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dc.contributor.authorÇelik, Ahmet Ozan
dc.contributor.authorDiplas, Panayiotis
dc.contributor.authorDancey, Clint L.
dc.date.accessioned2019-10-21T20:42:01Z
dc.date.available2019-10-21T20:42:01Z
dc.date.issued2013
dc.identifier.issn0043-1397
dc.identifier.issn1944-7973
dc.identifier.urihttps://dx.doi.org/10.1002/wrcr.20210
dc.identifier.urihttps://hdl.handle.net/11421/20941
dc.descriptionWOS: 000319282100033en_US
dc.description.abstractThe overall objective of this study is to identify the physical mechanisms responsible for the entrainment of an exposed particle subject to rapidly fluctuating hydrodynamic forces in the case of channel flow with a fully rough boundary. This is pursued here by examining particle dislodgment under uniform and cylinder wake-flow experiments. The critical impulse concept is investigated more rigorously by measuring directly the pressures at four points on the surface of a fixed test grain. The number of impulse events determined from these experiments increases by more than an order of magnitude, over a modest change of roughness Reynolds number. Furthermore, they are well described by a log-normal probability density function. Both results are consistent with those obtained from similar experiments via indirect (velocity-based) impulse calculations and reported in a prior contribution. This comparison supports the use of the velocity record for determining instantaneous hydrodynamic forces and impulses instead of the more difficult approach of measuring the pressure fluctuations directly. The present results demonstrate the dominant role the local, streamwise velocity component plays on particle dislodgment. This is attributed to the large impulse content and occasionally strong positive lift force associated with flow events, exhibiting pronounced positive streamwise velocity fluctuations. The majority (approximate to 70%) of these events occur in the fourth quadrant, while a significant number (approximate to 22%) appear as first-quadrant episodes. It was also determined that wake flows can increase substantially particle entrainment via enhanced lift and increased turbulence intensity.en_US
dc.description.sponsorshipNational Science Foundation [EAR-0439663, EAR-0738759, CBET-1033196]; Army Research Officeen_US
dc.description.sponsorshipThe support of the National Science Foundation (grants EAR-0439663, EAR-0738759, and CBET-1033196) and the Army Research Office is gratefully acknowledged.en_US
dc.language.isoengen_US
dc.publisherAmer Geophysical Unionen_US
dc.relation.isversionof10.1002/wrcr.20210en_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectIncipient Motionen_US
dc.subjectImpulseen_US
dc.subjectForce Fluctuationsen_US
dc.titleInstantaneous turbulent forces and impulse on a rough bed: Implications for initiation of bed material movementen_US
dc.typearticleen_US
dc.relation.journalWater Resources Researchen_US
dc.contributor.departmentAnadolu Üniversitesi, Mühendislik Fakültesi, İnşaat Mühendisliği Bölümüen_US
dc.identifier.volume49en_US
dc.identifier.issue4en_US
dc.identifier.startpage2213en_US
dc.identifier.endpage2227en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US]
dc.contributor.institutionauthorÇelik, Ahmet Ozan


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