Preliminary determination of the Radon-222 baseline in Houston, Tex.

dc.contributor.advisorAdams, John A. S.en_US
dc.contributor.committeeMemberGesell, Thomas F.en_US
dc.contributor.committeeMemberClark, Howard C.en_US
dc.creatorMoed, Barbara A.en_US
dc.date.accessioned2018-12-18T21:18:47Zen_US
dc.date.available2018-12-18T21:18:47Zen_US
dc.date.issued1979en_US
dc.description.abstractRadon-222 is a naturally occurring radionuclide that is present in rocks, sediments, and soils in detectable quantities. The migration of radon-222 is promoted by nonreactive chemical properties and by a. 3.82 day half life. A large fraction of the natural radioactivity in surface air is comprised of radon-222 and its short-lived progeny. The activity of radon-222 in soil gas and in surface air exhibits great variability spatially and temporally. This study investigated the temporal variation of radon-222 activities in soil gas and in the surface layer of the atmosphere. The alpha activity in soil gas was monitored at one site for a period of six months. Integrated countrates were recorded daily. Atmospheric radon-222 activities were monitored continuously at an adjacent site during four months of the same period. This difference in the span of monitoring periods was caused by equipment downtime in the air monitoring system. Meteorological data were concurrently tabulated. Univariate graphs were constructed to show the variation of daily mean atmospheric radon-222 activities and of soil gas activities versus mean temperature, mean barometric pressure, average wind speed, and resultant wind direction. The effects of rainfall on these activities were also assessed. The mean of daily soil gas activities is 4.2 counts/ minute; the range of these observations is 1. - 11. counts/ minute. The mean of the atmospheric radon activities is .39 pCi/1; the range of daily mean values is .22 - .79 pC/1. Atmospheric radon activities exhibited distinct diurnal variations. Composite soil samples from the vicinity of the monitoring site were collected and analyzed for uranium-238 and thorium-232 concentrations. The radon-222 and radon 22 emanating powers of these samples were also determined.en_US
dc.format.digitalOriginreformatted digitalen_US
dc.format.extent140 ppen_US
dc.identifier.callnoThesis Geol. 1979 Moeden_US
dc.identifier.citationMoed, Barbara A.. "Preliminary determination of the Radon-222 baseline in Houston, Tex.." (1979) Master’s Thesis, Rice University. <a href="https://hdl.handle.net/1911/104203">https://hdl.handle.net/1911/104203</a>.en_US
dc.identifier.digitalRICE1831en_US
dc.identifier.urihttps://hdl.handle.net/1911/104203en_US
dc.language.isoengen_US
dc.rightsCopyright is held by the author, unless otherwise indicated. Permission to reuse, publish, or reproduce the work beyond the bounds of fair use or other exemptions to copyright law must be obtained from the copyright holder.en_US
dc.titlePreliminary determination of the Radon-222 baseline in Houston, Tex.en_US
dc.typeThesisen_US
dc.type.materialTexten_US
thesis.degree.departmentEarth Scienceen_US
thesis.degree.disciplineNatural Sciencesen_US
thesis.degree.grantorRice Universityen_US
thesis.degree.levelMastersen_US
thesis.degree.nameMaster of Artsen_US
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