{"title":"塞尔维亚一些瓶装水中含有稀土元素","authors":"Maja Todorović, P. Papic, M. Ćuk, J. Stojković","doi":"10.2298/GABP1374071T","DOIUrl":null,"url":null,"abstract":"Twenty-one bottled mineral and spring waters from Serbia were analyzed for 16 \n inorganic chemical parameters, including lanthanides and yttrium which belong \n to the group of so-called rare earth elements (REE). REE concentrations in \n the bottled water samples varied over a broad range, from 5.39 to 1585.82 \n ng/L. Total concentrations in the bottled water samples were calculated \n taking into account the classification of lanthanides into heavy (HREE) and \n light (LREE), with yttrium added to the HREE group. The LREE concentrations \n ranged from 3.62 to 1449.63 ng/L, while those of the HREE were from 0 to \n 136.19 ng/L. Distinct REE signatures were observed in waters that drained \n specific rocks. The REE patterns in groundwater from granitic and related \n rocks showed LREE and HREE enrichment, while groundwater with mafic rock \n influence exhibited slightly LREE enrichment. Several bottled water samples \n featured naturally-occurring carbon dioxide, whose solutional capacity \n contributed to the highest REE concentrations in the analyzed samples. High \n REE concentrations are also a result of sudden changes in oxidation-reduction \n conditions, which particularly affect La, Ce and Eu. Aquifers developed in \n granitic and related rocks (methamorphic and sedimentary rocks) constitute \n favorable environments for HREE in groundwater, corroborated by the \n occurrence of HREE in bottled water samples. The bottled water samples \n largely exhibited a negative cerium anomaly and nearly all the samples showed \n a positive europium anomaly.","PeriodicalId":263923,"journal":{"name":"Geoloski Anali Balkanskog Poluostrva","volume":"27 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"Rare earth elements in some bottled waters of Serbia\",\"authors\":\"Maja Todorović, P. Papic, M. Ćuk, J. Stojković\",\"doi\":\"10.2298/GABP1374071T\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Twenty-one bottled mineral and spring waters from Serbia were analyzed for 16 \\n inorganic chemical parameters, including lanthanides and yttrium which belong \\n to the group of so-called rare earth elements (REE). REE concentrations in \\n the bottled water samples varied over a broad range, from 5.39 to 1585.82 \\n ng/L. Total concentrations in the bottled water samples were calculated \\n taking into account the classification of lanthanides into heavy (HREE) and \\n light (LREE), with yttrium added to the HREE group. The LREE concentrations \\n ranged from 3.62 to 1449.63 ng/L, while those of the HREE were from 0 to \\n 136.19 ng/L. Distinct REE signatures were observed in waters that drained \\n specific rocks. The REE patterns in groundwater from granitic and related \\n rocks showed LREE and HREE enrichment, while groundwater with mafic rock \\n influence exhibited slightly LREE enrichment. Several bottled water samples \\n featured naturally-occurring carbon dioxide, whose solutional capacity \\n contributed to the highest REE concentrations in the analyzed samples. High \\n REE concentrations are also a result of sudden changes in oxidation-reduction \\n conditions, which particularly affect La, Ce and Eu. Aquifers developed in \\n granitic and related rocks (methamorphic and sedimentary rocks) constitute \\n favorable environments for HREE in groundwater, corroborated by the \\n occurrence of HREE in bottled water samples. The bottled water samples \\n largely exhibited a negative cerium anomaly and nearly all the samples showed \\n a positive europium anomaly.\",\"PeriodicalId\":263923,\"journal\":{\"name\":\"Geoloski Anali Balkanskog Poluostrva\",\"volume\":\"27 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geoloski Anali Balkanskog Poluostrva\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.2298/GABP1374071T\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geoloski Anali Balkanskog Poluostrva","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2298/GABP1374071T","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Rare earth elements in some bottled waters of Serbia
Twenty-one bottled mineral and spring waters from Serbia were analyzed for 16
inorganic chemical parameters, including lanthanides and yttrium which belong
to the group of so-called rare earth elements (REE). REE concentrations in
the bottled water samples varied over a broad range, from 5.39 to 1585.82
ng/L. Total concentrations in the bottled water samples were calculated
taking into account the classification of lanthanides into heavy (HREE) and
light (LREE), with yttrium added to the HREE group. The LREE concentrations
ranged from 3.62 to 1449.63 ng/L, while those of the HREE were from 0 to
136.19 ng/L. Distinct REE signatures were observed in waters that drained
specific rocks. The REE patterns in groundwater from granitic and related
rocks showed LREE and HREE enrichment, while groundwater with mafic rock
influence exhibited slightly LREE enrichment. Several bottled water samples
featured naturally-occurring carbon dioxide, whose solutional capacity
contributed to the highest REE concentrations in the analyzed samples. High
REE concentrations are also a result of sudden changes in oxidation-reduction
conditions, which particularly affect La, Ce and Eu. Aquifers developed in
granitic and related rocks (methamorphic and sedimentary rocks) constitute
favorable environments for HREE in groundwater, corroborated by the
occurrence of HREE in bottled water samples. The bottled water samples
largely exhibited a negative cerium anomaly and nearly all the samples showed
a positive europium anomaly.