dc.creatorAmorim
dc.creatorJ.; Ridenti
dc.creatorM. A.; Guerra
dc.creatorV.
dc.date2015-JUL
dc.date2016-06-07T13:15:15Z
dc.date2016-06-07T13:15:15Z
dc.date.accessioned2018-03-29T01:35:58Z
dc.date.available2018-03-29T01:35:58Z
dc.identifier
dc.identifierExperimental And Theoretical Study Of Atmospheric-pressure Argon Microplasma Jets. Iop Publishing Ltd, v. 57, p. JUL-2015.
dc.identifier0741-3335
dc.identifierWOS:000357496900001
dc.identifier10.1088/0741-3335/57/7/074001
dc.identifierhttp://iopscience.iop.org/article/10.1088/0741-3335/57/7/074001/meta
dc.identifierhttp://repositorio.unicamp.br/jspui/handle/REPOSIP/241827
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1305525
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.descriptionSurface-wave discharges in argon at atmospheric pressure were experimentally studied by optical emission spectroscopy (OES) and mass spectrometry (MS). OES was employed to determine the rotational temperature using the ultraviolet OH band, Q(1) branch and found to be between 450 and 970 K. The electron density (5 x 10(13) cm(-3) <= n(e) <= 7 x 10(14) cm(-3)) was estimated using the H-beta line profile, and produced by dissociation of the water present as an impurity in the Ar gas. The electron temperature (0.63 eV <= T-e <= 1.3 eV) was estimated using a collisional-radiative (CR) model that takes the input measured intensities of four emission lines originating from 2p states including 2p(2), 2p(4), 2p(6), and 2p(10). The density of the metastable state Ar(1s(5)) (2.0 x 10(11) cm(-3) <= Ar(1s(5)) <= 4.2 x 10(12) cm(-3)) was estimated by means of OES using the self-absorbing method. Positive and negative ions were probed along the plasma column using MS. A theoretical model based on the solution of the homogeneous electron Boltzmann equation, considering inelastic and superelastic collisions with the Ar(1s) states and electron-electron collisions, coupled with a system of rate balance equations describing the creation and destruction of the most important heavy particles, is proposed. The experimental results are compared with theoretical ones obtained from a self-consistent model of these discharges, providing physical insight into the basic mechanisms and phenomena ruling the discharges.
dc.description57
dc.description7
dc.description
dc.description
dc.description
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionFundacao para a Ciencia e a Tecnologia (FCT) [Pest-OE/SADG/LA0010/2013]
dc.descriptionFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.descriptionFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.descriptionFAPESP [2008/58034-0]
dc.description
dc.description
dc.description
dc.languageen
dc.publisherIOP PUBLISHING LTD
dc.publisher
dc.publisherBRISTOL
dc.relationPLASMA PHYSICS AND CONTROLLED FUSION
dc.rightsfechado
dc.sourceWOS
dc.subjectTransition-probabilities
dc.subjectLignocellulosic Biomass
dc.subjectSugarcane Bagasse
dc.subjectOzonation Process
dc.subjectDischarge
dc.subjectElectron
dc.subjectPretreatment
dc.subjectTemperature
dc.subjectKinetics
dc.subjectEthanol
dc.titleExperimental And Theoretical Study Of Atmospheric-pressure Argon Microplasma Jets
dc.typeArtículos de revistas


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