Please use this identifier to cite or link to this item: https://olympias.lib.uoi.gr/jspui/handle/123456789/17663
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dc.contributor.authorIoannides, K. G.en
dc.contributor.authorPapachristodoulou, C.en
dc.contributor.authorKaramanis, D. T.en
dc.contributor.authorStamoulis, K. C.en
dc.contributor.authorMertzimekis, T. J.en
dc.date.accessioned2015-11-24T18:40:40Z-
dc.date.available2015-11-24T18:40:40Z-
dc.identifier.issn0236-5731-
dc.identifier.urihttps://olympias.lib.uoi.gr/jspui/handle/123456789/17663-
dc.rightsDefault Licence-
dc.titleMeasurements of Rn-222 migration in soilen
heal.typejournalArticle-
heal.type.enJournal articleen
heal.type.elΆρθρο Περιοδικούel
heal.identifier.secondary<Go to ISI>://A1996XQ08300016-
heal.identifier.secondaryhttp://www.springerlink.com/content/uw31r2wx1354370p/fulltext.pdf-
heal.languageen-
heal.accesscampus-
heal.recordProviderΠανεπιστήμιο Ιωαννίνων. Σχολή Επιστημών και Τεχνολογιών. Τμήμα Βιολογικών Εφαρμογών και Τεχνολογιώνel
heal.publicationDate1996-
heal.abstractThe concentration of radon (ZZ?Rn) was measured in the soil near the ground surface, using CR/39 solid st;rte nuclear track detectors. The measurements were carried out in PVC tubes at 0.25 m intervals up to 1.25 m. The detectors were etched in 7N NaOH solutions at 80 degrees C. The alpha-tacks from radon's decay were counted using a microscope. A microscope-camera-computer system developed for automatic counting wets also used. The results provide evidence for the non-diffusive transport of radon in soils. A transport length of (46.9 +/- 3.2) cm was estimated for non-transport near ground surface. Also the variation of soil's radon concentration was correlate to humidity and atmospheric pressure.en
heal.journalNameJournal of Radioanalytical and Nuclear Chemistry-Articlesen
heal.journalTypepeer reviewed-
heal.fullTextAvailabilityTRUE-
Appears in Collections:Άρθρα σε επιστημονικά περιοδικά ( Ανοικτά)

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