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High (36)Cl/Cl ratios in Chernobyl groundwater.

Identifieur interne : 001D19 ( Ncbi/Merge ); précédent : 001D18; suivant : 001D20

High (36)Cl/Cl ratios in Chernobyl groundwater.

Auteurs : Céline Roux [France] ; Corinne Le Gal La Salle [France] ; Caroline Simonucci [France] ; Nathalie Van Meir [France] ; L Keith Fifield [Australie] ; Olivier Diez [France] ; Sylvain Bassot [France] ; Roland Simler [France] ; Dmitri Bugai [Ukraine] ; Valery Kashparov [Ukraine] ; Joël Lancelot [France]

Source :

RBID : pubmed:25128774

Descripteurs français

English descriptors

Abstract

After the explosion of the Chernobyl Nuclear Power Plant in April 1986, contaminated material was buried in shallow trenches within the exclusion zone. A (90)Sr plume was evidenced downgradient of one of these trenches, trench T22. Due to its conservative properties, (36)Cl is investigated here as a potential tracer to determine the maximal extent of the contamination plume from the trench in groundwater. (36)Cl/Cl ratios measured in groundwater, trench soil water and leaf leachates are 1-5 orders of magnitude higher than the theoretical natural (36)Cl/Cl ratio. This contamination occurred after the Chernobyl explosion and currently persists. Trench T22 acts as an obvious modern point source of (36)Cl, however other sources have to be involved to explain such contamination. (36)Cl contamination of groundwater can be explained by dilution of trench soil water by uncontaminated water (rainwater or deep groundwater). With a plume extending further than that of (90)Sr, radionuclide which is impacted by retention and decay processes, (36)Cl can be considered as a suitable tracer of contamination from the trench in groundwater provided that modern release processes of (36)Cl from trench soil are better characterized.

DOI: 10.1016/j.jenvrad.2014.07.008
PubMed: 25128774

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pubmed:25128774

Le document en format XML

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<nlm:affiliation>Aix-Marseille Université, CNRS-IRD-Collège de France, UM 34 CEREGE, Technopôle de l'Environnement Arbois-Méditerranée, BP80, 13545 Aix-en-Provence, France; Institute for Radioprotection and Nuclear Safety, PRP-DGE/SRTG, BP 17, F-92262 Fontenay-aux-Roses, France. Electronic address: celine_roux@live.fr.</nlm:affiliation>
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<name sortKey="Kashparov, Valery" sort="Kashparov, Valery" uniqKey="Kashparov V" first="Valery" last="Kashparov">Valery Kashparov</name>
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<nlm:affiliation>Ukrainian Institute of Agricultural Radiology, UIAR NUBiP of Ukraine, Mashinobudivnykiv str. 7, Chabany, Kyiv-Svjatoshin, Ukraine. Electronic address: vak@uiar.kiev.ua.</nlm:affiliation>
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<name sortKey="Lancelot, Joel" sort="Lancelot, Joel" uniqKey="Lancelot J" first="Joël" last="Lancelot">Joël Lancelot</name>
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<nlm:affiliation>Aix-Marseille Université, CNRS-IRD-Collège de France, UM 34 CEREGE, Technopôle de l'Environnement Arbois-Méditerranée, BP80, 13545 Aix-en-Provence, France; Université de Nîmes, Laboratoire de Géochimie Isotopique (GIS), 150 rue George Besse, 30035 Nîmes, France. Electronic address: joel.lancelot@unimes.fr.</nlm:affiliation>
<country xml:lang="fr">France</country>
<wicri:regionArea>Aix-Marseille Université, CNRS-IRD-Collège de France, UM 34 CEREGE, Technopôle de l'Environnement Arbois-Méditerranée, BP80, 13545 Aix-en-Provence, France; Université de Nîmes, Laboratoire de Géochimie Isotopique (GIS), 150 rue George Besse, 30035 Nîmes</wicri:regionArea>
<wicri:noRegion>30035 Nîmes</wicri:noRegion>
<orgName type="university">Université d'Aix-Marseille</orgName>
<placeName>
<settlement type="city">Marseille</settlement>
<region type="region" nuts="2">Provence-Alpes-Côte d'Azur</region>
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<title level="j">Journal of environmental radioactivity</title>
<idno type="eISSN">1879-1700</idno>
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<term>Chernobyl Nuclear Accident</term>
<term>Chlorine (analysis)</term>
<term>Groundwater (analysis)</term>
<term>Radiation Monitoring</term>
<term>Radioisotopes (analysis)</term>
<term>Soil Pollutants, Radioactive (analysis)</term>
<term>Ukraine</term>
<term>Water Movements</term>
<term>Water Pollutants, Radioactive (analysis)</term>
</keywords>
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<term>Accident nucléaire de Tchernobyl</term>
<term>Chlore (analyse)</term>
<term>Contrôle des radiations</term>
<term>Mouvements de l'eau</term>
<term>Nappe phréatique (analyse)</term>
<term>Polluants radioactifs de l'eau (analyse)</term>
<term>Polluants radioactifs du sol (analyse)</term>
<term>Radio-isotopes (analyse)</term>
<term>Ukraine</term>
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<keywords scheme="MESH" type="chemical" qualifier="analysis" xml:lang="en">
<term>Chlorine</term>
<term>Radioisotopes</term>
<term>Soil Pollutants, Radioactive</term>
<term>Water Pollutants, Radioactive</term>
</keywords>
<keywords scheme="MESH" type="geographic" xml:lang="en">
<term>Ukraine</term>
</keywords>
<keywords scheme="MESH" qualifier="analyse" xml:lang="fr">
<term>Chlore</term>
<term>Nappe phréatique</term>
<term>Polluants radioactifs de l'eau</term>
<term>Polluants radioactifs du sol</term>
<term>Radio-isotopes</term>
</keywords>
<keywords scheme="MESH" qualifier="analysis" xml:lang="en">
<term>Groundwater</term>
</keywords>
<keywords scheme="MESH" xml:lang="en">
<term>Chernobyl Nuclear Accident</term>
<term>Radiation Monitoring</term>
<term>Water Movements</term>
</keywords>
<keywords scheme="MESH" xml:lang="fr">
<term>Accident nucléaire de Tchernobyl</term>
<term>Contrôle des radiations</term>
<term>Mouvements de l'eau</term>
<term>Ukraine</term>
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<term>Ukraine</term>
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<front>
<div type="abstract" xml:lang="en">After the explosion of the Chernobyl Nuclear Power Plant in April 1986, contaminated material was buried in shallow trenches within the exclusion zone. A (90)Sr plume was evidenced downgradient of one of these trenches, trench T22. Due to its conservative properties, (36)Cl is investigated here as a potential tracer to determine the maximal extent of the contamination plume from the trench in groundwater. (36)Cl/Cl ratios measured in groundwater, trench soil water and leaf leachates are 1-5 orders of magnitude higher than the theoretical natural (36)Cl/Cl ratio. This contamination occurred after the Chernobyl explosion and currently persists. Trench T22 acts as an obvious modern point source of (36)Cl, however other sources have to be involved to explain such contamination. (36)Cl contamination of groundwater can be explained by dilution of trench soil water by uncontaminated water (rainwater or deep groundwater). With a plume extending further than that of (90)Sr, radionuclide which is impacted by retention and decay processes, (36)Cl can be considered as a suitable tracer of contamination from the trench in groundwater provided that modern release processes of (36)Cl from trench soil are better characterized.</div>
</front>
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<DateCreated>
<Year>2014</Year>
<Month>12</Month>
<Day>03</Day>
</DateCreated>
<DateCompleted>
<Year>2015</Year>
<Month>07</Month>
<Day>16</Day>
</DateCompleted>
<DateRevised>
<Year>2014</Year>
<Month>12</Month>
<Day>03</Day>
</DateRevised>
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<ISSN IssnType="Electronic">1879-1700</ISSN>
<JournalIssue CitedMedium="Internet">
<Volume>138</Volume>
<PubDate>
<Year>2014</Year>
<Month>Dec</Month>
</PubDate>
</JournalIssue>
<Title>Journal of environmental radioactivity</Title>
<ISOAbbreviation>J Environ Radioact</ISOAbbreviation>
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<ArticleTitle>High (36)Cl/Cl ratios in Chernobyl groundwater.</ArticleTitle>
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<MedlinePgn>19-32</MedlinePgn>
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<ELocationID EIdType="pii" ValidYN="Y">S0265-931X(14)00213-6</ELocationID>
<Abstract>
<AbstractText>After the explosion of the Chernobyl Nuclear Power Plant in April 1986, contaminated material was buried in shallow trenches within the exclusion zone. A (90)Sr plume was evidenced downgradient of one of these trenches, trench T22. Due to its conservative properties, (36)Cl is investigated here as a potential tracer to determine the maximal extent of the contamination plume from the trench in groundwater. (36)Cl/Cl ratios measured in groundwater, trench soil water and leaf leachates are 1-5 orders of magnitude higher than the theoretical natural (36)Cl/Cl ratio. This contamination occurred after the Chernobyl explosion and currently persists. Trench T22 acts as an obvious modern point source of (36)Cl, however other sources have to be involved to explain such contamination. (36)Cl contamination of groundwater can be explained by dilution of trench soil water by uncontaminated water (rainwater or deep groundwater). With a plume extending further than that of (90)Sr, radionuclide which is impacted by retention and decay processes, (36)Cl can be considered as a suitable tracer of contamination from the trench in groundwater provided that modern release processes of (36)Cl from trench soil are better characterized.</AbstractText>
<CopyrightInformation>Copyright © 2014 Elsevier Ltd. All rights reserved.</CopyrightInformation>
</Abstract>
<AuthorList CompleteYN="Y">
<Author ValidYN="Y">
<LastName>Roux</LastName>
<ForeName>Céline</ForeName>
<Initials>C</Initials>
<AffiliationInfo>
<Affiliation>Aix-Marseille Université, CNRS-IRD-Collège de France, UM 34 CEREGE, Technopôle de l'Environnement Arbois-Méditerranée, BP80, 13545 Aix-en-Provence, France; Institute for Radioprotection and Nuclear Safety, PRP-DGE/SRTG, BP 17, F-92262 Fontenay-aux-Roses, France. Electronic address: celine_roux@live.fr.</Affiliation>
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<LastName>Le Gal La Salle</LastName>
<ForeName>Corinne</ForeName>
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<Affiliation>Aix-Marseille Université, CNRS-IRD-Collège de France, UM 34 CEREGE, Technopôle de l'Environnement Arbois-Méditerranée, BP80, 13545 Aix-en-Provence, France; Université de Nîmes, Laboratoire de Géochimie Isotopique (GIS), 150 rue George Besse, 30035 Nîmes, France. Electronic address: corinne.legallasalle@unimes.fr.</Affiliation>
</AffiliationInfo>
</Author>
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<LastName>Simonucci</LastName>
<ForeName>Caroline</ForeName>
<Initials>C</Initials>
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<Affiliation>Institute for Radioprotection and Nuclear Safety, PRP-DGE/SRTG, BP 17, F-92262 Fontenay-aux-Roses, France. Electronic address: caroline.simonucci@irsn.fr.</Affiliation>
</AffiliationInfo>
</Author>
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<LastName>Van Meir</LastName>
<ForeName>Nathalie</ForeName>
<Initials>N</Initials>
<AffiliationInfo>
<Affiliation>Institute for Radioprotection and Nuclear Safety, PRP-DGE/SRTG, BP 17, F-92262 Fontenay-aux-Roses, France. Electronic address: nathalie.vanmeir@gmail.com.</Affiliation>
</AffiliationInfo>
</Author>
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<LastName>Fifield</LastName>
<ForeName>L Keith</ForeName>
<Initials>LK</Initials>
<AffiliationInfo>
<Affiliation>Department of Nuclear Physics, Research School of Physics and Engineering, The Australian National University, ACT 0200, Australia. Electronic address: Keith.Fifield@anu.edu.au.</Affiliation>
</AffiliationInfo>
</Author>
<Author ValidYN="Y">
<CollectiveName>ASTER Team</CollectiveName>
</Author>
<Author ValidYN="Y">
<LastName>Diez</LastName>
<ForeName>Olivier</ForeName>
<Initials>O</Initials>
<AffiliationInfo>
<Affiliation>Institute for Radioprotection and Nuclear Safety, PRP-DGE/SRTG, BP 17, F-92262 Fontenay-aux-Roses, France. Electronic address: Olivier.DIEZ@irsn.fr.</Affiliation>
</AffiliationInfo>
</Author>
<Author ValidYN="Y">
<LastName>Bassot</LastName>
<ForeName>Sylvain</ForeName>
<Initials>S</Initials>
<AffiliationInfo>
<Affiliation>Institute for Radioprotection and Nuclear Safety, PRP-DGE/SRTG, BP 17, F-92262 Fontenay-aux-Roses, France. Electronic address: Sylvain.BASSOT@irsn.fr.</Affiliation>
</AffiliationInfo>
</Author>
<Author ValidYN="Y">
<LastName>Simler</LastName>
<ForeName>Roland</ForeName>
<Initials>R</Initials>
<AffiliationInfo>
<Affiliation>Laboratoire d'Hydrologie d'Avignon, UMR EMMAH 11144 INRA, Université d'Avignon, 84000 Avignon, France. Electronic address: roland.simler@univ-avignon.fr.</Affiliation>
</AffiliationInfo>
</Author>
<Author ValidYN="Y">
<LastName>Bugai</LastName>
<ForeName>Dmitri</ForeName>
<Initials>D</Initials>
<AffiliationInfo>
<Affiliation>Institute of Geological Sciences, 55-b, Gonchara Str., Kiev 01054, Ukraine. Electronic address: dmitri.bugay@gmail.com.</Affiliation>
</AffiliationInfo>
</Author>
<Author ValidYN="Y">
<LastName>Kashparov</LastName>
<ForeName>Valery</ForeName>
<Initials>V</Initials>
<AffiliationInfo>
<Affiliation>Ukrainian Institute of Agricultural Radiology, UIAR NUBiP of Ukraine, Mashinobudivnykiv str. 7, Chabany, Kyiv-Svjatoshin, Ukraine. Electronic address: vak@uiar.kiev.ua.</Affiliation>
</AffiliationInfo>
</Author>
<Author ValidYN="Y">
<LastName>Lancelot</LastName>
<ForeName>Joël</ForeName>
<Initials>J</Initials>
<AffiliationInfo>
<Affiliation>Aix-Marseille Université, CNRS-IRD-Collège de France, UM 34 CEREGE, Technopôle de l'Environnement Arbois-Méditerranée, BP80, 13545 Aix-en-Provence, France; Université de Nîmes, Laboratoire de Géochimie Isotopique (GIS), 150 rue George Besse, 30035 Nîmes, France. Electronic address: joel.lancelot@unimes.fr.</Affiliation>
</AffiliationInfo>
</Author>
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<Language>eng</Language>
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<PublicationType UI="D013485">Research Support, Non-U.S. Gov't</PublicationType>
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<Year>2014</Year>
<Month>08</Month>
<Day>15</Day>
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<Country>England</Country>
<MedlineTA>J Environ Radioact</MedlineTA>
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<Keyword MajorTopicYN="N">Chlore-36</Keyword>
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<Keyword MajorTopicYN="N">Strontium-90</Keyword>
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<li>Île-de-France</li>
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