Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.14365/5141
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dc.contributor.authorGüney, Mehmet Şükrü-
dc.contributor.authorOkan, Merve-
dc.contributor.authorDumlu, E.-
dc.contributor.authorBor Türkben, Aslı-
dc.contributor.authorAklık, Pelin-
dc.contributor.authorTayfur, G.-
dc.date.accessioned2024-01-26T19:42:33Z-
dc.date.available2024-01-26T19:42:33Z-
dc.date.issued2022-
dc.identifier.issn2521-7119-
dc.identifier.urihttps://doi.org/10.3850/IAHR-39WC2521716X20221298-
dc.identifier.urihttps://hdl.handle.net/20.500.14365/5141-
dc.description39th IAHR World Congress, 2022 -- 19 June 2022 through 24 June 2022 -- 299039en_US
dc.description.abstractInternal erosion, also known as piping, is one of the most important causes of earth-fill dam breaks. Many researchers dealing with numerical analyses in this area make some simplified assumptions about the shape of the breach and the discharge of water flowing through the breach. This study was conducted in the scope of the project supported financially by the Scientific and Technological Research Council of Turkey and it consists of experimental study which aims to provide data needed to perform numerical analyses with more realistic approaches. A dam with a height of 0.6 m, a bottom width of 2 m and a crest width of 0.20 m was built in a flume 1 m wide, 0.81 m high and 6.14 m long. Before the construction of the dam, some common soil mechanics tests were carried out. The dam was constructed by using a mixture consisting of 85 % sand and 15 % clay. A circular tunnel with a diameter of 2 cm was created along the centerline at 6 cm below the dam crest. In the closed system, water was pumped from the lower reservoir to the upper channel. Six cameras located at different locations recorded the evolution of the dam failure. Gauss Area formula was applied to determine the time-varied of the breach areas at upstream and downstream sides. The discharge of water through the breach and average flow velocity were determined by using the continuity equation. The changes in water depth in the channel were also recorded. © 2022 IAHR.en_US
dc.description.sponsorshipTürkiye Bilimsel ve Teknolojik Araştırma Kurumu, TÜBİTAK: 119M609en_US
dc.language.isoenen_US
dc.publisherInternational Association for Hydro-Environment Engineering and Researchen_US
dc.relation.ispartofProceedings of the IAHR World Congressen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectBreach developmenten_US
dc.subjectBreach geometryen_US
dc.subjectDischarge through breachen_US
dc.subjectEarth-fill damen_US
dc.subjectPipingen_US
dc.titleExperimental Study of the Evolution of the Breach and the Discharge Through the Breach Resulting from Piping due to Seepage at the Earth-Fill Dam Topen_US
dc.typeConference Objecten_US
dc.identifier.doi10.3850/IAHR-39WC2521716X20221298-
dc.identifier.scopus2-s2.0-85182012387en_US
dc.departmentİzmir Ekonomi Üniversitesien_US
dc.authorscopusid57197021308-
dc.authorscopusid58038392900-
dc.authorscopusid58037773900-
dc.authorscopusid57203956151-
dc.authorscopusid40461020600-
dc.authorscopusid6701638605-
dc.identifier.startpage2735en_US
dc.identifier.endpage2743en_US
dc.identifier.wosWOS:001070410603014en_US
dc.institutionauthor-
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.identifier.scopusqualityN/A-
dc.identifier.wosqualityN/A-
item.grantfulltextreserved-
item.openairetypeConference Object-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
item.languageiso639-1en-
item.cerifentitytypePublications-
crisitem.author.dept05.03. Civil Engineering-
crisitem.author.dept05.03. Civil Engineering-
crisitem.author.dept05.03. Civil Engineering-
crisitem.author.dept05.03. Civil Engineering-
Appears in Collections:Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection
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