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Measuring apparent dose rate factors using beta and gamma rays, and alpha efficiency for precise thermoluminescence dating of calcite
In addition to the conventional 14C and Th/U dating methods, thermoluminescence (TL) dating has been applied to calcite, but has been less popular partly because the luminescence responses for different types of radiation are unclear. To report more reliable TL ages for calcite, the fundamental char...
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Published in: | Journal of Mineralogical and Petrological Sciences 2017, Vol.112(6), pp.336-345 |
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description | In addition to the conventional 14C and Th/U dating methods, thermoluminescence (TL) dating has been applied to calcite, but has been less popular partly because the luminescence responses for different types of radiation are unclear. To report more reliable TL ages for calcite, the fundamental characteristics of its response to radiation exposure were investigated and related to chemical composition. Relative TL factors for calcite after beta and gamma irradiation normalized with quartz, hereafter termed the beta and gamma factors, were measured as 0.19–0.34 and 0.16–0.33, respectively. These lower values than for quartz may be caused by differences in common substitution elements in calcite (20Ca, 25Mn, and 26Fe) versus quartz (3Li, 11Na, 13Al, and 14Si), and the interaction between mediums with different atomic numbers and radiation energies. The beta factor is higher than the gamma factor for some samples. These samples show relatively higher concentrations in lighter elements (up to Ba); thus, the concentration of minor elements may cause differing behavior between beta and gamma rays. The gamma factor may depend on Mn concentration; however, the elements most affecting the beta factor remain unknown. The accumulated dose from alpha rays is affected by sample thickness because of the spatial energy density around the center of the alpha track and luminescence detection range. Thus, for accurate alpha efficiency measurements, evaluation of the effective alpha ray range and luminescence detection thickness is important. The alpha efficiency against the gamma factor, known as the k–value, increases with Mn concentration. Previous studies have suggested that the alpha efficiency is lower than beta and gamma efficiency because the ionization density produced by alpha particles is so great that the thermoluminescence traps in the tracks’ central core become saturated. This leads to a much greater proportion of the ionized electrons being wasted compared with beta and gamma radiation. Thus, we concluded that luminescence traps increase with increasing Mn concentrations. |
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To report more reliable TL ages for calcite, the fundamental characteristics of its response to radiation exposure were investigated and related to chemical composition. Relative TL factors for calcite after beta and gamma irradiation normalized with quartz, hereafter termed the beta and gamma factors, were measured as 0.19–0.34 and 0.16–0.33, respectively. These lower values than for quartz may be caused by differences in common substitution elements in calcite (20Ca, 25Mn, and 26Fe) versus quartz (3Li, 11Na, 13Al, and 14Si), and the interaction between mediums with different atomic numbers and radiation energies. The beta factor is higher than the gamma factor for some samples. These samples show relatively higher concentrations in lighter elements (up to Ba); thus, the concentration of minor elements may cause differing behavior between beta and gamma rays. The gamma factor may depend on Mn concentration; however, the elements most affecting the beta factor remain unknown. The accumulated dose from alpha rays is affected by sample thickness because of the spatial energy density around the center of the alpha track and luminescence detection range. Thus, for accurate alpha efficiency measurements, evaluation of the effective alpha ray range and luminescence detection thickness is important. The alpha efficiency against the gamma factor, known as the k–value, increases with Mn concentration. Previous studies have suggested that the alpha efficiency is lower than beta and gamma efficiency because the ionization density produced by alpha particles is so great that the thermoluminescence traps in the tracks’ central core become saturated. This leads to a much greater proportion of the ionized electrons being wasted compared with beta and gamma radiation. Thus, we concluded that luminescence traps increase with increasing Mn concentrations.</description><identifier>ISSN: 1345-6296</identifier><identifier>EISSN: 1349-3825</identifier><identifier>DOI: 10.2465/jmps.161126</identifier><language>eng</language><publisher>Sendai: Japan Association of Mineralogical Sciences</publisher><subject>Alpha particles ; Alpha rays ; Beta factor ; Beta rays ; Calcite ; Chemical composition ; Dating ; Dating techniques ; Detection ; Dosage ; Dose rate factor ; Efficiency ; Flux density ; Gamma irradiation ; Gamma radiation ; Gamma rays ; Ionization ; Irradiation ; Luminescence ; Luminescence efficiency ; Manganese ; Organic chemistry ; Quartz ; Radiation effects ; Thermoluminescence ; Thermoluminescence dating ; Thickness</subject><ispartof>Journal of Mineralogical and Petrological Sciences, 2017, Vol.112(6), pp.336-345</ispartof><rights>2017 Japan Association of Mineralogical Sciences</rights><rights>Copyright Japan Science and Technology Agency Dec 2017</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c525t-3db1145bbdb2bf4956635fa571329b31558a3f71de7da2f7ab616a35e6cf31233</citedby><cites>FETCH-LOGICAL-c525t-3db1145bbdb2bf4956635fa571329b31558a3f71de7da2f7ab616a35e6cf31233</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,4024,27923,27924,27925</link.rule.ids></links><search><creatorcontrib>OGATA, Manabu</creatorcontrib><creatorcontrib>HASEBE, Noriko</creatorcontrib><creatorcontrib>FUJII, Naoki</creatorcontrib><creatorcontrib>YAMAKAWA, Minoru</creatorcontrib><title>Measuring apparent dose rate factors using beta and gamma rays, and alpha efficiency for precise thermoluminescence dating of calcite</title><title>Journal of Mineralogical and Petrological Sciences</title><description>In addition to the conventional 14C and Th/U dating methods, thermoluminescence (TL) dating has been applied to calcite, but has been less popular partly because the luminescence responses for different types of radiation are unclear. To report more reliable TL ages for calcite, the fundamental characteristics of its response to radiation exposure were investigated and related to chemical composition. Relative TL factors for calcite after beta and gamma irradiation normalized with quartz, hereafter termed the beta and gamma factors, were measured as 0.19–0.34 and 0.16–0.33, respectively. These lower values than for quartz may be caused by differences in common substitution elements in calcite (20Ca, 25Mn, and 26Fe) versus quartz (3Li, 11Na, 13Al, and 14Si), and the interaction between mediums with different atomic numbers and radiation energies. The beta factor is higher than the gamma factor for some samples. These samples show relatively higher concentrations in lighter elements (up to Ba); thus, the concentration of minor elements may cause differing behavior between beta and gamma rays. The gamma factor may depend on Mn concentration; however, the elements most affecting the beta factor remain unknown. The accumulated dose from alpha rays is affected by sample thickness because of the spatial energy density around the center of the alpha track and luminescence detection range. Thus, for accurate alpha efficiency measurements, evaluation of the effective alpha ray range and luminescence detection thickness is important. The alpha efficiency against the gamma factor, known as the k–value, increases with Mn concentration. Previous studies have suggested that the alpha efficiency is lower than beta and gamma efficiency because the ionization density produced by alpha particles is so great that the thermoluminescence traps in the tracks’ central core become saturated. This leads to a much greater proportion of the ionized electrons being wasted compared with beta and gamma radiation. Thus, we concluded that luminescence traps increase with increasing Mn concentrations.</description><subject>Alpha particles</subject><subject>Alpha rays</subject><subject>Beta factor</subject><subject>Beta rays</subject><subject>Calcite</subject><subject>Chemical composition</subject><subject>Dating</subject><subject>Dating techniques</subject><subject>Detection</subject><subject>Dosage</subject><subject>Dose rate factor</subject><subject>Efficiency</subject><subject>Flux density</subject><subject>Gamma irradiation</subject><subject>Gamma radiation</subject><subject>Gamma rays</subject><subject>Ionization</subject><subject>Irradiation</subject><subject>Luminescence</subject><subject>Luminescence efficiency</subject><subject>Manganese</subject><subject>Organic chemistry</subject><subject>Quartz</subject><subject>Radiation effects</subject><subject>Thermoluminescence</subject><subject>Thermoluminescence dating</subject><subject>Thickness</subject><issn>1345-6296</issn><issn>1349-3825</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNo9kMtOwzAQRSMEEqWw4gcssYSU2I6dZokqXlIRG1hbE2fcOsoL21n0A_hvkqZiMw_dM3ekG0W3NFmxVIrHqun9ikpKmTyLFpSneczXTJwfZxFLlsvL6Mr7Kkl4xtfJIvr9QPCDs-2OQN-DwzaQsvNIHAQkBnTonCeDn4ACAxBoS7KDpoGROPiH4w51vweCxlhtsdUHYjpHeofajkZhj67p6qGxLXo9ykhKCJNfZ4iGWtuA19GFgdrjzakvo--X56_NW7z9fH3fPG1jLZgIMS8LSlNRFGXBCpPmQkouDIiMcpYXnAqxBm4yWmJWAjMZFJJK4AKlNpwyzpfR3ezbu-5nQB9U1Q2uHV8qNspZNgYnR-p-prTrvHdoVO9sA-6gaKKmnNWUs5pzHunNTFc-wA7_WXDB6hpPLGVKHut89a_qPTiFLf8DSmiK6Q</recordid><startdate>2017</startdate><enddate>2017</enddate><creator>OGATA, Manabu</creator><creator>HASEBE, Noriko</creator><creator>FUJII, Naoki</creator><creator>YAMAKAWA, Minoru</creator><general>Japan Association of Mineralogical Sciences</general><general>Japan Science and Technology Agency</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8BQ</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>JG9</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope></search><sort><creationdate>2017</creationdate><title>Measuring apparent dose rate factors using beta and gamma rays, and alpha efficiency for precise thermoluminescence dating of calcite</title><author>OGATA, Manabu ; HASEBE, Noriko ; FUJII, Naoki ; YAMAKAWA, Minoru</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c525t-3db1145bbdb2bf4956635fa571329b31558a3f71de7da2f7ab616a35e6cf31233</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Alpha particles</topic><topic>Alpha rays</topic><topic>Beta factor</topic><topic>Beta rays</topic><topic>Calcite</topic><topic>Chemical composition</topic><topic>Dating</topic><topic>Dating techniques</topic><topic>Detection</topic><topic>Dosage</topic><topic>Dose rate factor</topic><topic>Efficiency</topic><topic>Flux density</topic><topic>Gamma irradiation</topic><topic>Gamma radiation</topic><topic>Gamma rays</topic><topic>Ionization</topic><topic>Irradiation</topic><topic>Luminescence</topic><topic>Luminescence efficiency</topic><topic>Manganese</topic><topic>Organic chemistry</topic><topic>Quartz</topic><topic>Radiation effects</topic><topic>Thermoluminescence</topic><topic>Thermoluminescence dating</topic><topic>Thickness</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>OGATA, Manabu</creatorcontrib><creatorcontrib>HASEBE, Noriko</creatorcontrib><creatorcontrib>FUJII, Naoki</creatorcontrib><creatorcontrib>YAMAKAWA, Minoru</creatorcontrib><collection>CrossRef</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Materials Research Database</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of Mineralogical and Petrological Sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>OGATA, Manabu</au><au>HASEBE, Noriko</au><au>FUJII, Naoki</au><au>YAMAKAWA, Minoru</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Measuring apparent dose rate factors using beta and gamma rays, and alpha efficiency for precise thermoluminescence dating of calcite</atitle><jtitle>Journal of Mineralogical and Petrological Sciences</jtitle><date>2017</date><risdate>2017</risdate><volume>112</volume><issue>6</issue><spage>336</spage><epage>345</epage><pages>336-345</pages><issn>1345-6296</issn><eissn>1349-3825</eissn><abstract>In addition to the conventional 14C and Th/U dating methods, thermoluminescence (TL) dating has been applied to calcite, but has been less popular partly because the luminescence responses for different types of radiation are unclear. To report more reliable TL ages for calcite, the fundamental characteristics of its response to radiation exposure were investigated and related to chemical composition. Relative TL factors for calcite after beta and gamma irradiation normalized with quartz, hereafter termed the beta and gamma factors, were measured as 0.19–0.34 and 0.16–0.33, respectively. These lower values than for quartz may be caused by differences in common substitution elements in calcite (20Ca, 25Mn, and 26Fe) versus quartz (3Li, 11Na, 13Al, and 14Si), and the interaction between mediums with different atomic numbers and radiation energies. The beta factor is higher than the gamma factor for some samples. These samples show relatively higher concentrations in lighter elements (up to Ba); thus, the concentration of minor elements may cause differing behavior between beta and gamma rays. The gamma factor may depend on Mn concentration; however, the elements most affecting the beta factor remain unknown. The accumulated dose from alpha rays is affected by sample thickness because of the spatial energy density around the center of the alpha track and luminescence detection range. Thus, for accurate alpha efficiency measurements, evaluation of the effective alpha ray range and luminescence detection thickness is important. The alpha efficiency against the gamma factor, known as the k–value, increases with Mn concentration. Previous studies have suggested that the alpha efficiency is lower than beta and gamma efficiency because the ionization density produced by alpha particles is so great that the thermoluminescence traps in the tracks’ central core become saturated. This leads to a much greater proportion of the ionized electrons being wasted compared with beta and gamma radiation. 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subjects | Alpha particles Alpha rays Beta factor Beta rays Calcite Chemical composition Dating Dating techniques Detection Dosage Dose rate factor Efficiency Flux density Gamma irradiation Gamma radiation Gamma rays Ionization Irradiation Luminescence Luminescence efficiency Manganese Organic chemistry Quartz Radiation effects Thermoluminescence Thermoluminescence dating Thickness |
title | Measuring apparent dose rate factors using beta and gamma rays, and alpha efficiency for precise thermoluminescence dating of calcite |
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