FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2053553204> ?p ?o ?g. }

• W2053553204 endingPage "994" @default.
• W2053553204 startingPage "975" @default.
• W2053553204 abstract "The sparkling waters from the area of Kyselka near Karlovy Vary at the western slope of the Doupovske hory, Bohemia (Czech Republic), and CO2-poor waters from two underground boreholes at Jachymov, Krusne hory, Bohemia, have been studied with the aim of characterizing the distribution of rare earth elements, yttrium, and H, O, C, Sr, Nd, Pb isotopes during the low-temperature alteration processes of the host rocks. Additionally, leaching experiments were performed at pH 3 on the granitic and basaltic host rocks from Kyselka and the granite of Jachymov. All REE patterns of the granite- and the basalt-derived waters from the Kyselka area are different from those of their source rocks and the leachates of the latter. This elucidates the inhomogeneous distribution of REE and Y among the solid phases in the altered magmatic rocks. The Eu and Ce anomalies in granite-derived waters are inherited, the Y anomaly is achieved by fluid migration. Yttrium is always preferentially leached by mineral waters, whereas Y/Ho ratios of rocks and their leachates are very similar. The REE abundances in waters from the wells in Jachymov are derived from rocks intensely leached and depleted in easily soluble REE-bearing minerals, whereas the granites and basalts from Kyselka still contain soluble, REE-bearing minerals. A comparison of REE/Ca patterns of the experimental leachates with those of the mineral waters elucidate the high retention of REE in rocks during water–rock interaction. In strongly altered rocks Sr isotope ratios of mineral waters and rocks differ widely, whereas the corresponding Nd isotope ratios are very similar. 207Pb/208Pb, 206Pb/208Pb and 206Pb/207Pb ratios in mineral waters are independent from U/Th ratios in the rocks. 206Pb/208Pb and 206Pb/207Pb are lower in mineral waters than in their source rocks and their leachates, which indicates that Pb is primarily derived from solid phases that do not contain significant contents of leachable U and Th. Thus, mineral waters, although CO2 rich, only interact with surface films on minerals and not with the bulk of the minerals as in the leaching experiments. Calculation of mixing ratios of waters from the granitic and basaltic sources of the waters from the Kyselka area yield about 40% of water from the underlying granite in water recovered from the basalt, whereas the granite-derived water is mixed with only about 5% of the water from the basalt." @default.
• W2053553204 created "2016-06-24" @default.
• W2053553204 creator A5009491361 @default.
• W2053553204 creator A5019493496 @default.
• W2053553204 creator A5033749512 @default.
• W2053553204 creator A5056006366 @default.
• W2053553204 creator A5078648527 @default.
• W2053553204 date "1998-11-01" @default.
• W2053553204 modified "2023-10-18" @default.
• W2053553204 title "Rare earth elements, yttrium and H, O, C, Sr, Nd and Pb isotope studies in mineral waters and corresponding rocks from NW-Bohemia, Czech Republic" @default.
• W2053553204 cites W112581710 @default.
• W2053553204 cites W1964654012 @default.
• W2053553204 cites W1967192702 @default.
• W2053553204 cites W1970833454 @default.
• W2053553204 cites W1976312343 @default.
• W2053553204 cites W1988140719 @default.
• W2053553204 cites W1988378253 @default.
• W2053553204 cites W1994109027 @default.
• W2053553204 cites W1996695872 @default.
• W2053553204 cites W2005894404 @default.
• W2053553204 cites W2009073384 @default.
• W2053553204 cites W2009968238 @default.
• W2053553204 cites W2011367341 @default.
• W2053553204 cites W2014081310 @default.
• W2053553204 cites W2014855638 @default.
• W2053553204 cites W2016003875 @default.
• W2053553204 cites W2034079431 @default.
• W2053553204 cites W2039728532 @default.
• W2053553204 cites W2040184093 @default.
• W2053553204 cites W2043646032 @default.
• W2053553204 cites W2044933256 @default.
• W2053553204 cites W2050511855 @default.
• W2053553204 cites W2051410899 @default.
• W2053553204 cites W2054361831 @default.
• W2053553204 cites W2055116388 @default.
• W2053553204 cites W2058088400 @default.
• W2053553204 cites W2060094561 @default.
• W2053553204 cites W2061895284 @default.
• W2053553204 cites W2062020322 @default.
• W2053553204 cites W2065472702 @default.
• W2053553204 cites W2069282443 @default.
• W2053553204 cites W2070341572 @default.
• W2053553204 cites W2071103381 @default.
• W2053553204 cites W2071172756 @default.
• W2053553204 cites W2075386023 @default.
• W2053553204 cites W2084481447 @default.
• W2053553204 cites W2086145083 @default.
• W2053553204 cites W2087307320 @default.
• W2053553204 cites W2090231649 @default.
• W2053553204 cites W2141947981 @default.
• W2053553204 cites W2159980779 @default.
• W2053553204 cites W2217959321 @default.
• W2053553204 cites W4293252316 @default.
• W2053553204 doi "https://doi.org/10.1016/s0883-2927(98)00024-9" @default.
• W2053553204 hasPublicationYear "1998" @default.
• W2053553204 type Work @default.
• W2053553204 sameAs 2053553204 @default.
• W2053553204 citedByCount "31" @default.
• W2053553204 countsByYear W20535532042013 @default.
• W2053553204 countsByYear W20535532042014 @default.
• W2053553204 countsByYear W20535532042015 @default.
• W2053553204 countsByYear W20535532042016 @default.
• W2053553204 countsByYear W20535532042017 @default.
• W2053553204 countsByYear W20535532042018 @default.
• W2053553204 countsByYear W20535532042019 @default.
• W2053553204 countsByYear W20535532042020 @default.
• W2053553204 countsByYear W20535532042021 @default.
• W2053553204 countsByYear W20535532042022 @default.
• W2053553204 crossrefType "journal-article" @default.
• W2053553204 hasAuthorship W2053553204A5009491361 @default.
• W2053553204 hasAuthorship W2053553204A5019493496 @default.
• W2053553204 hasAuthorship W2053553204A5033749512 @default.
• W2053553204 hasAuthorship W2053553204A5056006366 @default.
• W2053553204 hasAuthorship W2053553204A5078648527 @default.
• W2053553204 hasConcept C120806208 @default.
• W2053553204 hasConcept C127313418 @default.
• W2053553204 hasConcept C159390177 @default.
• W2053553204 hasConcept C159750122 @default.
• W2053553204 hasConcept C161509811 @default.
• W2053553204 hasConcept C17409809 @default.
• W2053553204 hasConcept C177921069 @default.
• W2053553204 hasConcept C178790620 @default.
• W2053553204 hasConcept C185592680 @default.
• W2053553204 hasConcept C192241223 @default.
• W2053553204 hasConcept C199289684 @default.
• W2053553204 hasConcept C2776432453 @default.
• W2053553204 hasConcept C2779851234 @default.
• W2053553204 hasConcept C2983155866 @default.
• W2053553204 hasConcept C40724407 @default.
• W2053553204 hasConcept C42787717 @default.
• W2053553204 hasConcept C531131001 @default.
• W2053553204 hasConcept C90982505 @default.
• W2053553204 hasConceptScore W2053553204C120806208 @default.
• W2053553204 hasConceptScore W2053553204C127313418 @default.
• W2053553204 hasConceptScore W2053553204C159390177 @default.
• W2053553204 hasConceptScore W2053553204C159750122 @default.
• W2053553204 hasConceptScore W2053553204C161509811 @default.
• W2053553204 hasConceptScore W2053553204C17409809 @default.

• next