FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3126394004> ?p ?o ?g. }

• W3126394004 endingPage "104897" @default.
• W3126394004 startingPage "104897" @default.
• W3126394004 abstract "The mineralogical and geochemical compositions of an 11.5 m black shale weathering profile on the northern Yangtze platform, China, are documented to investigate the fate of rare earth elements and yttrium (REY) and their potential implications during chemical weathering. Our results signify that the profile has experienced an expected weathering trend in initial to moderate weathering stages based on the chemical index of alteration (CIA) values (54.45–75.50). Major elements (Ca, Mg, Na and K) have been leached to various degrees throughout the profile, roughly coupled with the weathering trends of primary minerals. Most REY were released from the black shale matrix, transported downwards and partially precipitated in a fracture. Lanthanum, Ce and Pr exhibited less mobility than other REY, which was connected with the weathering-resistant rhabdophane ((La,Ce)PO4). The REY enrichment in the fracture resulted from the adsorption of Fe–Mn oxyhydroxides and kaolinite. Negligible Ce anomalies (Ce/Ce* values of 0.95–1.12) and prominent negative Eu anomalies (Eu/Eu* values of 0.40–0.77) are observed throughout the profile. The Ce/Ce* values are covariant with the sizes of the first tetrad effect, while Eu anomalies were inherited from the bedrock, and the variation in Eu/Eu* values is related to plagioclase dissolution. LREE/HREE, Sm/Nd and Y/Ho fractionation occurred during black shale weathering. The LREE/HREE fractionation was mainly controlled by primary and secondary minerals (e.g., rhabdophane and kaolinite). The Sm–Nd and Y–Ho fractionation was affected by the tetrad effect. Fracture zones in black shales would be new potential targets for REY prospecting and extraction. Highly REY-enriched zones may occur in soils and underground aquifers, which would pose potential threats to crops and humans. Our findings, combined with previous studies, suggest that LREE/HREE fractionation is indicative of the weathering degree of continental rocks." @default.
• W3126394004 created "2021-02-15" @default.
• W3126394004 creator A5003799076 @default.
• W3126394004 creator A5009966429 @default.
• W3126394004 creator A5017359249 @default.
• W3126394004 creator A5037337966 @default.
• W3126394004 creator A5082689595 @default.
• W3126394004 date "2021-03-01" @default.
• W3126394004 modified "2023-10-14" @default.
• W3126394004 title "Investigations on mineralogy and geochemistry of a black shale profile on the northern Yangtze platform, China: Weathering fate of rare earth elements and yttrium (REY) and its implications" @default.
• W3126394004 cites W1063180586 @default.
• W3126394004 cites W1968437447 @default.
• W3126394004 cites W1969021495 @default.
• W3126394004 cites W1970531672 @default.
• W3126394004 cites W1973708310 @default.
• W3126394004 cites W1975730675 @default.
• W3126394004 cites W1975773022 @default.
• W3126394004 cites W1977457396 @default.
• W3126394004 cites W1982487268 @default.
• W3126394004 cites W1982636518 @default.
• W3126394004 cites W1984347866 @default.
• W3126394004 cites W1985727402 @default.
• W3126394004 cites W1989278070 @default.
• W3126394004 cites W1995865323 @default.
• W3126394004 cites W1996706541 @default.
• W3126394004 cites W1998172208 @default.
• W3126394004 cites W1999236298 @default.
• W3126394004 cites W1999708461 @default.
• W3126394004 cites W2000448055 @default.
• W3126394004 cites W2002647826 @default.
• W3126394004 cites W2003832228 @default.
• W3126394004 cites W2006081057 @default.
• W3126394004 cites W2011098114 @default.
• W3126394004 cites W2015996529 @default.
• W3126394004 cites W2019758284 @default.
• W3126394004 cites W2020228038 @default.
• W3126394004 cites W2020806066 @default.
• W3126394004 cites W2024818652 @default.
• W3126394004 cites W2029401070 @default.
• W3126394004 cites W2035859777 @default.
• W3126394004 cites W2038631041 @default.
• W3126394004 cites W2043747056 @default.
• W3126394004 cites W2046892047 @default.
• W3126394004 cites W2048898834 @default.
• W3126394004 cites W2051783195 @default.
• W3126394004 cites W2057482300 @default.
• W3126394004 cites W2058924927 @default.
• W3126394004 cites W2059675029 @default.
• W3126394004 cites W2062477123 @default.
• W3126394004 cites W2064123750 @default.
• W3126394004 cites W2068643896 @default.
• W3126394004 cites W2069136944 @default.
• W3126394004 cites W2071103381 @default.
• W3126394004 cites W2073386517 @default.
• W3126394004 cites W2073863738 @default.
• W3126394004 cites W2077125391 @default.
• W3126394004 cites W207824156 @default.
• W3126394004 cites W2078410096 @default.
• W3126394004 cites W2080570970 @default.
• W3126394004 cites W2082198109 @default.
• W3126394004 cites W2084849445 @default.
• W3126394004 cites W2086305547 @default.
• W3126394004 cites W2087937118 @default.
• W3126394004 cites W2091609376 @default.
• W3126394004 cites W2095417184 @default.
• W3126394004 cites W2097935007 @default.
• W3126394004 cites W2106597225 @default.
• W3126394004 cites W2113881893 @default.
• W3126394004 cites W2128239598 @default.
• W3126394004 cites W2133379437 @default.
• W3126394004 cites W2138072110 @default.
• W3126394004 cites W2151810991 @default.
• W3126394004 cites W2158056165 @default.
• W3126394004 cites W2165933596 @default.
• W3126394004 cites W2172110645 @default.
• W3126394004 cites W2282036201 @default.
• W3126394004 cites W2461461739 @default.
• W3126394004 cites W2606434384 @default.
• W3126394004 cites W2671517711 @default.
• W3126394004 cites W2774916246 @default.
• W3126394004 cites W2800594372 @default.
• W3126394004 cites W2807817165 @default.
• W3126394004 cites W2807863588 @default.
• W3126394004 cites W2903415012 @default.
• W3126394004 cites W2914301057 @default.
• W3126394004 cites W2962844003 @default.
• W3126394004 cites W2968043419 @default.
• W3126394004 cites W2990004904 @default.
• W3126394004 cites W2996270733 @default.
• W3126394004 cites W3008680885 @default.
• W3126394004 doi "https://doi.org/10.1016/j.apgeochem.2021.104897" @default.
• W3126394004 hasPublicationYear "2021" @default.
• W3126394004 type Work @default.
• W3126394004 sameAs 3126394004 @default.
• W3126394004 citedByCount "8" @default.
• W3126394004 countsByYear W31263940042021 @default.
• W3126394004 countsByYear W31263940042022 @default.
• W3126394004 countsByYear W31263940042023 @default.

• next