Modelling the ambient distribution of organic compounds during the august 2003 ozone episode in the southern UK.

A photochemical trajectory model containing speciated emissions of 124 non-methane volatile organic compounds (VOC), and a comprehensive description of the chemistry of VOC degradation, has been used to simulate the chemical evolution of boundary layer air masses arriving at a field campaign site in the southern UK during a widespread and prolonged photochemical pollution event in August 2003. The simulated concentrations and distributions of organic compounds at the arrival location are compared with observations of a series of hydrocarbons and carbonyl compounds, which were measured using GC-FID and multidimensional GC methods. The comparison of the simulated and observed distributions of 34 emitted hydrocarbons provides some support for the magnitude and applied emissions speciation of anthropogenic hydrocarbons, but is indicative of an under representation of the input of biogenic hydrocarbons, particularly at elevated temperatures. Simulations of the detailed distribution of ca. 1250 carbonyl compounds, formed primarily from the degradation of the 124 emitted VOC, focus on 61 aldehydes, ketones, dicarbonyls, hydroxycarbonyls and aromatic aldehydes which collectively account for ca. 90% of the simulated total molar concentration of carbonyls. The simulated distributions indicate that the photolysis of formaldehyde and alpha-dicarbonyls make major contributions to free radical production for the arrival conditions of five case study trajectories. The simulated concentrations of hydroxycarbonyls demonstrate preferential formation of the 1,4-substituted isomers (compared with 1,2- and 1,3-isomers of the same carbon number), which are formed during the initial oxidation sequence of longer chain alkanes.

[1]  C. Pio,et al.  Evaluation of isoprene degradation in the detailed tropospheric chemical mechanism, MCM v3, using environmental chamber data , 2005 .

[2]  R. Derwent,et al.  Multi-day ozone formation for alkenes and carbonyls investigated with a master chemical mechanism under European conditions , 2005 .

[3]  R. Griffin Modeling the oxidative capacity of the atmosphere of the south coast air basin of California. 2. HOx radical production. , 2004, Environmental science & technology.

[4]  P. Siskos,et al.  Carbonyl compounds in the urban environment of Athens, Greece. , 2003, Chemosphere.

[5]  A. Lewis,et al.  Peak amplitude and resolution in comprehensive gas chromatography using valve modulation , 2003 .

[6]  A. Lewis,et al.  Monoaromatic complexity in urban air and gasoline assessed using comprehensive GC and fast GC-TOF/MS , 2003 .

[7]  A. Lewis,et al.  A two-column method for long-term monitoring of non-methane hydrocarbons (NMHCs) and oxygenated volatile organic compounds (o-VOCs). , 2003, Journal of environmental monitoring : JEM.

[8]  S. M. Aschmann,et al.  Formation and atmospheric reactions of 4,5-dihydro-2-methylfuran , 2002 .

[9]  R. Derwent,et al.  Development of a reduced speciated VOC degradation mechanism for use in ozone models , 2002 .

[10]  E. Grosjean,et al.  Speciated ambient carbonyls in Rio de Janeiro, Brazil. , 2002, Environmental science & technology.

[11]  M. Jenkin,et al.  The origin and day-of-week dependence of photochemical ozone episodes in the UK , 2002 .

[12]  S. M. Aschmann,et al.  Atmospheric Chemistry of Three C10 Alkanes , 2001 .

[13]  S. M. Aschmann,et al.  Alkyl Nitrate, Hydroxyalkyl Nitrate, and Hydroxycarbonyl Formation from the NOx−Air Photooxidations of C5−C8 n-Alkanes , 2001 .

[14]  B. P. Andreini,et al.  Aldehydes in the atmospheric environment: evaluation of human exposure in the north-west area of Milan , 2000 .

[15]  Lei Zhu,et al.  Wavelength-Dependent Photolysis of Methylglyoxal in the 290−440 nm Region , 2000 .

[16]  A. Volz-Thomas,et al.  On the budget of hydroxyl radicals at Schauinsland during the Schauinsland Ozone Precursor Experiment (SLOPE96) , 2000 .

[17]  Peter Y.J. Zandveld,et al.  Sectoral emission inventories of greenhouse gases for 1990 on a per country basis as well as on 1°×1° , 1999 .

[18]  R. Derwent,et al.  Photochemical ozone creation potentials for organic compounds in northwest Europe calculated with a master chemical mechanism , 1998 .

[19]  Webster,et al.  Hydrogen radicals, nitrogen radicals, and the production of O3 in the upper troposphere , 1998, Science.

[20]  D. Klemp,et al.  Long-Term Measurements of Light Hydrocarbons (C2–C5) at Schauinsland (Black Forest) , 1997 .

[21]  C. N. Hewitt,et al.  Biogenic emissions in Europe: 1. Estimates and uncertainties , 1995 .

[22]  C. N. Hewitt,et al.  A global model of natural volatile organic compound emissions , 1995 .

[23]  Patrick R. Zimmerman,et al.  Natural volatile organic compound emission rate estimates for U.S. woodland landscapes , 1994 .

[24]  N. Blake,et al.  The seasonal variation of nonmethane hydrocarbons in the free troposphere over the North Atlantic Ocean: Possible evidence for extensive reaction of hydrocarbons with the nitrate radical , 1993 .

[25]  M. Jenkin,et al.  The UV-visible absorption spectrum of methylglyoxal , 1991 .

[26]  W. Carter,et al.  Hydroxyl radical rate constants and photolysis rates of .alpha.-dicarbonyls. , 1983, Environmental science & technology.

[27]  R. Atkinson Atmospheric chemistry of VOCs and NOx , 2000 .

[28]  K. Clemitshaw,et al.  Ozone and other secondary photochemical pollutants: chemical processes governing their formation in the planetary boundary layer , 2000 .

[29]  C. S. Christensen,et al.  Temporal variation of carbonyl compound concentrations at a semi-rural site in Denmark , 2000 .

[30]  M. Frattoni,et al.  A train of carbon and DNPH-coated cartridges for the determination of carbonyls from C1 to C12 in air and emission samples , 2000 .

[31]  M. Jenkin,et al.  The tropospheric degradation of volatile organic compounds: a protocol for mechanism development , 1997 .

[32]  R. Derwent,et al.  Photochemical ozone creation potentials for a large number of reactive hydrocarbons under European conditions , 1996 .

[33]  D. Stocker,et al.  Isomerization of Alkoxy Radicals under Atmospheric Conditions. , 1995, Environmental science & technology.

[34]  S. M. Saunders,et al.  Atmospheric Chemistry and Physics Protocol for the Development of the Master Chemical Mechanism, Mcm V3 (part B): Tropospheric Degradation of Aromatic Volatile Organic Compounds , 2022 .