Open AccessMeasurements of PAN, PPN, and MPAN made during the 1994 and 1995 Nashville Intensives of the Southern Oxidant Study: Implications for regional ozone production from biogenic hydrocarbons
Author(s) -
Roberts James M.,
Williams Jonathan,
Baumann Karsten,
Buhr Martin P.,
Goldan Paul D.,
Holloway John,
Hübler Gerhard,
Kuster William C.,
McKeen Stuart A.,
Ryerson Thomas B.,
Trainer Michael,
Williams Eric J.,
Fehsenfeld Fredrick C.,
Bertman Steven B.,
Nouaime George,
Seaver Craig,
Grodzinsky Gil,
Rodgers Michael,
Young Valerie L.
Publication year - 1998
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/98jd01637
Subject(s) - isoprene , ozone , environmental chemistry , chemistry , nox , environmental science , organic chemistry , copolymer , combustion , polymer
Isoprene and a variety of other reactive hydrocarbons are released in large quantities by vegetation in forested regions and are thought to participate in the NO x ‐catalyzed production of ozone, a serious air quality problem in North America and Europe [ National Research Council , 1991]. The determination of the fraction of O 3 formed from anthropogenic NO x and biogenic hydrocarbons (BHC) is a crucial step in the formulation of effective control strategies. Peroxymethacrylic nitric anhydride (MPAN, CH 2 C(CH 3 )C(O)OONO 2 ) is formed almost entirely from the atmospheric oxidation of isoprene in the presence of NO x and is an excellent indicator of recent ozone production from isoprene and therefore biogenic hydrocarbons. Measurements are presented here of MPAN, peroxyacetic nitric anhydride (PAN, CH 3 C(O)OONO 2 ), peroxypropionic nitric anhydride (PPN, CH 3 CH 2 C(O)OONO 2 ) and ozone from separate data sets acquired during the 1994 and 1995 Nashville intensive studies of the Southern Oxidant Study. It was found that PAN, a general product of HC‐NO x photochemistry, could be well represented as a simple linear combination of contributions from BHC and anthropogenic hydrocarbon (AHC) chemistries as indicated by MPAN and PPN, respectively. The PAN:MPAN ratios found to be characteristic of BHC‐dominated chemistry ranged from 6 to 10. The PAN:PPN ratios found to be characteristic of AHC‐dominated chemistry ranged from 5.8 to 7.4. These BHC and AHC attributions were used to estimate the contributions of anthropogenic and biogenic hydrocarbons to regional tropospheric ozone production, and substantial BHC‐O 3 (50–60 ppbv) was estimated in cases where high NO x from power plants was present in areas of high BHC emission. This estimation method provides direct evidence of significant photochemical ozone production from the oxidation of biogenic hydrocarbons in the presence of NO x .