{"title":"直接- ams法测定自然产236U","authors":"X.-L. Zhao , B.B.A. Francisco","doi":"10.1016/j.nimb.2025.165763","DOIUrl":null,"url":null,"abstract":"<div><div>From a multi-isotope direct-AMS survey of 310 uranium ore concentrates (UOCs), <sup>236</sup>U/<sup>238</sup>U ratios from ∼2 × 10<sup>−12</sup> to ∼2 × 10<sup>−7</sup> are measured. However, a range from low-10<sup>−12</sup> to mid-10<sup>−10</sup> is expected from directly mined natural uranium ore minerals. This upper-end discrepancy would normally be attributed to inputs of spent fuel materials, but the numerous occurrences and the lack of economic reasons to recycle anything in the front stage of UOC production make the abnormally high <sup>236</sup>U/<sup>238</sup>U ratios rather perplexing. When plotted against the <sup>187</sup>Os/<sup>188</sup>Os ratios, which were also obtained in the survey, the high <sup>236</sup>U/<sup>238</sup>U results are seen to occur around the value of <sup>187</sup>Os/<sup>188</sup>Os ∼10, a non-random pattern as might be anticipated from unwitting contaminations. This observed correlation favors those measured high <sup>236</sup>U/<sup>238</sup>U ratios being natural, and as such, it refers to an overlooked natural <sup>238</sup>U/<sup>235</sup>U isotope fraction mechanism. Therefore, this work calls for further studies of naturally occurring <sup>236</sup>U/<sup>238</sup>U in a wider range of native uranium-bearing minerals. To secure unambiguous natural <sup>236</sup>U surveys, an approach is described that combines UF<sub>5</sub><sup>−</sup> production directly from powdered native samples and ion source reconfiguration to minimize background.</div></div>","PeriodicalId":19380,"journal":{"name":"Nuclear Instruments & Methods in Physics Research Section B-beam Interactions With Materials and Atoms","volume":"566 ","pages":"Article 165763"},"PeriodicalIF":1.4000,"publicationDate":"2025-06-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Survey of naturally occurring 236U with direct-AMS\",\"authors\":\"X.-L. Zhao , B.B.A. Francisco\",\"doi\":\"10.1016/j.nimb.2025.165763\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>From a multi-isotope direct-AMS survey of 310 uranium ore concentrates (UOCs), <sup>236</sup>U/<sup>238</sup>U ratios from ∼2 × 10<sup>−12</sup> to ∼2 × 10<sup>−7</sup> are measured. However, a range from low-10<sup>−12</sup> to mid-10<sup>−10</sup> is expected from directly mined natural uranium ore minerals. This upper-end discrepancy would normally be attributed to inputs of spent fuel materials, but the numerous occurrences and the lack of economic reasons to recycle anything in the front stage of UOC production make the abnormally high <sup>236</sup>U/<sup>238</sup>U ratios rather perplexing. When plotted against the <sup>187</sup>Os/<sup>188</sup>Os ratios, which were also obtained in the survey, the high <sup>236</sup>U/<sup>238</sup>U results are seen to occur around the value of <sup>187</sup>Os/<sup>188</sup>Os ∼10, a non-random pattern as might be anticipated from unwitting contaminations. This observed correlation favors those measured high <sup>236</sup>U/<sup>238</sup>U ratios being natural, and as such, it refers to an overlooked natural <sup>238</sup>U/<sup>235</sup>U isotope fraction mechanism. Therefore, this work calls for further studies of naturally occurring <sup>236</sup>U/<sup>238</sup>U in a wider range of native uranium-bearing minerals. To secure unambiguous natural <sup>236</sup>U surveys, an approach is described that combines UF<sub>5</sub><sup>−</sup> production directly from powdered native samples and ion source reconfiguration to minimize background.</div></div>\",\"PeriodicalId\":19380,\"journal\":{\"name\":\"Nuclear Instruments & Methods in Physics Research Section B-beam Interactions With Materials and Atoms\",\"volume\":\"566 \",\"pages\":\"Article 165763\"},\"PeriodicalIF\":1.4000,\"publicationDate\":\"2025-06-03\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Nuclear Instruments & Methods in Physics Research Section B-beam Interactions With Materials and Atoms\",\"FirstCategoryId\":\"101\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0168583X25001533\",\"RegionNum\":3,\"RegionCategory\":\"物理与天体物理\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"INSTRUMENTS & INSTRUMENTATION\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Nuclear Instruments & Methods in Physics Research Section B-beam Interactions With Materials and Atoms","FirstCategoryId":"101","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0168583X25001533","RegionNum":3,"RegionCategory":"物理与天体物理","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"INSTRUMENTS & INSTRUMENTATION","Score":null,"Total":0}
Survey of naturally occurring 236U with direct-AMS
From a multi-isotope direct-AMS survey of 310 uranium ore concentrates (UOCs), 236U/238U ratios from ∼2 × 10−12 to ∼2 × 10−7 are measured. However, a range from low-10−12 to mid-10−10 is expected from directly mined natural uranium ore minerals. This upper-end discrepancy would normally be attributed to inputs of spent fuel materials, but the numerous occurrences and the lack of economic reasons to recycle anything in the front stage of UOC production make the abnormally high 236U/238U ratios rather perplexing. When plotted against the 187Os/188Os ratios, which were also obtained in the survey, the high 236U/238U results are seen to occur around the value of 187Os/188Os ∼10, a non-random pattern as might be anticipated from unwitting contaminations. This observed correlation favors those measured high 236U/238U ratios being natural, and as such, it refers to an overlooked natural 238U/235U isotope fraction mechanism. Therefore, this work calls for further studies of naturally occurring 236U/238U in a wider range of native uranium-bearing minerals. To secure unambiguous natural 236U surveys, an approach is described that combines UF5− production directly from powdered native samples and ion source reconfiguration to minimize background.
期刊介绍:
Section B of Nuclear Instruments and Methods in Physics Research covers all aspects of the interaction of energetic beams with atoms, molecules and aggregate forms of matter. This includes ion beam analysis and ion beam modification of materials as well as basic data of importance for these studies. Topics of general interest include: atomic collisions in solids, particle channelling, all aspects of collision cascades, the modification of materials by energetic beams, ion implantation, irradiation - induced changes in materials, the physics and chemistry of beam interactions and the analysis of materials by all forms of energetic radiation. Modification by ion, laser and electron beams for the study of electronic materials, metals, ceramics, insulators, polymers and other important and new materials systems are included. Related studies, such as the application of ion beam analysis to biological, archaeological and geological samples as well as applications to solve problems in planetary science are also welcome. Energetic beams of interest include atomic and molecular ions, neutrons, positrons and muons, plasmas directed at surfaces, electron and photon beams, including laser treated surfaces and studies of solids by photon radiation from rotating anodes, synchrotrons, etc. In addition, the interaction between various forms of radiation and radiation-induced deposition processes are relevant.