FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3147468044> ?p ?o ?g. }

• W3147468044 endingPage "116914" @default.
• W3147468044 startingPage "116914" @default.
• W3147468044 abstract "Atmospheric samples and surface seawater collected on a Chinese Antarctic Research Expedition (CHINARE) transect are used to investigate sources and production of nitrate ( NO 3 − ) in the atmosphere and its contribution to the surface NO 3 − pool in the ocean. Most atmospheric NO 3 − is concentrated on intermediate size particles, and much higher concentrations were observed in the northern hemisphere than in the high southern latitudes. Isotopes of NO 3 − ( δ 15 N , δ 18 O and Δ 17 O ) suggest that elevated atmospheric NO 3 − in coastal areas was associated with human activities, while NO 3 − in the high southern latitudes tends to be influenced by precursor Antarctic snowpack emissions driven by photolysis. In general, no clear association was found between the isotopes of surface seawater and atmospheric NO 3 − , suggesting that the ocean is unlikely to be an important direct source of atmospheric NO x on this transect. A significant linear relationship between δ 18 O and Δ 17 O of NO 3 − is used to interpret important pathways for NO 3 − production. In the tropics, >59% of atmospheric NO 3 − is produced via OH oxidation of NO 2 , while the elevated oxygen isotopic ratios ( δ 18 O and Δ 17 O ) in the high southern latitudes suggest increased NO 3 − production via BrO and/or DMS pathways assuming a minor contribution of the N 2 O 5 channel. In surface seawater, high NO 3 − concentrations are present in the coastal areas and in the Southern Ocean. In coastal areas of China, positive Δ 17 O values in seawater NO 3 − (1.7 ± 1.0‰) provide direct evidence of uncycled atmospheric deposition contribution, with a calculated contribution of at least 2-3% to total surface NO 3 − . A Δ 17 O = 0 was found everywhere else in seawater, suggesting that atmospheric deposition has a minimal presence in the surface NO 3 − pool. Near Antarctica, deposition of atmospheric NO 3 − with extremely low δ 15 N ( < − 30 ‰ ) could lower δ 15 N found in sea ice, and this process could be isotopically important to evaluate nitrogen cycling in sea ice. • Concentration and isotopic composition of NO 3 − show notable latitudinal gradients. • Atmospheric NO 3 − is mainly produced via OH oxidation in the tropics. • The high southern latitudes show an increased importance of BrO or DMS pathways. • Positive Δ 17 O of seawater NO 3 − is found in coastal waters and Δ 17 O ≈ 0 in other areas. • Atmospheric deposition near Antarctica can lower δ 15 N of NO 3 − in sea ice." @default.
• W3147468044 created "2021-04-13" @default.
• W3147468044 creator A5004357577 @default.
• W3147468044 creator A5015415143 @default.
• W3147468044 creator A5024056919 @default.
• W3147468044 creator A5025752123 @default.
• W3147468044 creator A5034308130 @default.
• W3147468044 creator A5035639413 @default.
• W3147468044 creator A5049168798 @default.
• W3147468044 creator A5055734137 @default.
• W3147468044 creator A5056620408 @default.
• W3147468044 creator A5064617154 @default.
• W3147468044 creator A5072622975 @default.
• W3147468044 creator A5072686542 @default.
• W3147468044 date "2021-06-01" @default.
• W3147468044 modified "2023-10-18" @default.
• W3147468044 title "Using stable isotopes to distinguish atmospheric nitrate production and its contribution to the surface ocean across hemispheres" @default.
• W3147468044 cites W1486119704 @default.
• W3147468044 cites W1573296852 @default.
• W3147468044 cites W1620512497 @default.
• W3147468044 cites W1901706366 @default.
• W3147468044 cites W1950181621 @default.
• W3147468044 cites W1964172124 @default.
• W3147468044 cites W1975093864 @default.
• W3147468044 cites W1975296191 @default.
• W3147468044 cites W1978029251 @default.
• W3147468044 cites W1978842620 @default.
• W3147468044 cites W1995163974 @default.
• W3147468044 cites W2007635294 @default.
• W3147468044 cites W2013077733 @default.
• W3147468044 cites W2022460322 @default.
• W3147468044 cites W2024415711 @default.
• W3147468044 cites W2025254507 @default.
• W3147468044 cites W2029350943 @default.
• W3147468044 cites W2032292978 @default.
• W3147468044 cites W2033801490 @default.
• W3147468044 cites W2051718272 @default.
• W3147468044 cites W2061417242 @default.
• W3147468044 cites W2072887130 @default.
• W3147468044 cites W2075033457 @default.
• W3147468044 cites W2084154199 @default.
• W3147468044 cites W2095540598 @default.
• W3147468044 cites W2095796446 @default.
• W3147468044 cites W2101813375 @default.
• W3147468044 cites W2107216028 @default.
• W3147468044 cites W2108004971 @default.
• W3147468044 cites W2113058638 @default.
• W3147468044 cites W2117936097 @default.
• W3147468044 cites W2127721506 @default.
• W3147468044 cites W2128332833 @default.
• W3147468044 cites W2136224973 @default.
• W3147468044 cites W2142180479 @default.
• W3147468044 cites W2147994024 @default.
• W3147468044 cites W2152262923 @default.
• W3147468044 cites W2167407334 @default.
• W3147468044 cites W2168796578 @default.
• W3147468044 cites W2227401735 @default.
• W3147468044 cites W2293435465 @default.
• W3147468044 cites W2314103220 @default.
• W3147468044 cites W2471279947 @default.
• W3147468044 cites W2519497602 @default.
• W3147468044 cites W2529122207 @default.
• W3147468044 cites W2535238237 @default.
• W3147468044 cites W2613810387 @default.
• W3147468044 cites W2615799312 @default.
• W3147468044 cites W2758320583 @default.
• W3147468044 cites W2758663503 @default.
• W3147468044 cites W2795759868 @default.
• W3147468044 cites W2800781541 @default.
• W3147468044 cites W2801696240 @default.
• W3147468044 cites W2895759727 @default.
• W3147468044 cites W2936105243 @default.
• W3147468044 cites W2944704243 @default.
• W3147468044 cites W3023786143 @default.
• W3147468044 cites W3032570819 @default.
• W3147468044 cites W3184258599 @default.
• W3147468044 doi "https://doi.org/10.1016/j.epsl.2021.116914" @default.
• W3147468044 hasPublicationYear "2021" @default.
• W3147468044 type Work @default.
• W3147468044 sameAs 3147468044 @default.
• W3147468044 citedByCount "16" @default.
• W3147468044 countsByYear W31474680442021 @default.
• W3147468044 countsByYear W31474680442022 @default.
• W3147468044 countsByYear W31474680442023 @default.
• W3147468044 crossrefType "journal-article" @default.
• W3147468044 hasAuthorship W3147468044A5004357577 @default.
• W3147468044 hasAuthorship W3147468044A5015415143 @default.
• W3147468044 hasAuthorship W3147468044A5024056919 @default.
• W3147468044 hasAuthorship W3147468044A5025752123 @default.
• W3147468044 hasAuthorship W3147468044A5034308130 @default.
• W3147468044 hasAuthorship W3147468044A5035639413 @default.
• W3147468044 hasAuthorship W3147468044A5049168798 @default.
• W3147468044 hasAuthorship W3147468044A5055734137 @default.
• W3147468044 hasAuthorship W3147468044A5056620408 @default.
• W3147468044 hasAuthorship W3147468044A5064617154 @default.
• W3147468044 hasAuthorship W3147468044A5072622975 @default.
• W3147468044 hasAuthorship W3147468044A5072686542 @default.
• W3147468044 hasConcept C111368507 @default.

• next