Matches in SemOpenAlex for { <https://semopenalex.org/work/W1991232829> ?p ?o ?g. }
- W1991232829 endingPage "92" @default.
- W1991232829 startingPage "84" @default.
- W1991232829 abstract "Clay mineralogy of 54 fluvial samples collected from 20 major rivers on Hainan Island are investigated in order to determine compositional changes of clay minerals and to assess the weathering processes. The clay mineral assemblages consist dominantly of kaolinite (31–66%), with a lesser abundance of chlorite (22–44%) and illite (4–33%), and a trace amount of smectite (0–15%). Fluvial sediments from the east and northwest of Hainan Island are characterized by a higher kaolinite content and illite chemical index and poorer illite crystallinity than those from southwest Hainan. Only minor smectite (mean of 7%) occurs in the sediments from west Hainan; smectite is total lacking in east Hainan. Compared with the adjacent basins, Hainan Island is characterized by moderate to intensive chemical weathering with strong hydrolysis. Our results suggest that rainfall is the principal factor controlling the intensity of chemical weathering on Hainan Island, with more intense chemical weathering occurring in eastern and northwestern Hainan. Another practical implication of this study is that it provides a “missing” end member (Hainan Island) in the provenance discrimination study focused on the northern South China Sea (SCS). Hainan fine-grained sediments likely play an important role in providing clay minerals to the northern SCS carried by the South China Sea Warm Current (SCSWC) during the summer." @default.
- W1991232829 created "2016-06-24" @default.
- W1991232829 creator A5005179076 @default.
- W1991232829 creator A5008292426 @default.
- W1991232829 creator A5009317905 @default.
- W1991232829 creator A5014670897 @default.
- W1991232829 creator A5025307595 @default.
- W1991232829 creator A5027835055 @default.
- W1991232829 creator A5048659414 @default.
- W1991232829 creator A5061628455 @default.
- W1991232829 creator A5072707334 @default.
- W1991232829 creator A5076607125 @default.
- W1991232829 date "2014-12-01" @default.
- W1991232829 modified "2023-10-14" @default.
- W1991232829 title "Clay mineralogy of the riverine sediments of Hainan Island, South China Sea: Implications for weathering and provenance" @default.
- W1991232829 cites W1563916034 @default.
- W1991232829 cites W1567579476 @default.
- W1991232829 cites W1615944818 @default.
- W1991232829 cites W1935059050 @default.
- W1991232829 cites W1967838752 @default.
- W1991232829 cites W1971284908 @default.
- W1991232829 cites W1972306362 @default.
- W1991232829 cites W1976680888 @default.
- W1991232829 cites W1986025435 @default.
- W1991232829 cites W1989970490 @default.
- W1991232829 cites W1990059612 @default.
- W1991232829 cites W1995613661 @default.
- W1991232829 cites W1996849400 @default.
- W1991232829 cites W2008685470 @default.
- W1991232829 cites W2010847048 @default.
- W1991232829 cites W2016684199 @default.
- W1991232829 cites W2017024367 @default.
- W1991232829 cites W2017922709 @default.
- W1991232829 cites W2025901524 @default.
- W1991232829 cites W2034818018 @default.
- W1991232829 cites W2039267937 @default.
- W1991232829 cites W2040651526 @default.
- W1991232829 cites W2051682718 @default.
- W1991232829 cites W2054578812 @default.
- W1991232829 cites W2061898270 @default.
- W1991232829 cites W2074079531 @default.
- W1991232829 cites W2074379113 @default.
- W1991232829 cites W2076890521 @default.
- W1991232829 cites W2077543697 @default.
- W1991232829 cites W2080710249 @default.
- W1991232829 cites W2086593238 @default.
- W1991232829 cites W2087250356 @default.
- W1991232829 cites W2089245486 @default.
- W1991232829 cites W2091185491 @default.
- W1991232829 cites W2092411281 @default.
- W1991232829 cites W2094840445 @default.
- W1991232829 cites W2099035636 @default.
- W1991232829 cites W2099251924 @default.
- W1991232829 cites W2101543912 @default.
- W1991232829 cites W2103592777 @default.
- W1991232829 cites W2103600357 @default.
- W1991232829 cites W2115454914 @default.
- W1991232829 cites W2116921785 @default.
- W1991232829 cites W2120970192 @default.
- W1991232829 cites W2122579123 @default.
- W1991232829 cites W2129106098 @default.
- W1991232829 cites W2132557089 @default.
- W1991232829 cites W2134339307 @default.
- W1991232829 cites W2148220871 @default.
- W1991232829 cites W2153401021 @default.
- W1991232829 cites W2154572728 @default.
- W1991232829 cites W2158113457 @default.
- W1991232829 cites W2166813482 @default.
- W1991232829 cites W2379575996 @default.
- W1991232829 cites W2482109340 @default.
- W1991232829 cites W2499850477 @default.
- W1991232829 cites W2503937471 @default.
- W1991232829 cites W257504522 @default.
- W1991232829 cites W3149453667 @default.
- W1991232829 doi "https://doi.org/10.1016/j.jseaes.2014.08.036" @default.
- W1991232829 hasPublicationYear "2014" @default.
- W1991232829 type Work @default.
- W1991232829 sameAs 1991232829 @default.
- W1991232829 citedByCount "36" @default.
- W1991232829 countsByYear W19912328292016 @default.
- W1991232829 countsByYear W19912328292017 @default.
- W1991232829 countsByYear W19912328292018 @default.
- W1991232829 countsByYear W19912328292019 @default.
- W1991232829 countsByYear W19912328292020 @default.
- W1991232829 countsByYear W19912328292021 @default.
- W1991232829 countsByYear W19912328292022 @default.
- W1991232829 countsByYear W19912328292023 @default.
- W1991232829 crossrefType "journal-article" @default.
- W1991232829 hasAuthorship W1991232829A5005179076 @default.
- W1991232829 hasAuthorship W1991232829A5008292426 @default.
- W1991232829 hasAuthorship W1991232829A5009317905 @default.
- W1991232829 hasAuthorship W1991232829A5014670897 @default.
- W1991232829 hasAuthorship W1991232829A5025307595 @default.
- W1991232829 hasAuthorship W1991232829A5027835055 @default.
- W1991232829 hasAuthorship W1991232829A5048659414 @default.
- W1991232829 hasAuthorship W1991232829A5061628455 @default.
- W1991232829 hasAuthorship W1991232829A5072707334 @default.
- W1991232829 hasAuthorship W1991232829A5076607125 @default.