1994
DOI: 10.2307/3431940
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Atmospheric Chemistry of Gas-Phase Polycyclic Aromatic Hydrocarbons: Formation of Atmospheric Mutagens

Abstract: The atmospheric chemistry of the 2-to 4-ring polycyclic aromatic hydrocarbons (PAH), which exist mainly in the gas phase in the atmosphere, is discussed. The dominant loss process for the gas-phase PAH is by reaction with the hydroxyl radical, resulting in calculated lifetimes in the atmosphere of generally less than one day. The hydroxyl (OH) radical-initiated reactions and nitrate (NO3) radical-initiated reactions often lead to the formation of mutagenic nitro-PAH and other nitropolycyclic aromatic compounds… Show more

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Cited by 129 publications
(164 citation statements)
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“…The main ions and relative abundances of both the products obtained with GC/MS in EI modes show good consistency with the experimental results of Herrmann et al 12 Since the benzene ring is the active sites of the nitro substitution reaction, 19,27 we speculate that the pyrimidine ring is more active than the functional groups in the Figure 3A shows the TOF mass spectrum of PM (C 11 H 18 N 4 O 2 , MW = 238 g mol −1 ) particles before exposure to NO 3 radicals. The mass peaks at m/z 238, 193, and 166 correspond to the molecular ion and two fragment ions of PM, respectively.…”
Section: Resultssupporting
confidence: 84%
“…The main ions and relative abundances of both the products obtained with GC/MS in EI modes show good consistency with the experimental results of Herrmann et al 12 Since the benzene ring is the active sites of the nitro substitution reaction, 19,27 we speculate that the pyrimidine ring is more active than the functional groups in the Figure 3A shows the TOF mass spectrum of PM (C 11 H 18 N 4 O 2 , MW = 238 g mol −1 ) particles before exposure to NO 3 radicals. The mass peaks at m/z 238, 193, and 166 correspond to the molecular ion and two fragment ions of PM, respectively.…”
Section: Resultssupporting
confidence: 84%
“…The calculated, nighttime, atmospheric lifetimes of eugenol and 4-ethylguaiacol toward NO 3 radicals were ∼3.5 and 0.5 h, respectively, under a typical tropospheric concentration of 5 × 10 8 molecules cm −3 of the NO 3 radical. 58 Therefore, these two kinds of methoxyphenols had high reactivities with NO 3 during the night, revealing an important sink for these types of compounds and indicating that they are not suitable tracers like some other methoxyphenols. 22 Because of their high reactivities, the fraction of these organic compounds in the atmosphere changes over time, and this factor should be considered in source apportionment and air-pollution model studies.…”
Section: Discussionmentioning
confidence: 99%
“…This was accomplished by developing a sensitive and specific LC-MS/ MS method and an effective pretreatment method for the simultaneous measurement of urinary 1-NP metabolites, intended to be biomarkers of low-level 1-NP exposure in humans. As described above, 1-NP is of interest because it is one of the distinctive components in DEP, is not formed by photochemical reactions in the atmosphere (40), and is primarily adsorbed to the particulate phase. These findings suggest that urinary 1-NP metabolites may be used as a representative biomarker for assessing exposure to diesel exhaust.…”
Section: Discussionmentioning
confidence: 99%