ASHRAE Transactions,1995,101(2):1095-1100.
[17]张群力,王晋.地源热泵和地下水源热泵的研发现状及应用过程中的问题分析[J].流体机械,2003,5:50-54.
[18] John W. Lund. International course on geothermal heat pumps, Chapter2.4-Design ofclosed-loop geothermal heat exchangers in the U.S.. International summer school ondirect implication geothermal energy[M]:134-146.
[19] Carl D. Orio. A new England school&climate master geothermal heat pumps[C]. In:Hastings School Westborough MA, First Successful100%Geothermal School in NewEngland1997,1-16.
[20] Burkhard Sanner. Ground heat sources for heat pumps (classification, characteristics,advantages)[C]. In: International summer school on direct implication geothermalenergy,1997,1-8.
[21] Zum Boden. Geothermal heat pumps[J]. UbeG.1999,3:16-23.
[22]胡继华，地下水源热泵水力学机理及其对地下温度场影响研究[M]，2009，吉林大学
[23] Ladislaus Rybach, Burkhard Sanner. Ground-source heat pump systems the Europeanexperience [Z]. GHC BULLETIN,2000,(3):16-26.
[24]汪训昌.关于国外电热泵的发展道理及模型-兼谈洋为中用的几点借鉴[J].暖通空调,1994,24(2):22-26.
[25]张延军,王世辉,于子望,吴刚,胡继华.基于岩土工程的地源热泵研究热点及回顾[C].北京:地质出版社,2008.91-95.
[26]李元旦,张旭.土壤源热泵的国内外研究和应用现状及展望[J].制冷空调与电力机械,2002,23(1),4-7.
[27]李家伟,等.土壤源热泵的理论与实践研究[C].1995年暖通空调年会资料集，1995:408-410.
[28]高祖锟.用于供暖的土壤-水热泵系统[J].暖通空调,1995,(4)：9-12.
[29]张昆峰等.土壤热源与热泵联结运行冬季工况的实验研究[J].华中理工大学学报,1996,24(1):23-26.
[30]刘宪英,王勇,胡鸣明,魏唐棣.地源热泵地下垂直埋管换热器的试验研究[J].重庆建筑大学学报,1999,21(5):22-26.
[31]刘冬生,孙友宏.浅层地能利用新技术-地源热泵技术[J].岩土工程技术，2003,(1):57-59.
[32]殷平.地源热泵在中国[J].现代空调,2001,(8):1-10.
[33] http://baike.baidu.com/view/97115.htm
[34] http://baike.baidu.com/view/107252.htm
[35]杨世铭.传热学[M].北京:高等教育出版社,1965.
[36] HAMMERSCHMIDT U.A quasi-steady state technique to measure thethermalconductivity[J].International Journal of Thermophysics,2003,24(5):1291-1312.
[37] American Society for Testing and Materials.Thermal conductivity of materials bymeans of a guarded hot plate,ASTM Specifications, C177-63,1963[C].
[38] KERSTEN M S.Thermal properties of soils.University of Minnesota,Engineering Experiment Station.Bulletin No.28,1949[C].
[39] MOCHLINSKI K.Some industrial measurements of thermal properties ofsoils.International Study Group on Soils[C],Cambridge,England,July12-26,1964:168-178.
[40] SCOTT R F,Sanger F J.Heat exchange at the ground surface.Cold RegionsScience andEngineering.Monograph II-A1,AD0449434,1964[R]. Hanover,NH:Cold RegionsResearch and Engineering Lab.
[41]王庆华，浅层岩土体热物理性质原位测试仪的研制及传热数值模拟[M],2009,吉林大学
[42]张汝惠，谢毅真，利杏荣.QTM导热仪测试条件的研究[J]，地震地质，1986,8(2):26-32
[43] HOOPER F C,LEPPER F R.Transient heat flow apparatus for the determonation ofthermal conductivity[J].Journal of American Society of Heating and VentilatingEngineers,1950(56),309-322.
[44] DE VRIES D A,PECK A J.On the cylindrical probe method of measuring ther-malconductivity with special reference to soils[J].Australian Journal ofPhysics,1958,11:255-271.
[45] SLEGEL D L,DAVIS L R.Transient heat and mass transfer in soils in the vicinity ofheated porous pipes[J].Journal of Heat Transfer,1977,79:541-621.
[46] RAO M V,SINGH D N.Soil thermal resistivity[J].Geotechnical EngineeringBulletin,1999,7(3):179-199.
[47] MANTHENA K C,SINGH D N.Measuring soil thermal resistivity in a geotechnicalcentrifuge[J].International Journal of Physical Modelling inGeotechnics,2001,1(4):29-34.
[48] American Society for Testing and Materials.Standard test method for determination ofthermal conductivity of soil and soft rock by thermal needle probeprocedure.1992[C],ASTM D5334:346-348.
[49]张延军,于子望,黄锐，吴刚等.岩土热导率测量和温度影响研究[J].岩土工程学报,2009,31(2)：213-217.
[50]彭担任,赵全富等.煤与岩石的导热系数研究[J].矿业安全与环保。2000，27(6):16-18
[51]侯方卓.用探针法测定材料的导热系数[J].石油大学学报.1994,18(5):94-98.
[52]孟凡凤,李香龙等.利用探针法测定土壤的导热系数[J].绝缘材料。2006，39(6):65-70.
[52]冯健美,高晓兵等,土壤热源热泵地下换热性能分析[J].太阳能学报。2002,6(3):349-353.
[53]张旭,高晓兵.华东地区土壤及土沙混合物导热系数的实验研究[J].暖通空调.2004,34(5):83-89.
[54]张旭,高晓兵等.土壤及其与黄沙混合物导热系数的实验研究.全国暖通空调制冷2000年学术年会论文集.2000[C],478-481.
[55]苏天明,刘彤等.南京地区土体热物理性质测试与分析[J].岩石力学与工程学报。2006,25(6):1278-1283.
[57] L.A. Salomone L. Aetal. Thermal Performance of Fine-Grained Soils. Journal ofGeotechnical Engineering, Vol.110, No.3, March1984, pp.359-374.
[58]徐学祖，王家澄,张立新.冻土物理学[M].北京:科学出版社,2001.
[59] MOGESEN P.Fluid to duct wall heat transfer in duct system heatstorages[C].Proc.Inc.Conf.On Subsurface Heat Storage in Theory andPractice,Stockholm,Sweden,June6-8,1983:652-657.
[60] EKLOF C,GEHLIN S.A mobile equipment for thermal response test-testing andevaluation[D].Lulea:Lule?University of Technology,1996.
[61] AUSTIN W A.Development of an in situ system for measuring ground thermalproperties[D].Stillwater,Oklahoma:Oklahoma State University,1998.
[62] Sanner B,Hellstr?m G,Spitler J.Thermal response test-current status and world-wideapplication[C].Proceedings World Geothermal Congress,Antalya, Turkey,April2005:24-29.
[63] SANNER B,REUSS M,Thermal response test-experiences in Germany. Proceedings ofTerrastock2000[C],Stuttgart,Germany,August28-Sepertemper1,2000:177-182.
[64] GEHLIN S.Thermal response test-method development and evaluation[D].LuleaUniversity of Technology,2002.
[65]李晓东,于明志等.基于地源热泵的便携式岩土热物性测试仪的研制与应用[J].电子技术应用,2004(5):28-29.
[66]于明志,方肇洪.现场测试地下岩土平均热物性参数方法[J].热能动力工程,2002,17(101):489-492.
[67]于明志,方肇洪.现场测量深层岩土热物性方法[J].工程热物理学，2002，23(3):354-356.
[68]于明志,彭晓峰等.基于线热源模型的地下岩土热物性测试方法[J].太阳能学报，2006,27(3):279-283.
[69]张汝惠，谢毅真，利杏荣.QTM导热仪测试条件的研究[J]，地震地质，1986,8(2):26-32
[70]蔡长录，黄贤龙，等.加格达奇地区浅层土热物性研究[J].中国水运，2011，11（3）：173-175.
[71] Gehlin S. Thermal Response Test-in Situ Measurements of Thermal Properties in HardRock[D].Sweden: Lunea University of Technology,1998.
[72] Witte H,G van Gelder,J Spitler.In-situ thermal conductiv-eity test: a Dutchperspective[J].ASHRAE Transactions,108(1):2002.
[73]王成，群井抽灌地下TH耦合模型及影响因素研究[M],2010,吉林大学
[74] Yu-Shu Wu,Karsten Pruess. A3-D hydrodynamic dispersion model for modelingtracer transport inGeothermal Reservoirs[J]. Lawrence Berkeley NationalLaboratory,1998:1-12.
[75] Pruess, K. TOUGH-A General Purpose Numerical Simulator for Multiphase Fluid andHeat Flow, Lawrence Berkeley Laboratory Report LBL-29400, Lawrence BerkeleyLaboratory, Berkeley, CA,May1991.
[76]施晓清，张可霓，吴吉春，TOUGH发展及应用[J]，工程勘察，2009,10:29~34
[77] Pruess, K, C. Oldenburg and G. Moridis. TOUGH User`s Guide Version2.0[M].Lawrence Berkeley National Laboratory Report LBNL243134, Berkeley, CA,November1999.
[78] Zhang Keni, Yu2Shu Wu, G. S. Bodvarsson and Hui Hai Liu. FlowFocusing inUnsaturated Fracture Networks2A NumericalInvestigation [J]. Vadose Zone Journal,2004,3:624-633.
[79]铁道部第三勘察设计院编著.岩土工程[S].1994，北京：中国铁道出版社
[80]王小柯等编著，C#开发实战宝典[M]，清华大学出版社，2010
[81]王新娟李玲等，浅层地温能数据库基础信息管理系统建设[J]，城市地质，2009-02-15
[82]刘力赟，基于SharpMap的世界地图连续漫游研究与实现，中国科技论文在线http://www.paper.edu.cn/index.php/default/releasepaper/content/200812-345
[83]晏可奇,王宏.沈阳市地下水源热泵系统应用问题分析[C].地温资源与地源热泵技术应用论文集（第二集）,2008,10