FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3169713938> ?p ?o ?g. }

• W3169713938 abstract "Abstract. Speciated atmospheric mercury observations collected over the period from 2008 to 2010 at the Environmental Protection Agency and National Atmospheric Deposition Program Atmospheric Mercury Network sites (AMNet) were analyzed for its spatial, seasonal, and diurnal characteristics across the US Median values of gaseous elemental mercury (GEM), gaseous oxidized mercury (GOM) and particulate bound mercury (PBM) at 11 different AMNet sites ranged from 148–226 ppqv (1.32–2.02 ng m−3), 0.05–1.4 ppqv (0.47–12.4 pg m−3) and 0.18–1.5 ppqv (1.61–13.7 pg m−3), respectively. Common characteristics of these sites were the similar median levels of GEM as well as its seasonality, with the highest mixing ratios occurring in winter and spring and the lowest in fall. However, discernible differences in monthly average GEM were as large as 30 ppqv, which may be caused by sporadic influence from local emission sources. The largest diurnal variation amplitude of GEM occurred in the summer. Seven rural sites displayed similar GEM summer diurnal patterns, in that the lowest levels appeared in the early morning, and then the GEM mixing ratio increased after sunrise and reached its maxima at noon or in the early afternoon. However, sites in Utah (UT96, UT97) and New York (NY95) showed a distinctly different pattern, with the lowest mixing ratios appearing in the afternoon and the highest mixing ratios at night. Unlike GEM, GOM exhibited higher mixing ratios in spring and summer. The largest diurnal variation amplitude of GOM occurred in spring for most AMNet sites. GOM diurnal minima appeared before sunrise and maxima appeared in the afternoon, and the variation in magnitude for all seasons at most monitoring sites fell in the range of 0 to 2 ppqv, except the Utah sites (up to 5 ppqv). The increased GOM mixing ratio in the afternoon indicated a photochemically driven oxidation of GEM resulting in GOM formation. PBM exhibited diurnal fluctuations in summertime instead of wintertime, although the PBM mixing ratio in summer was not as high as in winter. The summertime PBM diurnal pattern displayed a daily maximum in the early afternoon and lower mixing ratios at night, implying photochemical production of PBM in summer. The marine sea salt aerosol uptake of GEM and GOM was not apparent in the PBM data collected at coastal sites, with PBM being higher at inland sites." @default.
• W3169713938 created "2021-06-22" @default.
• W3169713938 creator A5068339434 @default.
• W3169713938 creator A5090638918 @default.
• W3169713938 date "2012-04-26" @default.
• W3169713938 modified "2023-09-23" @default.
• W3169713938 title "Seasonal and diurnal variations of atmospheric mercury across the US determined from AMNet monitoring data" @default.
• W3169713938 cites W132594222 @default.
• W3169713938 cites W1492346868 @default.
• W3169713938 cites W1616357741 @default.
• W3169713938 cites W1964077300 @default.
• W3169713938 cites W1968733385 @default.
• W3169713938 cites W1969440390 @default.
• W3169713938 cites W1975147171 @default.
• W3169713938 cites W1981366469 @default.
• W3169713938 cites W1982192639 @default.
• W3169713938 cites W1988729840 @default.
• W3169713938 cites W1989300302 @default.
• W3169713938 cites W1994321957 @default.
• W3169713938 cites W199889995 @default.
• W3169713938 cites W2002861022 @default.
• W3169713938 cites W2006371079 @default.
• W3169713938 cites W2010149500 @default.
• W3169713938 cites W2011241549 @default.
• W3169713938 cites W2014261257 @default.
• W3169713938 cites W2026985376 @default.
• W3169713938 cites W2033502042 @default.
• W3169713938 cites W2036452987 @default.
• W3169713938 cites W2037944726 @default.
• W3169713938 cites W2044929344 @default.
• W3169713938 cites W2045530099 @default.
• W3169713938 cites W2051108273 @default.
• W3169713938 cites W2060468368 @default.
• W3169713938 cites W2061828799 @default.
• W3169713938 cites W2067557605 @default.
• W3169713938 cites W2068012376 @default.
• W3169713938 cites W2071630238 @default.
• W3169713938 cites W2077116437 @default.
• W3169713938 cites W2078707188 @default.
• W3169713938 cites W2091083575 @default.
• W3169713938 cites W2095117336 @default.
• W3169713938 cites W2095753719 @default.
• W3169713938 cites W2110208764 @default.
• W3169713938 cites W2117302987 @default.
• W3169713938 cites W2125301092 @default.
• W3169713938 cites W2127466807 @default.
• W3169713938 cites W2141307366 @default.
• W3169713938 cites W2148463939 @default.
• W3169713938 cites W2149236361 @default.
• W3169713938 cites W2151691558 @default.
• W3169713938 cites W2155019272 @default.
• W3169713938 cites W2163421314 @default.
• W3169713938 cites W2168139722 @default.
• W3169713938 cites W2315680816 @default.
• W3169713938 cites W4247447529 @default.
• W3169713938 cites W4251167380 @default.
• W3169713938 doi "https://doi.org/10.5194/acpd-12-10845-2012" @default.
• W3169713938 hasPublicationYear "2012" @default.
• W3169713938 type Work @default.
• W3169713938 sameAs 3169713938 @default.
• W3169713938 citedByCount "0" @default.
• W3169713938 crossrefType "posted-content" @default.
• W3169713938 hasAuthorship W3169713938A5068339434 @default.
• W3169713938 hasAuthorship W3169713938A5090638918 @default.
• W3169713938 hasBestOaLocation W31697139381 @default.
• W3169713938 hasConcept C121332964 @default.
• W3169713938 hasConcept C125403950 @default.
• W3169713938 hasConcept C127313418 @default.
• W3169713938 hasConcept C1276947 @default.
• W3169713938 hasConcept C167678106 @default.
• W3169713938 hasConcept C178790620 @default.
• W3169713938 hasConcept C18459110 @default.
• W3169713938 hasConcept C185592680 @default.
• W3169713938 hasConcept C18903297 @default.
• W3169713938 hasConcept C19720800 @default.
• W3169713938 hasConcept C199360897 @default.
• W3169713938 hasConcept C24245907 @default.
• W3169713938 hasConcept C2777777548 @default.
• W3169713938 hasConcept C38262639 @default.
• W3169713938 hasConcept C39432304 @default.
• W3169713938 hasConcept C41008148 @default.
• W3169713938 hasConcept C49204034 @default.
• W3169713938 hasConcept C58650310 @default.
• W3169713938 hasConcept C86803240 @default.
• W3169713938 hasConcept C91586092 @default.
• W3169713938 hasConceptScore W3169713938C121332964 @default.
• W3169713938 hasConceptScore W3169713938C125403950 @default.
• W3169713938 hasConceptScore W3169713938C127313418 @default.
• W3169713938 hasConceptScore W3169713938C1276947 @default.
• W3169713938 hasConceptScore W3169713938C167678106 @default.
• W3169713938 hasConceptScore W3169713938C178790620 @default.
• W3169713938 hasConceptScore W3169713938C18459110 @default.
• W3169713938 hasConceptScore W3169713938C185592680 @default.
• W3169713938 hasConceptScore W3169713938C18903297 @default.
• W3169713938 hasConceptScore W3169713938C19720800 @default.
• W3169713938 hasConceptScore W3169713938C199360897 @default.
• W3169713938 hasConceptScore W3169713938C24245907 @default.
• W3169713938 hasConceptScore W3169713938C2777777548 @default.
• W3169713938 hasConceptScore W3169713938C38262639 @default.
• W3169713938 hasConceptScore W3169713938C39432304 @default.

• next