Beta dose rates derived from gamma spectroscopy and low beta anticoincident system of various environmental materials, mainly of archeoglogical origin
Identifieur interne : 000068 ( Istex/Corpus ); précédent : 000067; suivant : 000069Beta dose rates derived from gamma spectroscopy and low beta anticoincident system of various environmental materials, mainly of archeoglogical origin
Auteurs : Y. Liritzis ; Y. Danali-CotsakiSource :
- Science of the Total Environment [ 0048-9697 ] ; 1988.
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Abstract
Abstract: Beta dose-rates (BDR) have been derived from tephras, pumices and pottery of archaeological origin. The BDRs were obtained from two counting systems: (1) gamma spectrometry through appropriate conversion of gamma activity to U, Th, 40K concentration values, and (2) by counting total beta, using a gas-flow sample detector in an anticoincidence mode of counting.Assuming radioactive equilibrium in the U and Th series, the two methods of obtaining BDRs are compared. The degree of disequilibrium, the calibration, and radon escape will be critically considered. The employment of either methods to swift BDR measurements for the TL dating will be discussed.The radioactivity measurements of tephras were used also to provenance those, as Santorini volcano might had not been the only eruption in the Aegean in the 2nd mill. B.C., it might have experienced more than one eruptive phase.BDRs in the samples ranged from 13 to about 470 mrads/year and the agreement between the two methods were in general satisfactory.
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DOI: 10.1016/0048-9697(88)90250-1
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Liritzis</name><affiliation><mods:affiliation>Ministry of Culture, 30 Kalisperi Str., Athens, Greece</mods:affiliation></affiliation></author><author><name sortKey="Danali Cotsaki, Y" sort="Danali Cotsaki, Y" uniqKey="Danali Cotsaki Y" first="Y." last="Danali-Cotsaki">Y. Danali-Cotsaki</name><affiliation><mods:affiliation>N.R.C. Democritos, Agia Paraskevi, Athens, Greece</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Science of the Total Environment</title><title level="j" type="abbrev">STOTEN</title><idno type="ISSN">0048-9697</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1988">1988</date><biblScope unit="volume">70</biblScope><biblScope unit="supplement">C</biblScope><biblScope unit="page" from="41">41</biblScope><biblScope unit="page" to="54">54</biblScope></imprint><idno type="ISSN">0048-9697</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0048-9697</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Agia paraskevi</term><term>Aitken</term><term>Anticoincidence mode</term><term>Bdrs</term><term>Beta</term><term>Chania</term><term>Chania pumices</term><term>Disequilibrium</term><term>Dose rates</term><term>Dosimetry</term><term>Gamma spectrometry</term><term>Liritzis</term><term>Nisyros</term><term>Pottery samples</term><term>Present work</term><term>Pumice</term><term>Santorini</term><term>Tephras</term><term>Thermoluminescence</term><term>Tilos</term><term>Volcano</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Agia paraskevi</term><term>Aitken</term><term>Anticoincidence mode</term><term>Bdrs</term><term>Beta</term><term>Chania</term><term>Chania pumices</term><term>Disequilibrium</term><term>Dose rates</term><term>Dosimetry</term><term>Gamma spectrometry</term><term>Liritzis</term><term>Nisyros</term><term>Pottery samples</term><term>Present work</term><term>Pumice</term><term>Santorini</term><term>Tephras</term><term>Thermoluminescence</term><term>Tilos</term><term>Volcano</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Beta dose-rates (BDR) have been derived from tephras, pumices and pottery of archaeological origin. The BDRs were obtained from two counting systems: (1) gamma spectrometry through appropriate conversion of gamma activity to U, Th, 40K concentration values, and (2) by counting total beta, using a gas-flow sample detector in an anticoincidence mode of counting.Assuming radioactive equilibrium in the U and Th series, the two methods of obtaining BDRs are compared. The degree of disequilibrium, the calibration, and radon escape will be critically considered. The employment of either methods to swift BDR measurements for the TL dating will be discussed.The radioactivity measurements of tephras were used also to provenance those, as Santorini volcano might had not been the only eruption in the Aegean in the 2nd mill. B.C., it might have experienced more than one eruptive phase.BDRs in the samples ranged from 13 to about 470 mrads/year and the agreement between the two methods were in general satisfactory.</div></front></TEI><istex><corpusName>elsevier</corpusName><keywords><teeft><json:string>santorini</json:string><json:string>disequilibrium</json:string><json:string>tephras</json:string><json:string>pumice</json:string><json:string>liritzis</json:string><json:string>bdrs</json:string><json:string>chania</json:string><json:string>thermoluminescence</json:string><json:string>nisyros</json:string><json:string>tilos</json:string><json:string>aitken</json:string><json:string>dosimetry</json:string><json:string>beta</json:string><json:string>present work</json:string><json:string>gamma spectrometry</json:string><json:string>pottery samples</json:string><json:string>dose rates</json:string><json:string>anticoincidence mode</json:string><json:string>agia paraskevi</json:string><json:string>chania pumices</json:string><json:string>volcano</json:string></teeft></keywords><author><json:item><name>Y. 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The degree of disequilibrium, the calibration, and radon escape will be critically considered. The employment of either methods to swift BDR measurements for the TL dating will be discussed.The radioactivity measurements of tephras were used also to provenance those, as Santorini volcano might had not been the only eruption in the Aegean in the 2nd mill. 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Salmon</persName></editor><editor xml:id="book-author-0005"><persName>A.R. Ware</persName></editor><imprint><publisher>ELSEVIER</publisher><date type="published" when="1988"></date><biblScope unit="volume">70</biblScope><biblScope unit="supplement">C</biblScope><biblScope unit="page" from="41">41</biblScope><biblScope unit="page" to="54">54</biblScope></imprint></monogr></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1988</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Beta dose-rates (BDR) have been derived from tephras, pumices and pottery of archaeological origin. The BDRs were obtained from two counting systems: (1) gamma spectrometry through appropriate conversion of gamma activity to U, Th, 40K concentration values, and (2) by counting total beta, using a gas-flow sample detector in an anticoincidence mode of counting.Assuming radioactive equilibrium in the U and Th series, the two methods of obtaining BDRs are compared. The degree of disequilibrium, the calibration, and radon escape will be critically considered. The employment of either methods to swift BDR measurements for the TL dating will be discussed.The radioactivity measurements of tephras were used also to provenance those, as Santorini volcano might had not been the only eruption in the Aegean in the 2nd mill. B.C., it might have experienced more than one eruptive phase.BDRs in the samples ranged from 13 to about 470 mrads/year and the agreement between the two methods were in general satisfactory.</p></abstract></profileDesc><revisionDesc><change when="1988">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/0222BEA5BE71671DA8A0F7E1BF5C8B33D5981E6E/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Elsevier, elements deleted: tail"><istex:xmlDeclaration>version="1.0" encoding="utf-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//ES//DTD journal article DTD version 4.5.2//EN//XML" URI="art452.dtd" name="istex:docType"></istex:docType><istex:document><converted-article version="4.5.2" docsubtype="fla"><item-info><jid>STOTEN</jid><aid>88902501</aid><ce:pii>0048-9697(88)90250-1</ce:pii><ce:doi>10.1016/0048-9697(88)90250-1</ce:doi><ce:copyright type="unknown" year="1988"></ce:copyright></item-info><head><ce:title>Beta dose rates derived from gamma spectroscopy and low beta anticoincident system of various environmental materials, mainly of archeoglogical origin</ce:title><ce:author-group><ce:author><ce:given-name>Y.</ce:given-name><ce:surname>Liritzis</ce:surname><ce:cross-ref refid="AFF1"><ce:sup>∗</ce:sup></ce:cross-ref></ce:author><ce:author><ce:surname>Danali-Cotsaki</ce:surname><ce:cross-ref refid="AFF2"><ce:sup>∗∗</ce:sup></ce:cross-ref></ce:author><ce:affiliation id="AFF1"><ce:label>a</ce:label><ce:textfn>Ministry of Culture, 30 Kalisperi Str., Athens, Greece</ce:textfn></ce:affiliation><ce:affiliation id="AFF2"><ce:label>b</ce:label><ce:textfn>N.R.C. Democritos, Agia Paraskevi, Athens, Greece</ce:textfn></ce:affiliation></ce:author-group><ce:abstract><ce:section-title>Abstract</ce:section-title><ce:abstract-sec><ce:simple-para>Beta dose-rates (BDR) have been derived from tephras, pumices and pottery of archaeological origin. The BDRs were obtained from two counting systems: (1) gamma spectrometry through appropriate conversion of gamma activity to U, Th, <ce:sup loc="pre">40</ce:sup>K concentration values, and (2) by counting total beta, using a gas-flow sample detector in an anticoincidence mode of counting.</ce:simple-para><ce:simple-para>Assuming radioactive equilibrium in the U and Th series, the two methods of obtaining BDRs are compared. The degree of disequilibrium, the calibration, and radon escape will be critically considered. The employment of either methods to swift BDR measurements for the TL dating will be discussed.</ce:simple-para><ce:simple-para>The radioactivity measurements of tephras were used also to provenance those, as Santorini volcano might had not been the only eruption in the Aegean in the 2nd mill. B.C., it might have experienced more than one eruptive phase.</ce:simple-para><ce:simple-para>BDRs in the samples ranged from 13 to about 470 mrads/year and the agreement between the two methods were in general satisfactory.</ce:simple-para></ce:abstract-sec></ce:abstract></head></converted-article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo><title>Beta dose rates derived from gamma spectroscopy and low beta anticoincident system of various environmental materials, mainly of archeoglogical origin</title></titleInfo><titleInfo type="alternative" contentType="CDATA"><title>Beta dose rates derived from gamma spectroscopy and low beta anticoincident system of various environmental materials, mainly of archeoglogical origin</title></titleInfo><name type="personal"><namePart type="given">Y.</namePart><namePart type="family">Liritzis</namePart><affiliation>Ministry of Culture, 30 Kalisperi Str., Athens, Greece</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="family">Danali-Cotsaki</namePart><affiliation>N.R.C. Democritos, Agia Paraskevi, Athens, Greece</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="Full-length article" authority="ISTEX" authorityURI="https://content-type.data.istex.fr" valueURI="https://content-type.data.istex.fr/ark:/67375/XTP-1JC4F85T-7">research-article</genre><originInfo><publisher>ELSEVIER</publisher><dateIssued encoding="w3cdtf">1988</dateIssued><copyrightDate encoding="w3cdtf">1988</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">eng</languageTerm><languageTerm type="code" authority="rfc3066">en</languageTerm></language><abstract lang="en">Abstract: Beta dose-rates (BDR) have been derived from tephras, pumices and pottery of archaeological origin. 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