Matches in SemOpenAlex for { <https://semopenalex.org/work/W2300919321> ?p ?o ?g. }
- W2300919321 endingPage "548" @default.
- W2300919321 startingPage "534" @default.
- W2300919321 abstract "Remote marine aerosol samples (total suspended particles) were collected during a cruise in the central Pacific from Japan to Mexico (1°59′N–35°N and 171°54′E–90°58′W). The aerosol samples were analyzed for dicarboxylic acids (C2–C11), ω-oxoacids, pyruvic acid, α-dicarbonyls, and fatty acids as well as organic and elemental carbon, water-soluble organic carbon, and total nitrogen (WSTN). During the study, diacids were the most abundant compound class followed by fatty acids, ω-oxoacids, and α-dicarbonyls. Molecular compositions of diacids showed a predominance of oxalic (C2) acid followed by malonic (C3) and succinic (C4) acids. Oxalic acid comprises 74% of total diacids. This result suggests that photochemical production of oxalic acid is significant over the central Pacific. Spatial distributions of diacids, ω-oxoacids, pyruvic acid, α-dicarbonyls, and fatty acids together with total carbon and WSTN showed higher abundances in the eastern equatorial Pacific where the upwelling of high-nutrient waters followed by high biological productivity is common, indicating that their in situ production is important in the warmer central Pacific through photochemical oxidation from their gaseous and particulate precursors. This study demonstrates that there is a strong linkage in biogeochemical cycles of carbon in the sea-air interface via ocean upwelling, phytoplankton productivity, sea-to-air emissions of organic matter, and formation of secondary organic aerosols in the eastern equatorial Pacific." @default.
- W2300919321 created "2016-06-24" @default.
- W2300919321 creator A5021555258 @default.
- W2300919321 creator A5047201907 @default.
- W2300919321 date "2016-03-01" @default.
- W2300919321 modified "2023-10-14" @default.
- W2300919321 title "Longitudinal distributions of dicarboxylic acids,<i>ω</i>-oxoacids, pyruvic acid,<i>α</i>-dicarbonyls, and fatty acids in the marine aerosols from the central Pacific including equatorial upwelling" @default.
- W2300919321 cites W1619936992 @default.
- W2300919321 cites W1964400493 @default.
- W2300919321 cites W1969883708 @default.
- W2300919321 cites W1971266541 @default.
- W2300919321 cites W1974703729 @default.
- W2300919321 cites W1975262842 @default.
- W2300919321 cites W1975581786 @default.
- W2300919321 cites W1978690291 @default.
- W2300919321 cites W1980725928 @default.
- W2300919321 cites W1985636284 @default.
- W2300919321 cites W1986326162 @default.
- W2300919321 cites W1998026389 @default.
- W2300919321 cites W1999102942 @default.
- W2300919321 cites W2000074954 @default.
- W2300919321 cites W2000931437 @default.
- W2300919321 cites W2003692005 @default.
- W2300919321 cites W2005612323 @default.
- W2300919321 cites W2005820608 @default.
- W2300919321 cites W2008579740 @default.
- W2300919321 cites W2011589420 @default.
- W2300919321 cites W2012966691 @default.
- W2300919321 cites W2013306321 @default.
- W2300919321 cites W2013858314 @default.
- W2300919321 cites W2018337903 @default.
- W2300919321 cites W2019130702 @default.
- W2300919321 cites W2021800968 @default.
- W2300919321 cites W2032415871 @default.
- W2300919321 cites W2037973147 @default.
- W2300919321 cites W2042331645 @default.
- W2300919321 cites W2042898683 @default.
- W2300919321 cites W2043882330 @default.
- W2300919321 cites W2046387947 @default.
- W2300919321 cites W2047833486 @default.
- W2300919321 cites W2048943000 @default.
- W2300919321 cites W2050900007 @default.
- W2300919321 cites W2052506961 @default.
- W2300919321 cites W2052961453 @default.
- W2300919321 cites W2053856375 @default.
- W2300919321 cites W2057973658 @default.
- W2300919321 cites W2062279169 @default.
- W2300919321 cites W2063359930 @default.
- W2300919321 cites W2065011172 @default.
- W2300919321 cites W2066277002 @default.
- W2300919321 cites W2072726267 @default.
- W2300919321 cites W2075668796 @default.
- W2300919321 cites W2081647409 @default.
- W2300919321 cites W2082257375 @default.
- W2300919321 cites W2082459819 @default.
- W2300919321 cites W2092401329 @default.
- W2300919321 cites W2095363507 @default.
- W2300919321 cites W2095540598 @default.
- W2300919321 cites W2098088485 @default.
- W2300919321 cites W2101328904 @default.
- W2300919321 cites W2104486009 @default.
- W2300919321 cites W2109404362 @default.
- W2300919321 cites W2110878334 @default.
- W2300919321 cites W2116873172 @default.
- W2300919321 cites W2123019220 @default.
- W2300919321 cites W2123764507 @default.
- W2300919321 cites W2127055282 @default.
- W2300919321 cites W2127814074 @default.
- W2300919321 cites W2129432128 @default.
- W2300919321 cites W2133231233 @default.
- W2300919321 cites W2134464139 @default.
- W2300919321 cites W2138361360 @default.
- W2300919321 cites W2141924834 @default.
- W2300919321 cites W2143525187 @default.
- W2300919321 cites W2144883848 @default.
- W2300919321 cites W2145123870 @default.
- W2300919321 cites W2145415667 @default.
- W2300919321 cites W2151257693 @default.
- W2300919321 cites W2153888273 @default.
- W2300919321 cites W2154690810 @default.
- W2300919321 cites W2155153115 @default.
- W2300919321 cites W2155516010 @default.
- W2300919321 cites W2163361418 @default.
- W2300919321 cites W2163854746 @default.
- W2300919321 cites W2164188573 @default.
- W2300919321 cites W2167919787 @default.
- W2300919321 cites W2171810356 @default.
- W2300919321 cites W2189685544 @default.
- W2300919321 cites W4210954732 @default.
- W2300919321 doi "https://doi.org/10.1002/2015gb005346" @default.
- W2300919321 hasPublicationYear "2016" @default.
- W2300919321 type Work @default.
- W2300919321 sameAs 2300919321 @default.
- W2300919321 citedByCount "15" @default.
- W2300919321 countsByYear W23009193212017 @default.
- W2300919321 countsByYear W23009193212018 @default.
- W2300919321 countsByYear W23009193212019 @default.
- W2300919321 countsByYear W23009193212020 @default.