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On Turbulent Rayleigh-Bénard Convection in a Two-Phase Binary Gas Mixture

dc.contributor.advisorNobach, Holger Dr.
dc.contributor.authorWinkel, Florian
dc.date.accessioned2015-11-27T09:56:43Z
dc.date.available2015-11-27T09:56:43Z
dc.date.issued2015-11-27
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0028-8645-2
dc.identifier.urihttp://dx.doi.org/10.53846/goediss-5396
dc.language.isoengde
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subject.ddc571.4de
dc.titleOn Turbulent Rayleigh-Bénard Convection in a Two-Phase Binary Gas Mixturede
dc.typedoctoralThesisde
dc.contributor.refereeNobach, Holger Dr.
dc.date.examination2014-10-27
dc.description.abstractengIn this thesis an attempt is made to generate cloud patterns in a laboratory scale experiment. A two-phase binary gas mixture is employed as a physical model system. The fluid mixture is composed of a condensable gas which forms a liquid and a vapor phase and a noncondensable gas which serves as a background or carrier gas. The fluid mixture is confined between a bottom and a top plate. If the fluid mixture is exposed to a constant temperature difference, two intriguing phenomena can be observed. First a film condensation sets in at the cold top plate that results in the formation of a very regular hexagonal droplet pattern. The temporal evolution of the droplet pattern is quantified and it is shown that a stable mass flux is essential in order to the maintain the hexagonal symmetry of the droplet patten. Second cloud-like patterns occur in a thin layer above the liquid-vapor interface. The dynamics of the cloud-like patterns reveal the turbulent flow inside the gaseous phase. An area-perimeter analysis of the cloud-like patterns results in a fractal dimension that is similar to the one obtained by the fractal analysis of two-dimensional cloud and rain areas in satellite and radar data. This thesis is meant as a proof of concept which is why most of the results are still qualitative. However, a physical model system is presented that is appropriate in order to study the dynamics of cloud-like patterns in a turbulent Rayleigh-Bénard convection experiment. The origin of the cloud-like patterns is still a matter of debate. Therefore further experiments that could reveal the nature of these patterns must be performed.de
dc.contributor.coRefereeTilgner, Andreas Prof. Dr.
dc.subject.engBuoyancy-driven flowsde
dc.subject.engRayleigh-Bénard convectionde
dc.subject.engInterfacial instabilitiesde
dc.subject.engRayleigh-Taylor instabilityde
dc.subject.engGas/liquid flowsde
dc.subject.engThermal convectionde
dc.identifier.urnurn:nbn:de:gbv:7-11858/00-1735-0000-0028-8645-2-7
dc.affiliation.instituteGöttinger Graduiertenschule für Neurowissenschaften, Biophysik und molekulare Biowissenschaften (GGNB)de
dc.subject.gokfullBiologie (PPN619462639)de
dc.identifier.ppn841076863


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