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Peroxyacetyl nitrate
Chemical compound From Wikipedia, the free encyclopedia
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Peroxyacetyl nitrate is a peroxyacyl nitrate.[1] It is a secondary pollutant present in photochemical smog and PAN concentrations can be sensitive to precursor emissions.[2][1] It is thermally unstable and decomposes into peroxyethanoyl radicals and nitrogen dioxide gas. It is a lachrymatory substance, meaning that it irritates the lungs and eyes.[3]
It has been suggested that this article be merged with Peroxyacyl nitrates. (Discuss) Proposed since November 2025. |
Peroxyacetyl nitrate, or PAN, is an oxidant that is more stable than ozone.[1] Hence, it is more capable of long-range transport than ozone.[1] It serves as a carrier for oxides of nitrogen (NOx) into rural regions and causes ozone formation in the global troposphere.[1]
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Atmospheric chemistry
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Perspective
PAN is produced in the atmosphere via photochemical oxidation of hydrocarbons (e.g. Alkenes, Aromatics, and isoprenes).[4][3] Carbonyls (oxidized VOCs) create acyl radicals which then become peroxyacetic acid (PA) radicals.[4] Acetaldehyde is the dominant carbonyl species to produce PA radicals followed by Methylglyoxal, combined they can account for up to 80% of PA radical formation.[1][4] The PA radicals can reversibly react with nitrogen dioxide (NO2) to form PAN.[1] Night-time reaction of acetaldehyde with nitrogen trioxide is another possible source.[4] Since there are no direct PAN emissions, it is a secondary pollutant.[1] Next to ozone and hydrogen peroxide (H2O2), it is an important component of photochemical smog.[1]
Other peroxyacyl nitrates in the atmosphere are peroxypropionyl nitrate (PPN), peroxybutyryl nitrate (PBN), and peroxybenzoyl nitrate (PBzN). Chlorinated forms have also been observed.[1] PAN is the most important peroxyacyl nitrate. PAN and its homologues reach about 5 to 20 percent of the concentration of ozone in urban areas.[1] At lower temperatures, these peroxy-nitrates are stable and can be transported over long distances,[1] providing nitrogen oxides to otherwise unpolluted areas. At higher temperatures, they decompose into NO2 and the peroxyacyl radica[1] l.
The decay of PAN in the atmosphere is mainly thermal.[1] Thus, the long-range transport occurs through cold regions of the atmosphere, whereas the decomposition takes place at warmer levels.[1] PAN can also be photolyzed by UV radiation.[1] It is a reservoir gas that serves both as a source and a sink of ROx- and NOx radicals.[1] Nitrogen oxides from PAN decomposition enhance ozone production in the lower troposphere.[1]
The natural concentration of PAN in the atmosphere is below 0.1 μg/m3.[1] Measurements in German cities showed values up to 25 μg/m3.[1] Peak values above 200 μg/m3 have been measured in Los Angeles in the second half of the 20th century (1 ppb of PAN corresponds to 4.37 μg/m3).[1] Due to the complexity of the measurement setup, only sporadic measurements are available.[2][5] The satellite based Cross-Track Infrared sounder (CrIS) instrument is able to provide mid-tropospheric PAN measurements on a global scale.[5][2]
PAN is a greenhouse gas.
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Sensitivity
PAN has a sensitivity to precursor emissions, mainly from VOCs and NOx.[1][2][4] PANs sensitivity towards VOCs is greater than that of NOx.[4] VOC reductions have more of an effect on PA radicals than on NOx.[4] Notably, global emissions of precursor during Covid-19 demonstrated that PAN concentrations do not always decrease with a decrease in NOx concentrations.[2][6] Similarly, PAN responds non-linearly to precursor changes.[1][2] Alkenes and oxidized VOCs strongly influence the formation of PA radicals.[4] Meteorological effects also influence the availability of these radicals and hence PAN formation.[6]
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Synthesis
PAN can be produced in a lipophilic solvent from peroxyacetic acid.[7][8] For the synthesis, concentrated sulfuric acid is added to degassed n-tridecane and peroxyacetic acid in an ice bath. Next, concentrated nitric acid is added.[8][9]
As an alternative, PAN can also be synthesized in the gas phase via photolysis of acetone and NO2 with a mercury lamp. Methyl nitrate (CH3ONO2) is created as a by-product.[9]
Atmospheric effects
Seasonal cycles of PAN have been observed.[1] Meteorological effects such as temperatures, wind patterns, and the availability of radicals influence PANs stability as well as transportation in the atmosphere.[1][6] During the springtime in the northern hemisphere, high concentrations are attributed to an increase in photochemical activity.[6] In addition, concentrations of PAN increase due to it having a relatively large lifetime against thermal decomposition.[1] Transportation of PAN can also occur by wildfire smoke moving it into an otherwise unpolluted region.[2] In the northern hemisphere winter however, PAN levels become limited when there is reduced hydrocarbons, NO2, and low solar radiation.[1]
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Toxicity
The toxicity of PAN is similar to that of NO2 but higher than sulfur dioxide (SO2).[3] Populations with pulmonary disease tend to be more sensitive to the toxic effects of PAN.[3] Eye irritation from photochemical smog can be caused by an increase in PAN levels.[3] Concentrations at or above 0.64 mg/m3 increase the likelihood of eye irritation.[3] PAN is a very weak mutagen.[3]
References
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