{"title":"两种中子通量热化程度不同的辐照设施的裂变径迹定年zeta标定常数的直接比较","authors":"Seong-Cheon Shin , Susumu Nishimura","doi":"10.1016/0168-9622(91)90018-R","DOIUrl":null,"url":null,"abstract":"<div><p>Zeta (ζ) constants were determined using zircon, apatite and sphene age standards for a systematic calibration of fission-track dating. Identical crystals were double-checked in two facilities having significantly different degrees of neutron flux thermalization: Irradiation Pit-6 (IP-6) of the Korea Atomic Energy Research Institute (KAERI) TRIGA III reactor and the Graphite Pneumatic Tube (GrPn) of the Kyoto University Research Reactor (KUR-<em>1</em>) which have Cd ratios of 12.5 and ∼200, respectively, for Au. The final single weighted mean ζ baselines are given with errors (2σ) as: 324.5 ± 7.9 for SRM<em>612</em>, 110.9±2.7 for CN<em>1</em> and 118.8±2.9 for CN<em>2</em> from KAERI IP-<em>6</em>; and 333.7±8.5 for SRM<em>612</em>, 109.0±2.8 for CN<em>1</em> and 119.5 ± 3.1 for CN<em>2</em> from KUR GrPn. The final results from both facilities show anexcellent consistency in ζs for CN<em>1</em> and CN<em>2</em> and a discrepancy ( ∼2.8%) in SRM<em>612</em>-ζ values despite of a rough agreement within the error (2σ). Lower ratios (∼2.5–4%) of <em>ϱ</em><sub>d</sub><sup>CN1</sup>/<em>ϱ</em><sub>d</sub><sup><em>SRM</em></sup>612, <em>ϱ</em><sub>d</sub><sup>CN2</sup>/<em>ϱ</em><sub>d</sub><sup>SRM612</sup> and <em>ϱ</em><sub>i</sub><sup>mineral</sup>/<em>ϱ</em><sub>d<sup><em>SRM</em>612</sup></sub> in KAERI IP-<em>6</em> strongly imply such a decrease of <em>ζ</em><sub>SRM6<em>l</em>2</sub>.</p><p>The consistency in <em>ζ</em><sub>CN1</sub> and <em>ζ</em><sub>CN2</sub> in both facilities implies that the large difference in <sup>232</sup>Th/<sup>235</sup>5U ratio between the mineral and CN<em>1</em> or CN<em>2</em> may not significantly affect thermal neutron dosimetry, even for apatite which has the largest difference of the ratio against dosimeter glasses. The larger (n,f ) reaction cross-section of <sup>238</sup>U than that of <sup>232</sup>2Th in epithermal and fast neutron energy regions also suggests that the difference of <sup>238</sup>U /<sup>235</sup>U ratio as seen in glass SRM<em>612</em>, which has depleted U, may affect the thermal neutron dosimetry more significantly than that of <sup>232</sup>Th/<sup>235</sup>U ratio regardless of Th/U ratios of the three minerals. Therefore, the discrepancy in <em>ζ</em><sub>SRM</sub>612 results mainly from the larger contribution of <sup>238</sup>U fission induced by non-thermal neutrons to the thermal neutron dosimetry in the less thermalized KAERI IP-<em>6</em>. In consequence, the final <em>ζ</em><sub>SRM6<em>l</em>1</sub> from KAERI IP-<em>6</em> is significantly less precise. The final ζ baselines for CN<em>1</em> and CN<em>2</em>, obtained independently from both facilities, are to be recommended for accurate fission-track analyses in preference to the SRM<em>612</em>-ζ baseline, even in the well-thermalized facility, e.g. KUR GrPn.</p></div>","PeriodicalId":100231,"journal":{"name":"Chemical Geology: Isotope Geoscience section","volume":"87 3","pages":"Pages 147-166"},"PeriodicalIF":0.0000,"publicationDate":"1991-10-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0168-9622(91)90018-R","citationCount":"5","resultStr":"{\"title\":\"Direct comparison of zeta calibration constants for fission-track dating by double-checking of two irradiation facilities with different degrees of neutron flux thermalization\",\"authors\":\"Seong-Cheon Shin , Susumu Nishimura\",\"doi\":\"10.1016/0168-9622(91)90018-R\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Zeta (ζ) constants were determined using zircon, apatite and sphene age standards for a systematic calibration of fission-track dating. Identical crystals were double-checked in two facilities having significantly different degrees of neutron flux thermalization: Irradiation Pit-6 (IP-6) of the Korea Atomic Energy Research Institute (KAERI) TRIGA III reactor and the Graphite Pneumatic Tube (GrPn) of the Kyoto University Research Reactor (KUR-<em>1</em>) which have Cd ratios of 12.5 and ∼200, respectively, for Au. The final single weighted mean ζ baselines are given with errors (2σ) as: 324.5 ± 7.9 for SRM<em>612</em>, 110.9±2.7 for CN<em>1</em> and 118.8±2.9 for CN<em>2</em> from KAERI IP-<em>6</em>; and 333.7±8.5 for SRM<em>612</em>, 109.0±2.8 for CN<em>1</em> and 119.5 ± 3.1 for CN<em>2</em> from KUR GrPn. The final results from both facilities show anexcellent consistency in ζs for CN<em>1</em> and CN<em>2</em> and a discrepancy ( ∼2.8%) in SRM<em>612</em>-ζ values despite of a rough agreement within the error (2σ). Lower ratios (∼2.5–4%) of <em>ϱ</em><sub>d</sub><sup>CN1</sup>/<em>ϱ</em><sub>d</sub><sup><em>SRM</em></sup>612, <em>ϱ</em><sub>d</sub><sup>CN2</sup>/<em>ϱ</em><sub>d</sub><sup>SRM612</sup> and <em>ϱ</em><sub>i</sub><sup>mineral</sup>/<em>ϱ</em><sub>d<sup><em>SRM</em>612</sup></sub> in KAERI IP-<em>6</em> strongly imply such a decrease of <em>ζ</em><sub>SRM6<em>l</em>2</sub>.</p><p>The consistency in <em>ζ</em><sub>CN1</sub> and <em>ζ</em><sub>CN2</sub> in both facilities implies that the large difference in <sup>232</sup>Th/<sup>235</sup>5U ratio between the mineral and CN<em>1</em> or CN<em>2</em> may not significantly affect thermal neutron dosimetry, even for apatite which has the largest difference of the ratio against dosimeter glasses. The larger (n,f ) reaction cross-section of <sup>238</sup>U than that of <sup>232</sup>2Th in epithermal and fast neutron energy regions also suggests that the difference of <sup>238</sup>U /<sup>235</sup>U ratio as seen in glass SRM<em>612</em>, which has depleted U, may affect the thermal neutron dosimetry more significantly than that of <sup>232</sup>Th/<sup>235</sup>U ratio regardless of Th/U ratios of the three minerals. Therefore, the discrepancy in <em>ζ</em><sub>SRM</sub>612 results mainly from the larger contribution of <sup>238</sup>U fission induced by non-thermal neutrons to the thermal neutron dosimetry in the less thermalized KAERI IP-<em>6</em>. In consequence, the final <em>ζ</em><sub>SRM6<em>l</em>1</sub> from KAERI IP-<em>6</em> is significantly less precise. The final ζ baselines for CN<em>1</em> and CN<em>2</em>, obtained independently from both facilities, are to be recommended for accurate fission-track analyses in preference to the SRM<em>612</em>-ζ baseline, even in the well-thermalized facility, e.g. KUR GrPn.</p></div>\",\"PeriodicalId\":100231,\"journal\":{\"name\":\"Chemical Geology: Isotope Geoscience section\",\"volume\":\"87 3\",\"pages\":\"Pages 147-166\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1991-10-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0168-9622(91)90018-R\",\"citationCount\":\"5\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Chemical Geology: Isotope Geoscience section\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/016896229190018R\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemical Geology: Isotope Geoscience section","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/016896229190018R","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Direct comparison of zeta calibration constants for fission-track dating by double-checking of two irradiation facilities with different degrees of neutron flux thermalization
Zeta (ζ) constants were determined using zircon, apatite and sphene age standards for a systematic calibration of fission-track dating. Identical crystals were double-checked in two facilities having significantly different degrees of neutron flux thermalization: Irradiation Pit-6 (IP-6) of the Korea Atomic Energy Research Institute (KAERI) TRIGA III reactor and the Graphite Pneumatic Tube (GrPn) of the Kyoto University Research Reactor (KUR-1) which have Cd ratios of 12.5 and ∼200, respectively, for Au. The final single weighted mean ζ baselines are given with errors (2σ) as: 324.5 ± 7.9 for SRM612, 110.9±2.7 for CN1 and 118.8±2.9 for CN2 from KAERI IP-6; and 333.7±8.5 for SRM612, 109.0±2.8 for CN1 and 119.5 ± 3.1 for CN2 from KUR GrPn. The final results from both facilities show anexcellent consistency in ζs for CN1 and CN2 and a discrepancy ( ∼2.8%) in SRM612-ζ values despite of a rough agreement within the error (2σ). Lower ratios (∼2.5–4%) of ϱdCN1/ϱdSRM612, ϱdCN2/ϱdSRM612 and ϱimineral/ϱdSRM612 in KAERI IP-6 strongly imply such a decrease of ζSRM6l2.
The consistency in ζCN1 and ζCN2 in both facilities implies that the large difference in 232Th/2355U ratio between the mineral and CN1 or CN2 may not significantly affect thermal neutron dosimetry, even for apatite which has the largest difference of the ratio against dosimeter glasses. The larger (n,f ) reaction cross-section of 238U than that of 2322Th in epithermal and fast neutron energy regions also suggests that the difference of 238U /235U ratio as seen in glass SRM612, which has depleted U, may affect the thermal neutron dosimetry more significantly than that of 232Th/235U ratio regardless of Th/U ratios of the three minerals. Therefore, the discrepancy in ζSRM612 results mainly from the larger contribution of 238U fission induced by non-thermal neutrons to the thermal neutron dosimetry in the less thermalized KAERI IP-6. In consequence, the final ζSRM6l1 from KAERI IP-6 is significantly less precise. The final ζ baselines for CN1 and CN2, obtained independently from both facilities, are to be recommended for accurate fission-track analyses in preference to the SRM612-ζ baseline, even in the well-thermalized facility, e.g. KUR GrPn.