Y. Miyamoto, K. Yasuda, M. Magara, T. Kimura, S. Usuda
{"title":"用阴离子交换柱顺序分离U、Th、Pb和镧系元素","authors":"Y. Miyamoto, K. Yasuda, M. Magara, T. Kimura, S. Usuda","doi":"10.14494/JNRS.10.2_7","DOIUrl":null,"url":null,"abstract":"Uranium (U), thorium (Th), lead (Pb), and the lanthanides are key elements in geochemistry and cosmochemistry. Abundance ratios and isotopic ratios of these elements in rocks, meteorites, and airborne dust are used for estimating their origin, 1-3 dating of mineral formation, 4 history of mineralization, 58 and age determination of nuclear materials. 9-11","PeriodicalId":16569,"journal":{"name":"Journal of nuclear and radiochemical sciences","volume":"48 1","pages":"2"},"PeriodicalIF":0.0000,"publicationDate":"2009-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"5","resultStr":"{\"title\":\"Sequential Separation of U, Th, Pb, and Lanthanides with a Single Anion-Exchange Column\",\"authors\":\"Y. Miyamoto, K. Yasuda, M. Magara, T. Kimura, S. Usuda\",\"doi\":\"10.14494/JNRS.10.2_7\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Uranium (U), thorium (Th), lead (Pb), and the lanthanides are key elements in geochemistry and cosmochemistry. Abundance ratios and isotopic ratios of these elements in rocks, meteorites, and airborne dust are used for estimating their origin, 1-3 dating of mineral formation, 4 history of mineralization, 58 and age determination of nuclear materials. 9-11\",\"PeriodicalId\":16569,\"journal\":{\"name\":\"Journal of nuclear and radiochemical sciences\",\"volume\":\"48 1\",\"pages\":\"2\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2009-12-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"5\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of nuclear and radiochemical sciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.14494/JNRS.10.2_7\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of nuclear and radiochemical sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.14494/JNRS.10.2_7","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Sequential Separation of U, Th, Pb, and Lanthanides with a Single Anion-Exchange Column
Uranium (U), thorium (Th), lead (Pb), and the lanthanides are key elements in geochemistry and cosmochemistry. Abundance ratios and isotopic ratios of these elements in rocks, meteorites, and airborne dust are used for estimating their origin, 1-3 dating of mineral formation, 4 history of mineralization, 58 and age determination of nuclear materials. 9-11