Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.14279/1430
DC FieldValueLanguage
dc.contributor.authorFlorides, Georgios A.-
dc.contributor.authorKalogirou, Soteris A.-
dc.date.accessioned2009-05-26T08:38:04Zen
dc.date.accessioned2013-05-17T05:23:03Z-
dc.date.accessioned2015-12-02T10:13:06Z-
dc.date.available2009-05-26T08:38:04Zen
dc.date.available2013-05-17T05:23:03Z-
dc.date.available2015-12-02T10:13:06Z-
dc.date.issued2008-02-
dc.identifier.citationApplied Thermal Engineering, 2008, vol. 28, no. 2-3, pp. 157-163en_US
dc.identifier.issn13594311-
dc.identifier.urihttps://hdl.handle.net/20.500.14279/1430-
dc.description.abstractA ground heat exchanger can be used for the injection or extraction of thermal energy into/from the ground. The line source model is an easy method of evaluating the characteristics of the borehole and does not need expensive equipment. This method is presented and a test is performed in order to determine a borehole’s characteristics in layers consisting of clay, silt and sand at various analogies. For the borehole under test the ground thermal conductivity (λ) was found to be 1.605 W/(m K) and the effective borehole thermal resistance (Rb) to be 0.257 K/(W/m). The accuracy of the collected data could be affected mainly by two factors. The first factor is the daily flux penetration through the ground which gradually increases the temperature of the top layers and the second factor is a variation of the heating coil injection rate per active length of borehole. As it was observed this combined effect has a negligible result on the mean fluid temperature during the test hours of 280–400, when the system was operating at steady state. The steady state conditions yield values of borehole thermal resistance which deviates about 25% from the values given by the line source method. The ground thermal conductivity deviates only about 5%. This method however is not suitable for estimating the above values because of the uncertainty that exists in the estimation of the mean ground temperature, which is not constant throughout the borehole length nor is it constant at different points in a cross section of the grout. Also this method takes a lot of time until the steady state is reached.en_US
dc.formatpdfen_US
dc.language.isoenen_US
dc.relation.ispartofApplied Thermal Engineeringen_US
dc.rights© Elsevier 2007en_US
dc.subjectBoreholeen_US
dc.subjectGround thermal conductivityen_US
dc.subjectLine source methoden_US
dc.titleFirst in situ determination of the thermal performance of a U-pipe borehole heat exchanger, in Cyprusen_US
dc.typeArticleen_US
dc.collaborationHigher Technical Institute Cyprusen_US
dc.subject.categoryEnvironmental Engineeringen_US
dc.journalsHybrid Open Accessen_US
dc.countryCyprusen_US
dc.subject.fieldEngineering and Technologyen_US
dc.publicationPeer Revieweden_US
dc.identifier.doi10.1016/j.applthermaleng.2007.03.026en_US
dc.dept.handle123456789/54en
dc.relation.issue2-3en_US
dc.relation.volume28en_US
cut.common.academicyear2019-2020en_US
dc.identifier.spage157en_US
dc.identifier.epage163en_US
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.openairetypearticle-
item.cerifentitytypePublications-
item.grantfulltextnone-
item.languageiso639-1en-
item.fulltextNo Fulltext-
crisitem.journal.journalissn1359-4311-
crisitem.journal.publisherElsevier-
crisitem.author.deptDepartment of Mechanical Engineering and Materials Science and Engineering-
crisitem.author.deptDepartment of Mechanical Engineering and Materials Science and Engineering-
crisitem.author.facultyFaculty of Engineering and Technology-
crisitem.author.facultyFaculty of Engineering and Technology-
crisitem.author.orcid0000-0001-9079-1907-
crisitem.author.orcid0000-0002-4497-0602-
crisitem.author.parentorgFaculty of Engineering and Technology-
crisitem.author.parentorgFaculty of Engineering and Technology-
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