Matches in SemOpenAlex for { <https://semopenalex.org/work/W4385319274> ?p ?o ?g. }
- W4385319274 endingPage "8402" @default.
- W4385319274 startingPage "8383" @default.
- W4385319274 abstract "Abstract. Secondary organic aerosols (SOAs) play a key role in climate change and public health. However, the oxidation state and volatility of SOAs are still not well understood. Here, we investigated the highly oxygenated organic molecules (HOMs) in SOAs formed from ozonolysis of β-pinene and limonene. Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) was used to characterize HOMs in aerosol filter samples, and a scanning mobility particle sizer (SMPS) was used to measure the concentration and size distribution of SOA particles. The relative abundance of HOMs (i.e., ratio of summed mass spectrometry peak intensity of HOMs to totally identified organic compounds) in limonene SOA was 14 %–20 %, higher than in β-pinene SOA (3 %–13 %), exhibiting different trends with increasing ozone concentrations. β-pinene oxidation-derived HOMs exhibit higher yield at high ozone concentration, accompanied by substantial formation of ultra-low-volatile organic compounds (ULVOCs). Limonene oxidation-derived HOMs exhibit higher yield at moderate ozone concentrations, with semi-, low-, and extremely low-volatile organic compounds (SVOCs, LOVCs, and ELVOCs) play a major role. Combined experimental evidence and theoretical analysis indicate that oxygen-increasing-based peroxy radical chemistry is a plausible mechanism for the formation of oxygenated organic compounds with 10 carbon atoms. Our findings show that HOMs and low-volatile species in β-pinene and limonene SOA are largely different. The ozone concentration-driven SOA formation and evolution mechanism for monoterpenes is suggested to be considered in future climate or exposure risk models, which may enable more accurate air quality prediction and management." @default.
- W4385319274 created "2023-07-28" @default.
- W4385319274 creator A5006349365 @default.
- W4385319274 creator A5019376425 @default.
- W4385319274 creator A5023874610 @default.
- W4385319274 creator A5024087192 @default.
- W4385319274 creator A5026229938 @default.
- W4385319274 creator A5028783832 @default.
- W4385319274 creator A5039837606 @default.
- W4385319274 creator A5047393236 @default.
- W4385319274 creator A5052620727 @default.
- W4385319274 creator A5057640513 @default.
- W4385319274 creator A5064055729 @default.
- W4385319274 creator A5078024000 @default.
- W4385319274 creator A5085722015 @default.
- W4385319274 date "2023-07-26" @default.
- W4385319274 modified "2023-10-12" @default.
- W4385319274 title "Large differences of highly oxygenated organic molecules (HOMs) and low-volatile species in secondary organic aerosols (SOAs) formed from ozonolysis of <i>β</i>-pinene and limonene" @default.
- W4385319274 cites W1504241111 @default.
- W4385319274 cites W1902682689 @default.
- W4385319274 cites W1973477740 @default.
- W4385319274 cites W1983936554 @default.
- W4385319274 cites W1997272876 @default.
- W4385319274 cites W2004687112 @default.
- W4385319274 cites W2007240210 @default.
- W4385319274 cites W2011953192 @default.
- W4385319274 cites W2015133270 @default.
- W4385319274 cites W2023037439 @default.
- W4385319274 cites W2028892886 @default.
- W4385319274 cites W2039437298 @default.
- W4385319274 cites W2044724516 @default.
- W4385319274 cites W2045617521 @default.
- W4385319274 cites W2049288655 @default.
- W4385319274 cites W2049411469 @default.
- W4385319274 cites W2050154334 @default.
- W4385319274 cites W2057887602 @default.
- W4385319274 cites W2059256691 @default.
- W4385319274 cites W2073812074 @default.
- W4385319274 cites W2077425974 @default.
- W4385319274 cites W2085840444 @default.
- W4385319274 cites W2089431002 @default.
- W4385319274 cites W2102042448 @default.
- W4385319274 cites W2107569910 @default.
- W4385319274 cites W2109419617 @default.
- W4385319274 cites W2110235526 @default.
- W4385319274 cites W2116507044 @default.
- W4385319274 cites W2119744638 @default.
- W4385319274 cites W2120270786 @default.
- W4385319274 cites W2121586490 @default.
- W4385319274 cites W2127281457 @default.
- W4385319274 cites W2127510753 @default.
- W4385319274 cites W2130975189 @default.
- W4385319274 cites W2141507669 @default.
- W4385319274 cites W2141693044 @default.
- W4385319274 cites W2156633761 @default.
- W4385319274 cites W2158540706 @default.
- W4385319274 cites W2158598318 @default.
- W4385319274 cites W2165121527 @default.
- W4385319274 cites W2167302998 @default.
- W4385319274 cites W2170758644 @default.
- W4385319274 cites W2271813080 @default.
- W4385319274 cites W2320712911 @default.
- W4385319274 cites W2327561941 @default.
- W4385319274 cites W2402503711 @default.
- W4385319274 cites W2402991992 @default.
- W4385319274 cites W2466617439 @default.
- W4385319274 cites W2498665214 @default.
- W4385319274 cites W2528574402 @default.
- W4385319274 cites W2530753443 @default.
- W4385319274 cites W2532716002 @default.
- W4385319274 cites W2558735553 @default.
- W4385319274 cites W2559481487 @default.
- W4385319274 cites W2564343832 @default.
- W4385319274 cites W2592219204 @default.
- W4385319274 cites W2607350314 @default.
- W4385319274 cites W2608193111 @default.
- W4385319274 cites W2614250595 @default.
- W4385319274 cites W2746422685 @default.
- W4385319274 cites W2786696364 @default.
- W4385319274 cites W2794087825 @default.
- W4385319274 cites W2883444401 @default.
- W4385319274 cites W2886321309 @default.
- W4385319274 cites W2890277796 @default.
- W4385319274 cites W2890397218 @default.
- W4385319274 cites W2891423847 @default.
- W4385319274 cites W2893612070 @default.
- W4385319274 cites W2896785715 @default.
- W4385319274 cites W2897729160 @default.
- W4385319274 cites W2897936584 @default.
- W4385319274 cites W2917630884 @default.
- W4385319274 cites W2922556553 @default.
- W4385319274 cites W2954308819 @default.
- W4385319274 cites W2955601895 @default.
- W4385319274 cites W2956582015 @default.
- W4385319274 cites W2969528346 @default.
- W4385319274 cites W2974232801 @default.
- W4385319274 cites W2975724601 @default.
- W4385319274 cites W2995210816 @default.