Matches in SemOpenAlex for { <https://semopenalex.org/work/W4381951777> ?p ?o ?g. }
- W4381951777 endingPage "165116" @default.
- W4381951777 startingPage "165116" @default.
- W4381951777 abstract "Secondary organic aerosol (SOA) exerts a considerable influence on atmospheric chemistry. However, little information about the vertical distribution of SOA in the alpine setting is available, which limited the simulation of SOA using chemical transport models. Here, a total of 15 biogenic and anthropogenic SOA tracers were measured in PM2.5 aerosols at both the summit (1840 m a.s.l.) and foot (480 m a.s.l.) of Mt. Huang during the winter of 2020 to explore their vertical distribution and formation mechanism. Most of the determined chemical species (e.g., BSOA and ASOA tracers, carbonaceous components, major inorganic ions) and gaseous pollutants at the foot of Mt. Huang were 1.7-3.2 times higher concentrations than those at the summit, suggesting the relatively more significant effect of anthropogenic emissions at the ground level. The ISORROPIA-II model showed that aerosol acidity increases as altitude decreases. Air mass trajectories, potential source contribution function (PSCF), and correlation analysis of BSOA tracers with temperature revealed that SOA at the foot of Mt. Huang was mostly derived from the local oxidation of volatile organic compounds (VOCs), while SOA at the summit was mainly influenced by long-distance transport. The robust correlations of BSOA tracers with anthropogenic pollutants (e.g., NH3, NO2, and SO2) (r = 0.54-0.91, p < 0.05) indicated that anthropogenic emissions could promote BSOA productions in the mountainous background atmosphere. Moreover, most of SOA tracers (r = 0.63-0.96, p < 0.01) and carbonaceous species (r = 0.58-0.81, p < 0.01) were correlated well with levoglucosan in all samples, suggesting that biomass burning played an important role in the mountain troposphere. This work demonstrated that daytime SOA at the summit of Mt. Huang was significantly influenced by the valley breeze in winter. Our results provide new insights into the vertical distributions and provenance of SOA in the free troposphere over East China." @default.
- W4381951777 created "2023-06-26" @default.
- W4381951777 creator A5014262816 @default.
- W4381951777 creator A5036244981 @default.
- W4381951777 creator A5056821526 @default.
- W4381951777 creator A5059039253 @default.
- W4381951777 creator A5071538308 @default.
- W4381951777 creator A5077827495 @default.
- W4381951777 creator A5078536205 @default.
- W4381951777 creator A5082061627 @default.
- W4381951777 creator A5087563479 @default.
- W4381951777 date "2023-10-01" @default.
- W4381951777 modified "2023-09-23" @default.
- W4381951777 title "Contrasting molecular characteristics and formation mechanisms of biogenic and anthropogenic secondary organic aerosols at the summit and foot of Mt. Huang, East China" @default.
- W4381951777 cites W1499375438 @default.
- W4381951777 cites W1614117239 @default.
- W4381951777 cites W1666891192 @default.
- W4381951777 cites W1738160726 @default.
- W4381951777 cites W1966779205 @default.
- W4381951777 cites W1974430896 @default.
- W4381951777 cites W1982969719 @default.
- W4381951777 cites W1988467524 @default.
- W4381951777 cites W1989889548 @default.
- W4381951777 cites W2001851660 @default.
- W4381951777 cites W2002570697 @default.
- W4381951777 cites W2007922946 @default.
- W4381951777 cites W2020427455 @default.
- W4381951777 cites W2026186615 @default.
- W4381951777 cites W2066887109 @default.
- W4381951777 cites W2068577259 @default.
- W4381951777 cites W2090646981 @default.
- W4381951777 cites W2122054302 @default.
- W4381951777 cites W2126430862 @default.
- W4381951777 cites W2132381103 @default.
- W4381951777 cites W2133789872 @default.
- W4381951777 cites W2143510929 @default.
- W4381951777 cites W2144923407 @default.
- W4381951777 cites W2156122616 @default.
- W4381951777 cites W2171877122 @default.
- W4381951777 cites W2204253375 @default.
- W4381951777 cites W2327670757 @default.
- W4381951777 cites W2332804823 @default.
- W4381951777 cites W2397673276 @default.
- W4381951777 cites W2470089823 @default.
- W4381951777 cites W2512936980 @default.
- W4381951777 cites W2581178033 @default.
- W4381951777 cites W2626365493 @default.
- W4381951777 cites W2714243732 @default.
- W4381951777 cites W2755088366 @default.
- W4381951777 cites W2769849368 @default.
- W4381951777 cites W2778905951 @default.
- W4381951777 cites W2781802033 @default.
- W4381951777 cites W2793110666 @default.
- W4381951777 cites W2798172230 @default.
- W4381951777 cites W2899306247 @default.
- W4381951777 cites W2930847631 @default.
- W4381951777 cites W2939064738 @default.
- W4381951777 cites W2942154925 @default.
- W4381951777 cites W2947769261 @default.
- W4381951777 cites W2954657411 @default.
- W4381951777 cites W2955601895 @default.
- W4381951777 cites W2956421733 @default.
- W4381951777 cites W2967890588 @default.
- W4381951777 cites W2984415803 @default.
- W4381951777 cites W2989701166 @default.
- W4381951777 cites W3012067595 @default.
- W4381951777 cites W3024350206 @default.
- W4381951777 cites W3048060975 @default.
- W4381951777 cites W3094932809 @default.
- W4381951777 cites W3107492361 @default.
- W4381951777 cites W3114987306 @default.
- W4381951777 cites W3120190105 @default.
- W4381951777 cites W3130230994 @default.
- W4381951777 cites W3134745554 @default.
- W4381951777 cites W3165820327 @default.
- W4381951777 cites W3170287835 @default.
- W4381951777 cites W4205693356 @default.
- W4381951777 cites W4221033377 @default.
- W4381951777 cites W4282976413 @default.
- W4381951777 cites W4294362076 @default.
- W4381951777 cites W4306293877 @default.
- W4381951777 cites W4308032005 @default.
- W4381951777 cites W4308344704 @default.
- W4381951777 doi "https://doi.org/10.1016/j.scitotenv.2023.165116" @default.
- W4381951777 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/37364833" @default.
- W4381951777 hasPublicationYear "2023" @default.
- W4381951777 type Work @default.
- W4381951777 citedByCount "0" @default.
- W4381951777 crossrefType "journal-article" @default.
- W4381951777 hasAuthorship W4381951777A5014262816 @default.
- W4381951777 hasAuthorship W4381951777A5036244981 @default.
- W4381951777 hasAuthorship W4381951777A5056821526 @default.
- W4381951777 hasAuthorship W4381951777A5059039253 @default.
- W4381951777 hasAuthorship W4381951777A5071538308 @default.
- W4381951777 hasAuthorship W4381951777A5077827495 @default.
- W4381951777 hasAuthorship W4381951777A5078536205 @default.
- W4381951777 hasAuthorship W4381951777A5082061627 @default.
- W4381951777 hasAuthorship W4381951777A5087563479 @default.