Gas‐phase products and secondary aerosol yields from the ozonolysis of ten different terpenes

The ozonolyses of six monoterpenes (α-pinene, β-pinene, 3-carene, terpinolene, α-terpinene, and myrcene), two sesquiterpenes (α-humulene and β-caryophyllene), and two oxygenated terpenes (methyl chavicol and linalool) were conducted individually in Teflon chambers to examine the gas-phase oxidation product and secondary organic aerosol (SOA) yields from these reactions. Particle size distribution and number concentration were monitored and allowed for the calculation of the SOA yield from each experiment, which ranged from 1 to 54%. A proton transfer reaction mass spectrometer (PTR-MS) was used to monitor the evolution of gas-phase products, identified by their mass to charge ratio (m/z). Several gas-phase oxidation products, formaldehyde, acetaldehyde, formic acid, acetone, acetic acid, and nopinone, were identified and calibrated. Aerosol yields, and the yields of these identified and calibrated oxidation products, as well as many higher m/z oxidation products observed with the PTR-MS, varied significantly between the different parent terpene compounds. The sum of measured oxidation products in the gas and particle phase ranged from 33 to 77% of the carbon in the reacted terpenes, suggesting there are still unmeasured products from these reactions. The observations of the higher molecular weight oxidation product ions provide evidence of previously unreported compounds and their temporal evolution in the smog chamber from multistep oxidation processes. Many of the observed ions, including m/z 111 and 113, have also been observed in ambient air above a Ponderosa pine forest canopy, and our results confirm they are consistent with products from terpene + O_3 reactions. Many of these products are stable on the timescale of our experiments and can therefore be monitored in field campaigns as evidence for ozone oxidative chemistry.

[1]  J. Seinfeld,et al.  Contribution of first- versus second-generation products to secondary organic aerosols formed in the oxidation of biogenic hydrocarbons. , 2006, Environmental science & technology.

[2]  R. I C H,et al.  Contribution of First-versus Second-Generation Products to Secondary Organic Aerosols Formed in the Oxidation of Biogenic Hydrocarbons , 2006 .

[3]  Albert A Presto,et al.  Secondary organic aerosol production from terpene ozonolysis. 1. Effect of UV radiation. , 2005, Environmental science & technology.

[4]  Albert A Presto,et al.  Secondary organic aerosol production from terpene ozonolysis. 2. Effect of NOx concentration. , 2005, Environmental science & technology.

[5]  R C Flagan,et al.  Measurements of secondary organic aerosol from oxidation of cycloalkenes, terpenes, and m-xylene using an Aerodyne aerosol mass spectrometer. , 2005, Environmental science & technology.

[6]  Yong Bin Lim,et al.  Contributions of organic peroxides to secondary aerosol formed from reactions of monoterpenes with O3. , 2005, Environmental science & technology.

[7]  A. Presto,et al.  Secondary Organic Aerosol Production from Terpene Ozonolysis. 2. Effect of NO x Concentration , 2005 .

[8]  A. Goldstein,et al.  A comparison of new measurements of total monoterpene flux with improved measurements of speciated monoterpene flux , 2004 .

[9]  A. Goldstein,et al.  Forest thinning experiment confirms ozone deposition to forest canopy is dominated by reaction with biogenic VOCs , 2004 .

[10]  K. T. Paw,et al.  Observations of oxidation products above a forest imply biogenic emissions of very reactive compounds , 2004 .

[11]  Michael E. Jenkin,et al.  Modelling the formation and composition of secondary organic aerosol from α- and β-pinene ozonolysis using MCM v3 , 2004 .

[12]  M. P. Scheele,et al.  Stratospheric age of air computed with trajectories based on various 3D-Var and 4D-Var data sets , 2004 .

[13]  J. Seinfeld,et al.  Secondary organic aerosol formation from the ozonolysis of cycloalkenes and related compounds. , 2004, Environmental science & technology.

[14]  R C Flagan,et al.  Secondary organic aerosol formation from cyclohexene ozonolysis: effect of OH scavenger and the role of radical chemistry. , 2004, Environmental science & technology.

[15]  Paul B. Shepson,et al.  Missing OH Reactivity in a Forest: Evidence for Unknown Reactive Biogenic VOCs , 2004, Science.

[16]  P. Ziemann,et al.  Effects of Stabilized Criegee Intermediate and OH Radical Scavengers on Aerosol Formation from Reactions of β-Pinene with O 3 , 2003 .

[17]  Frank Stratmann,et al.  Gas-phase ozonolysis of α-pinene: gaseous products and particle formation , 2003 .

[18]  R. Kamens,et al.  Gas and Particle Products Distribution from the Reaction of β-Caryophyllene with Ozone , 2003 .

[19]  R. Kamens,et al.  Gas phase photolysis of pinonaldehyde in the presence of sunlight , 2003 .

[20]  A. Goldstein,et al.  Gas‐phase chemistry dominates O3 loss to a forest, implying a source of aerosols and hydroxyl radicals to the atmosphere , 2003 .

[21]  A. Goldstein,et al.  Increase of monoterpene emissions from a pine plantation as a result of mechanical disturbances , 2003 .

[22]  R. Dingenen,et al.  LC-MS analysis of aerosol particles from the oxidation of α-pinene by ozone and OH-radicals , 2003 .

[23]  Roger Atkinson,et al.  Gas-phase tropospheric chemistry of biogenic volatile organic compounds: a review , 2003 .

[24]  R. Kamens,et al.  Heterogeneous Atmospheric Aerosol Production by Acid-Catalyzed Particle-Phase Reactions , 2002, Science.

[25]  S. M. Aschmann,et al.  OH radical formation from the gas-phase reactions of O3 with a series of terpenes , 2002 .

[26]  A. Reissell,et al.  Products of the OH radical‐ and O3‐initiated reactions of myrcene and ocimene , 2002 .

[27]  S. M. Aschmann,et al.  Reactions of stabilized criegee intermediates from the gas‐phase reactions of O3 with selected alkenes , 2002 .

[28]  A. Wisthaler,et al.  Measurements of acetone and other gas phase product yields from the OH-initiated oxidation of terpenes by proton-transfer-reaction mass spectrometry (PTR-MS) , 2001 .

[29]  P. Shepson,et al.  Nighttime observations of anomalously high levels of hydroxyl radicals above a deciduous forest canopy , 2001 .

[30]  R C Flagan,et al.  State-of-the-art chamber facility for studying atmospheric aerosol chemistry. , 2001, Environmental science & technology.

[31]  T. Hoffmann,et al.  On-line measurements of α-pinene ozonolysis products using an atmospheric pressure chemical ionisation ion-trap mass spectrometer , 2001 .

[32]  James G. Anderson,et al.  Mechanism of HOx Formation in the Gas-Phase Ozone-Alkene Reaction. 1. Direct, Pressure-Dependent Measurements of Prompt OH Yields†. , 2001, The journal of physical chemistry. A.

[33]  B. Lamb,et al.  Biogenic Hydrocarbons in the Atmospheric Boundary Layer: A Review , 2000 .

[34]  Y. Rudich,et al.  Product studies of the OH‐ and ozone‐initiated oxidation of some monoterpenes , 2000 .

[35]  G. Moortgat,et al.  Products and Mechanism of the Gas Phase Reaction of Ozone with β-Pinene , 2000 .

[36]  C. Geron,et al.  A review and synthesis of monoterpene speciation from forests in the United States. , 2000 .

[37]  John H. Seinfeld,et al.  Gas-Phase Ozone Oxidation of Monoterpenes: Gaseous and Particulate Products , 1999 .

[38]  A. Reissell,et al.  Formation of acetone from the OH radical‐ and O3‐initiated reactions of a series of monoterpenes , 1999 .

[39]  J. Kesselmeier,et al.  Biogenic Volatile Organic Compounds (VOC): An Overview on Emission, Physiology and Ecology , 1999 .

[40]  R. Valentini,et al.  Emission of reactive terpene compounds from orange orchards and their removal by within‐canopy processes , 1999 .

[41]  J. Seinfeld,et al.  Observation of gaseous and particulate products of monoterpene oxidation in forest atmospheres , 1999 .

[42]  D. Kotzias,et al.  Gas Phase Terpene Oxidation Products. A Review. , 1999 .

[43]  John H. Seinfeld,et al.  Organic aerosol formation from the oxidation of biogenic hydrocarbons , 1999 .

[44]  R. Kamens,et al.  Newly characterized products and composition of secondary aerosols from the reaction of α-pinene with ozone , 1999 .

[45]  N. Mihalopoulos,et al.  Formation and gas/particle partitioning of monoterpenes photo‐oxidation products over forests , 1999 .

[46]  S. M. Aschmann,et al.  Products of the gas‐phase reactions of O(3 P) atoms and O3 with α‐pinene and 1,2‐dimethyl‐1‐cyclohexene , 1998 .

[47]  Werner Lindinger,et al.  Proton-transfer-reaction mass spectrometry (PTR–MS): on-line monitoring of volatile organic compounds at pptv levels , 1998 .

[48]  J. Arey,et al.  Products of the Gas-Phase Reactions of Linalool with OH Radicals, NO3 Radicals, and O3 , 1997 .

[49]  Frank M. Bowman,et al.  Formation of Organic Aerosols from the Oxidation of Biogenic Hydrocarbons , 1997 .

[50]  R. Atkinson,et al.  Atmospheric lifetimes and fates of a series of sesquiterpenes , 1995 .

[51]  H. Hakola,et al.  Product formation from the gas-phase reactions of OH radicals and O3 with a series of monoterpenes , 1994 .

[52]  John H. Seinfeld,et al.  Atmospheric oxidation of biogenic hydrocarbons : Reaction of ozone with β-pinene, d-limonene and trans-caryophyllene , 1993 .

[53]  J. Seinfeld,et al.  Photochemical aerosol formation from α‐pinene‐ and β‐pinene , 1992 .

[54]  S. M. Aschmann,et al.  Formation of OH radicals in the gas phase reactions of O3 with a series of terpenes , 1992 .

[55]  John H. Seinfeld,et al.  Aerosol formation in the photooxidation of isoprene and β-pinene , 1991 .

[56]  S. M. Aschmann,et al.  Rate constants for the gas-phase reactions of OH and NO3 radicals and O3 with sabinene and camphene at 296±2 K , 1990 .

[57]  H. Akimoto,et al.  Reactions of ozone with α‐pinene and β‐pinene in air: Yields of gaseous and particulate products , 1989 .

[58]  W. Carter,et al.  Alkyl nitrate formation from the NO/sub x/-air photooxidations of C/sub 2/-C/sub 8/ n-alkanes , 1982 .

[59]  F. Went Blue Hazes in the Atmosphere , 1960, Nature.