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dc.contributor.advisorMarlow, William H.
dc.creatorYoon, Suk-Chul
dc.date.accessioned2024-02-09T20:43:56Z
dc.date.available2024-02-09T20:43:56Z
dc.date.issued1990
dc.identifier.urihttps://hdl.handle.net/1969.1/DISSERTATIONS-1120389
dc.descriptionTypescript (photocopy)en
dc.descriptionVitaen
dc.descriptionMajor subject: Nuclear engineeringen
dc.description.abstractA number of investigators have reported formation of radiolytic ultrafine particles produced by the interaction of ionizing radiation with atmospheric trace gases. Previous studies have suggested that a very high localized concentration of the hydroxyl radical produced by the radiolysis of water can react with atmospheric trace gases such as SO2 and produce lower vapor pressure compounds that can subsequently nucleate. To determine the trace gas and water vapor concentration dependence of the active, positively charged, first decay product of radon, a well-controlled experimental chamber, the Illinois-Clarkson system, was used in this research. The mobility spectrum of the decay products in the range of 0.07-5.0 cm^2/V*sec from the Illinois-Clarkson radon chamber was measured using a specially-designed mobility spectrometer. Measurements were taken for different relative humidities and concentrations of SO2 in purified, compressed air. The mobility of a new-born Po-218 ion measured by the spectrometer was determined to be 1.92 cm^2/V*sec. A comparison of the theoretical and measured alpha track densities was completed to investigate the performance of the ion spectrometer. The resultant mobility spectra at low and high humidities were compared. A Condensation Nuclei Counter (CNC) was used for counting condensation nuclei in each experiment. In the case of low humidities, the reduction of available hydroxyl radical concentration, and hence the neutralization rate, leads to an increase of the shoulder around 1.35 cm^2/V*sec with increasing SO2. This suggests SO2 clustering around the PoO[x]+ ion. For a high humidity condition (5 ppm SO2, 30 % RH), there was clear droplet formation, H2SO4 clustering around the ion and also an increase in the background level between the high mobility peak and the droplet peak. A kinetics study for interpretation of the reaction processes was performed.en
dc.format.extentxiii, 89 leavesen
dc.format.mediumelectronicen
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.rightsThis thesis was part of a retrospective digitization project authorized by the Texas A&M University Libraries. Copyright remains vested with the author(s). It is the user's responsibility to secure permission from the copyright holder(s) for re-use of the work beyond the provision of Fair Use.en
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjectMajor nuclear engineeringen
dc.subject.classification1990 Dissertation Y59
dc.subject.lcshAtmospheric radonen
dc.subject.lcshIon mobility spectroscopyen
dc.subject.lcshPoloniumen
dc.titleMeasurement of the effect of indoor atmospheric trace gas on the polonium-218 ion mobility spectrum by alpha-track detectionen
dc.typeThesisen
thesis.degree.disciplineNuclear engineeringen
thesis.degree.grantorTexas A&M Universityen
thesis.degree.nameDoctor of Philosophyen
thesis.degree.namePh. Den
thesis.degree.levelDoctorialen
dc.contributor.committeeMemberHassan, Yassin A.
dc.contributor.committeeMemberMcFarland, Andrew R.
dc.contributor.committeeMemberMcLain, Milton E.
dc.contributor.committeeMemberPoston, John W.
dc.type.genredissertationsen
dc.type.materialtexten
dc.format.digitalOriginreformatted digitalen
dc.publisher.digitalTexas A&M University. Libraries
dc.identifier.oclc23354089


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