{"title":"格陵兰岛Dye 3地区雪中铅来源的季节变化","authors":"K.J.R Rosman , W Chisholm , C.F Boutron , J.-P Candelone , J.-L Jaffrezo , C.I Davidson","doi":"10.1016/S0012-821X(98)00098-3","DOIUrl":null,"url":null,"abstract":"<div><p><span><span>The isotopic composition and concentration of lead has been measured in fresh and slightly aged snow collected at Dye 3 in southern Greenland during one full year. The lead concentration displayed large variations ranging from 14–3016 pg/g in April (spring) to 3–6 pg/g in September (summer) while the </span>isotopic ratios changed in regular manner during the year. The </span><sup>206</sup>Pb/<sup>207</sup>Pb ratios were ∼1.15 from spring to mid-summer snow, and increased in late summer to early autumn, reaching ∼1.20 in winter. These isotopic data indicate that the lead in the autumn to winter snow originated in North America, while that in spring to mid-summer snow is from Eurasia.</p></div>","PeriodicalId":11481,"journal":{"name":"Earth and Planetary Science Letters","volume":"160 3","pages":"Pages 383-389"},"PeriodicalIF":4.8000,"publicationDate":"1998-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S0012-821X(98)00098-3","citationCount":"40","resultStr":"{\"title\":\"Seasonal variations in the origin of lead in snow at Dye 3, Greenland\",\"authors\":\"K.J.R Rosman , W Chisholm , C.F Boutron , J.-P Candelone , J.-L Jaffrezo , C.I Davidson\",\"doi\":\"10.1016/S0012-821X(98)00098-3\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p><span><span>The isotopic composition and concentration of lead has been measured in fresh and slightly aged snow collected at Dye 3 in southern Greenland during one full year. The lead concentration displayed large variations ranging from 14–3016 pg/g in April (spring) to 3–6 pg/g in September (summer) while the </span>isotopic ratios changed in regular manner during the year. The </span><sup>206</sup>Pb/<sup>207</sup>Pb ratios were ∼1.15 from spring to mid-summer snow, and increased in late summer to early autumn, reaching ∼1.20 in winter. These isotopic data indicate that the lead in the autumn to winter snow originated in North America, while that in spring to mid-summer snow is from Eurasia.</p></div>\",\"PeriodicalId\":11481,\"journal\":{\"name\":\"Earth and Planetary Science Letters\",\"volume\":\"160 3\",\"pages\":\"Pages 383-389\"},\"PeriodicalIF\":4.8000,\"publicationDate\":\"1998-08-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/S0012-821X(98)00098-3\",\"citationCount\":\"40\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Earth and Planetary Science Letters\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0012821X98000983\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earth and Planetary Science Letters","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0012821X98000983","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Seasonal variations in the origin of lead in snow at Dye 3, Greenland
The isotopic composition and concentration of lead has been measured in fresh and slightly aged snow collected at Dye 3 in southern Greenland during one full year. The lead concentration displayed large variations ranging from 14–3016 pg/g in April (spring) to 3–6 pg/g in September (summer) while the isotopic ratios changed in regular manner during the year. The 206Pb/207Pb ratios were ∼1.15 from spring to mid-summer snow, and increased in late summer to early autumn, reaching ∼1.20 in winter. These isotopic data indicate that the lead in the autumn to winter snow originated in North America, while that in spring to mid-summer snow is from Eurasia.
期刊介绍:
Earth and Planetary Science Letters (EPSL) is a leading journal for researchers across the entire Earth and planetary sciences community. It publishes concise, exciting, high-impact articles ("Letters") of broad interest. Its focus is on physical and chemical processes, the evolution and general properties of the Earth and planets - from their deep interiors to their atmospheres. EPSL also includes a Frontiers section, featuring invited high-profile synthesis articles by leading experts on timely topics to bring cutting-edge research to the wider community.