Matches in SemOpenAlex for { <https://semopenalex.org/work/W2138302511> ?p ?o ?g. }
- W2138302511 endingPage "512" @default.
- W2138302511 startingPage "501" @default.
- W2138302511 abstract "Abstract. Dissolved nitrous oxide (N2O) concentrations are usually determined by gas chromatography (GC). Here we present laboratory tests and initial field measurements using a novel setup comprising a commercially available laser-based analyser for N2O, carbon monoxide and water vapour coupled to a glass-bed equilibrator. This approach is less labour-intensive and provides higher temporal and spatial resolution than the conventional GC technique. The standard deviation of continuous equilibrator or atmospheric air measurements was 0.2 nmol mol−1 (averaged over 5 min). The short-term repeatability for reference gas measurements within 1 h of each other was 0.2 nmol mol−1 or better. Another indicator of the long-term stability of the analyser is the standard deviation of the calibrated N2O mole fraction in marine air, which was between 0.5 and 0.7 nmol mol−1. The equilibrator measurements were compared with purge-and-trap gas chromatography–mass spectrometry (GC-MS) analyses of N2O concentrations in discrete samples from the Southern Ocean and showed agreement to within the 2% measurement uncertainty of the GC-MS method. The equilibrator response time to concentration changes in water was from 142 to 203 s, depending on the headspace flow rate. The system was tested at sea during a north-to-south transect of the Atlantic Ocean. While the subtropical gyres were slightly undersaturated, the equatorial region was a source of nitrous oxide to the atmosphere, confirming previous findings (Forster et al., 2009). The ability to measure at high temporal and spatial resolution revealed submesoscale variability in dissolved N2O concentrations. Mean sea-to-air fluxes in the tropical and subtropical Atlantic ranged between −1.6 and 0.11 μmol m−2 d−1 and confirm that the subtropical Atlantic is not an important source region for N2O to the atmosphere, compared to global average fluxes of 0.6–2.4 μmol m−2 d−1. The system can be easily modified for autonomous operation on voluntary observing ships (VOS). Future work should include an interlaboratory comparison exercise with other methods of dissolved N2O analyses." @default.
- W2138302511 created "2016-06-24" @default.
- W2138302511 creator A5048003327 @default.
- W2138302511 creator A5069738292 @default.
- W2138302511 date "2014-06-19" @default.
- W2138302511 modified "2023-10-17" @default.
- W2138302511 title "Equilibrator-based measurements of dissolved nitrous oxide in the surface ocean using an integrated cavity output laser absorption spectrometer" @default.
- W2138302511 cites W1513196349 @default.
- W2138302511 cites W1543246845 @default.
- W2138302511 cites W1658815594 @default.
- W2138302511 cites W1678157725 @default.
- W2138302511 cites W1775216094 @default.
- W2138302511 cites W1903052351 @default.
- W2138302511 cites W1971991115 @default.
- W2138302511 cites W1981574408 @default.
- W2138302511 cites W1986539646 @default.
- W2138302511 cites W2001213182 @default.
- W2138302511 cites W2003653419 @default.
- W2138302511 cites W2007352478 @default.
- W2138302511 cites W2011820761 @default.
- W2138302511 cites W2012118586 @default.
- W2138302511 cites W2014820681 @default.
- W2138302511 cites W2025343504 @default.
- W2138302511 cites W2026511451 @default.
- W2138302511 cites W2041913176 @default.
- W2138302511 cites W2047855988 @default.
- W2138302511 cites W2048202376 @default.
- W2138302511 cites W2055910928 @default.
- W2138302511 cites W2058775767 @default.
- W2138302511 cites W2058995292 @default.
- W2138302511 cites W2066831210 @default.
- W2138302511 cites W2067841165 @default.
- W2138302511 cites W2068473749 @default.
- W2138302511 cites W2081569456 @default.
- W2138302511 cites W2083524788 @default.
- W2138302511 cites W2094300388 @default.
- W2138302511 cites W2094841197 @default.
- W2138302511 cites W2102680356 @default.
- W2138302511 cites W2115212093 @default.
- W2138302511 cites W2127658270 @default.
- W2138302511 cites W2133813560 @default.
- W2138302511 cites W2139127544 @default.
- W2138302511 cites W2141553100 @default.
- W2138302511 cites W2142308015 @default.
- W2138302511 cites W2149932227 @default.
- W2138302511 cites W2154610441 @default.
- W2138302511 cites W2335163798 @default.
- W2138302511 cites W4229735386 @default.
- W2138302511 cites W4242531998 @default.
- W2138302511 cites W4251551940 @default.
- W2138302511 doi "https://doi.org/10.5194/os-10-501-2014" @default.
- W2138302511 hasPublicationYear "2014" @default.
- W2138302511 type Work @default.
- W2138302511 sameAs 2138302511 @default.
- W2138302511 citedByCount "18" @default.
- W2138302511 countsByYear W21383025112015 @default.
- W2138302511 countsByYear W21383025112016 @default.
- W2138302511 countsByYear W21383025112017 @default.
- W2138302511 countsByYear W21383025112018 @default.
- W2138302511 countsByYear W21383025112019 @default.
- W2138302511 countsByYear W21383025112020 @default.
- W2138302511 countsByYear W21383025112021 @default.
- W2138302511 crossrefType "journal-article" @default.
- W2138302511 hasAuthorship W2138302511A5048003327 @default.
- W2138302511 hasAuthorship W2138302511A5069738292 @default.
- W2138302511 hasBestOaLocation W21383025111 @default.
- W2138302511 hasConcept C107872376 @default.
- W2138302511 hasConcept C113196181 @default.
- W2138302511 hasConcept C121332964 @default.
- W2138302511 hasConcept C123460561 @default.
- W2138302511 hasConcept C127313418 @default.
- W2138302511 hasConcept C14168384 @default.
- W2138302511 hasConcept C153294291 @default.
- W2138302511 hasConcept C154020017 @default.
- W2138302511 hasConcept C178790620 @default.
- W2138302511 hasConcept C185592680 @default.
- W2138302511 hasConcept C26834552 @default.
- W2138302511 hasConcept C2777573673 @default.
- W2138302511 hasConcept C30380174 @default.
- W2138302511 hasConcept C39432304 @default.
- W2138302511 hasConcept C43617362 @default.
- W2138302511 hasConcept C505870484 @default.
- W2138302511 hasConcept C65440619 @default.
- W2138302511 hasConcept C86803240 @default.
- W2138302511 hasConcept C91586092 @default.
- W2138302511 hasConceptScore W2138302511C107872376 @default.
- W2138302511 hasConceptScore W2138302511C113196181 @default.
- W2138302511 hasConceptScore W2138302511C121332964 @default.
- W2138302511 hasConceptScore W2138302511C123460561 @default.
- W2138302511 hasConceptScore W2138302511C127313418 @default.
- W2138302511 hasConceptScore W2138302511C14168384 @default.
- W2138302511 hasConceptScore W2138302511C153294291 @default.
- W2138302511 hasConceptScore W2138302511C154020017 @default.
- W2138302511 hasConceptScore W2138302511C178790620 @default.
- W2138302511 hasConceptScore W2138302511C185592680 @default.
- W2138302511 hasConceptScore W2138302511C26834552 @default.
- W2138302511 hasConceptScore W2138302511C2777573673 @default.
- W2138302511 hasConceptScore W2138302511C30380174 @default.