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dc.contributor.authorGer, Ahmet Metin
dc.date.accessioned2020-06-29T10:07:49Z
dc.date.available2020-06-29T10:07:49Z
dc.date.issued2019
dc.identifier.issn1300-3453
dc.identifier.urihttps://doi.org/10.18400/tekderg.467567en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12469/2972
dc.description.abstractThe heated surface jet discharged into a bay which is connected to a larger body of water through a strait may experience bifurcation in the bay and stratification in the strait. The combined effects of bifurcation and stratification may lead to a substantially greater rise in temperature than the rise expected in case of unrestricted receiving body of water. In this study, the behavior of heated effluents discharged into bays with a restricted access to a large body of water is scrutinized experimentally by the help of a scaled physical model. Dimensional analysis leads to a new dimensionless parameter A(r), area restriction parameter, on which the difference between the excess temperatures at the inlet of the strait for restricted and free receiving mediums, Delta(Delta T/Delta T-0) is shown to be strongly dependent.en_US
dc.language.isoEnglishen_US
dc.publisherTurkish Chamber Civil Engineersen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectHeated effluentsen_US
dc.subjectSurface jetsen_US
dc.subjectExcess heaten_US
dc.titleEffects of Straits on Hydro-Thermal Performance of Small Baysen_US
dc.typeArticleen_US
dc.identifier.startpage9675en_US
dc.identifier.endpage9682en_US
dc.relation.journalTeknik Dergien_US
dc.identifier.issue6en_US
dc.identifier.volume30en_US
dc.identifier.wosWOS:000494262000007en_US
dc.identifier.doi10.18400/tekderg.467567en_US
dc.contributor.khasauthorGer, Ahmet Metinen_US


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