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Theory of Surface Deposition from Boundary Layers

dc.conference.date22-28 May 2008
dc.conference.placeLondres (UK)
dc.conference.titleEuropean Conference for Mathematics in Industry
dc.contributor.authorNeu, John
dc.contributor.authorCarpio Rodríguez, Ana María
dc.contributor.authorBonilla, Luis L.
dc.date.accessioned2023-06-20T14:18:08Z
dc.date.available2023-06-20T14:18:08Z
dc.date.issued2008-05
dc.description.abstractHeterogeneous condensation of vapours mixed with a carrier gas in the stagnation point boundary layer flow near a cold wall is considered in the presence of solid particles much larger than the mean free path of vapour particles. The supersaturated vapour condenses on the particles by diffusion, and particles and droplets are thermophoretically attracted to the wall. Assuming that the heat of vaporization large enough vapour condensation occurs in a condensation layer (CL). The CL width and characteristics depend on the parameters of the problem, and a parameter R yielding the rate of vapour scavenging by solid particles is particularly important. Assuming that the CL is so narrow that temperature, particle density and velocity do not change appreciably inside it, an asymptotic theory is found that approximates very well the vapour and droplet profiles, the dew point shift and the deposition rates at the wall for wide ranges of the wall temperature and the scavenging parameter R. This theory breaks down for wall temperatures very close to the maximum temperature yielding non-zero droplet deposition rate. If the width of the CL is assumed to be zero, the vapour density reaches local equilibrium with the condensate immediately after it enters the dew surface. This theory yields appropriate profiles and deposition rates in the limit as R tends to infinity and also for any R, provided the wall temperature is very close to the above mentioned maximum temperature. Nonlinear multiple scales also improve this theory, providing good uniform approximations to the deposition rates and the profiles for large R or for moderate R. These findings are in contrast with observations for homogeneous nucleation.en
dc.description.departmentDepto. de Análisis Matemático y Matemática Aplicada
dc.description.facultyFac. de Ciencias Matemáticas
dc.description.refereedTRUE
dc.description.statussubmitted
dc.eprint.idhttps://eprints.ucm.es/id/eprint/74504
dc.identifier.urihttps://hdl.handle.net/20.500.14352/54105
dc.language.isoeng
dc.rights.accessRightsopen access
dc.subject.ucmFísica atmosférica
dc.subject.ucmFísica de materiales
dc.subject.unesco2501 Ciencias de la Atmósfera
dc.titleTheory of Surface Deposition from Boundary Layersen
dc.typeconference paper
dspace.entity.typePublication
relation.isAuthorOfPublicationf301b87d-970b-4da8-9373-fef22632392a
relation.isAuthorOfPublication.latestForDiscoveryf301b87d-970b-4da8-9373-fef22632392a

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