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In-situ radionuclide characterization of a submarine groundwater discharge site at Kalogria Bay, Stoupa, Greece

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dc.contributor.author Tsabaris, C en
dc.contributor.author Patiris, DL en
dc.contributor.author Karageorgis, AP en
dc.contributor.author Eleftheriou, G en
dc.contributor.author Papadopoulos, VP en
dc.contributor.author Georgopoulos, D en
dc.contributor.author Papathanassiou, E en
dc.contributor.author Povinec, PP en
dc.date.accessioned 2014-03-01T02:09:20Z
dc.date.available 2014-03-01T02:09:20Z
dc.date.issued 2012 en
dc.identifier.issn 0265931X en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/29825
dc.subject In-situ gamma-ray spectrometry en
dc.subject Kalogria Bay en
dc.subject Marine environment en
dc.subject Radon en
dc.subject Submarine groundwater discharge en
dc.subject Thoron en
dc.subject.other Gamma ray spectrometry en
dc.subject.other Kalogria Bay en
dc.subject.other Marine environment en
dc.subject.other Submarine groundwater discharge en
dc.subject.other Thoron en
dc.subject.other Aquifers en
dc.subject.other Coastal zones en
dc.subject.other Gamma ray spectrometers en
dc.subject.other Lead en
dc.subject.other Radioisotopes en
dc.subject.other Radon en
dc.subject.other Salinity measurement en
dc.subject.other Spectrometers en
dc.subject.other Groundwater resources en
dc.subject.other bismuth en
dc.subject.other bismuth 214 en
dc.subject.other ground water en
dc.subject.other lead en
dc.subject.other lead 214 en
dc.subject.other potassium 40 en
dc.subject.other radon en
dc.subject.other radon 220 en
dc.subject.other thallium en
dc.subject.other thallium 208 en
dc.subject.other unclassified drug en
dc.subject.other aquifer en
dc.subject.other coastal zone en
dc.subject.other concentration (composition) en
dc.subject.other discharge en
dc.subject.other gamma ray spectrometry en
dc.subject.other groundwater-seawater interaction en
dc.subject.other half life en
dc.subject.other in situ measurement en
dc.subject.other marine environment en
dc.subject.other radionuclide en
dc.subject.other radon isotope en
dc.subject.other salinity en
dc.subject.other seasonality en
dc.subject.other temporal variation en
dc.subject.other thorium en
dc.subject.other time series en
dc.subject.other underwater environment en
dc.subject.other aquifer en
dc.subject.other article en
dc.subject.other bay en
dc.subject.other gamma spectrometry en
dc.subject.other half life time en
dc.subject.other marine environment en
dc.subject.other radioactivity en
dc.subject.other salinity en
dc.subject.other spring en
dc.subject.other summer en
dc.subject.other water temperature en
dc.subject.other Bays en
dc.subject.other Greece en
dc.subject.other Groundwater en
dc.subject.other Radiation Monitoring en
dc.subject.other Radioisotopes en
dc.subject.other Salinity en
dc.subject.other Water Pollutants, Radioactive en
dc.subject.other Greece en
dc.subject.other Kalogria Bay en
dc.subject.other Messenia en
dc.subject.other Peloponnisos en
dc.title In-situ radionuclide characterization of a submarine groundwater discharge site at Kalogria Bay, Stoupa, Greece en
heal.type journalArticle en
heal.identifier.primary 10.1016/j.jenvrad.2011.08.005 en
heal.identifier.secondary http://dx.doi.org/10.1016/j.jenvrad.2011.08.005 en
heal.publicationDate 2012 en
heal.abstract In-situ underwater gamma-ray spectrometer KATERINA was used for continuous measurements of radon progenies (214Pb,214Bi), thoron progeny (208Tl) and40K in submarine groundwater discharge (SGD) sites at Kalogria Bay, SW Peloponnesus (Greece). The spectrometer was deployed attached on measuring platform along with two conductivity - temperature data loggers while underwater battery packs supplied the system for acquisition periods up to 25 days. The radionuclide time series together with salinity data were obtained for spring (wet) and summer (dry) seasons. The40K activity concentrations correlated well with salinity of the emanating groundwater. Although the214Bi and208Tl activities showed usually similar trends anticorrelating with salinity, in some cases208Tl did not follow the214Bi record due to changes in the dynamics of the groundwater aquifer. As the half-life of220Rn is very short (55.6 s), its concentration in SGD may depend on the distance from its origin to the monitoring point. The observed temporal variations of214Bi and208Tl confirmed advantages of continuous in-situ monitoring of SGD in coastal areas. © 2011 Elsevier Ltd. en
heal.journalName Journal of Environmental Radioactivity en
dc.identifier.doi 10.1016/j.jenvrad.2011.08.005 en
dc.identifier.volume 108 en
dc.identifier.spage 50 en
dc.identifier.epage 59 en


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