1998
DOI: 10.1016/s1010-6030(97)00290-6
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Photochemistry of acenaphthene at a silica gel/air interface

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Cited by 33 publications
(32 citation statements)
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“…Thereinto, amorphous silica (AS) in soils is assumed to play a major role in Si availability and cycling because it is more soluble than crystalline minerals . A significant portion of total particulate matters in the atmosphere is originally from soils, and thus AS is always found in the constituents of aerosol particulates . It was reported that Si–O • or Si • radicals on AS surfaces could form after light irradiation due to the disordered structure of AS, which could react with adsorbed H 2 O 2 , H 2 O, and O 2 to yield reactive oxygen species (ROS) such as • OH, O 2 •– , etc .…”
Section: Introductionmentioning
confidence: 99%
“…Thereinto, amorphous silica (AS) in soils is assumed to play a major role in Si availability and cycling because it is more soluble than crystalline minerals . A significant portion of total particulate matters in the atmosphere is originally from soils, and thus AS is always found in the constituents of aerosol particulates . It was reported that Si–O • or Si • radicals on AS surfaces could form after light irradiation due to the disordered structure of AS, which could react with adsorbed H 2 O 2 , H 2 O, and O 2 to yield reactive oxygen species (ROS) such as • OH, O 2 •– , etc .…”
Section: Introductionmentioning
confidence: 99%
“…8, as the particulate matter before, during and after the fog has very large OPAC/PAH ratios. The gas phase has a significantly lower OPAC content, indicating that the oxidation of acenaphthene is either facilitated by the air-particulate interface 64 or that the (gas-phase) oxidation products associate predominantly with particles. Both effects are likely to happen simultaneously as the surface-enhanced oxidation of acenaphthene has been described before 64 and the vapor pressure of the monitored oxidation products 65,66 (acenaphthenequinone, 1-acenaphthenone, 1-acenaphthenol and 1,8-naphthalic acid anhydride) is at least two orders of magnitude lower than that of acenaphthene.…”
Section: Resultsmentioning
confidence: 99%
“…The gas phase has a significantly lower OPAC content, indicating that the oxidation of acenaphthene is either facilitated by the air-particulate interface 64 or that the (gas-phase) oxidation products associate predominantly with particles. Both effects are likely to happen simultaneously as the surface-enhanced oxidation of acenaphthene has been described before 64 and the vapor pressure of the monitored oxidation products 65,66 (acenaphthenequinone, 1-acenaphthenone, 1-acenaphthenol and 1,8-naphthalic acid anhydride) is at least two orders of magnitude lower than that of acenaphthene. The presence of fog water does not enhance the degradation of acenaphthene significantly, as its degradation rate is already high; however, the dissolution of the oxidation products of acenaphthene from the PM 2.5 to the fog water can be clearly seen in Fig.…”
Section: Resultsmentioning
confidence: 99%
“…In other laboratory experiments [26][27][28], it was reported that 1,8-NA could be formed by the oxidation of several PAHs, such as acenaphthylene, acenaphthene and even those with more than three rings like benz [a]anthracene. In addition, Kamens et al [14] conducted outdoor chamber experiments where diluted wood smoke was exposed to midday natural sunlight and found that particle-associated 1,8-NA increased in concentrations with time in the presence of the sunlight (and low photochemical O 3 accumulation, i.e.…”
Section: Size Distribution Of Pahs In Urban Atmospheric Particlesmentioning
confidence: 99%