TY - JOUR
T1 - Gas-phase ozone oxidation of monoterpenes
T2 - Gaseous and particulate products
AU - Yu, Jianzhen
AU - Cocker, David R.
AU - Griffin, Robert J.
AU - Flagan, Richard C.
AU - Seinfeld, John H.
PY - 1999
Y1 - 1999
N2 - Atmospheric oxidation of monoterpenes contributes to formation of tropospheric ozone and secondary organic aerosol, but their products are poorly characterized. In this work, we report a series of outdoor smog chamber experiments to investigate both gaseous and particulate products in the ozone oxidation of four monoterpenes: α-pinene, β-pinene, Δ3-carene, and sabinene. More than ten oxygenated products are detected and identified in each monoterpene/O3 reaction by coupling derivatization techniques and GC/MS detection. A denuder/filter pack sampling system is used to separate and simultaneously collect gas and aerosol samples. The identified products, consisting of compounds containing carbonyl, hydroxyl, and carboxyl functional groups, are estimated to account for about 34-50%, 57%, 29-67%, and 24% of the reacted carbon mass for β-pinene, sabinene, α-pinene, and Δ3-carene, respectively. The identified individual products account for > 83%, ~ 100%, > 90%, and 61% of the aerosol mass produced in the ozone reaction of β-pinene, sabinene, α-pinene, and Δ3-carene. The uncertainty in the yield data is estimated to be ~ ± 50%. Many of the products partition between gas and aerosol phases, and their gas-aerosol partitioning coefficients are determined and reported here. Reaction schemes are suggested to account for the products observed.
AB - Atmospheric oxidation of monoterpenes contributes to formation of tropospheric ozone and secondary organic aerosol, but their products are poorly characterized. In this work, we report a series of outdoor smog chamber experiments to investigate both gaseous and particulate products in the ozone oxidation of four monoterpenes: α-pinene, β-pinene, Δ3-carene, and sabinene. More than ten oxygenated products are detected and identified in each monoterpene/O3 reaction by coupling derivatization techniques and GC/MS detection. A denuder/filter pack sampling system is used to separate and simultaneously collect gas and aerosol samples. The identified products, consisting of compounds containing carbonyl, hydroxyl, and carboxyl functional groups, are estimated to account for about 34-50%, 57%, 29-67%, and 24% of the reacted carbon mass for β-pinene, sabinene, α-pinene, and Δ3-carene, respectively. The identified individual products account for > 83%, ~ 100%, > 90%, and 61% of the aerosol mass produced in the ozone reaction of β-pinene, sabinene, α-pinene, and Δ3-carene. The uncertainty in the yield data is estimated to be ~ ± 50%. Many of the products partition between gas and aerosol phases, and their gas-aerosol partitioning coefficients are determined and reported here. Reaction schemes are suggested to account for the products observed.
KW - Aerosols
KW - Monoterpenes
KW - Organic aerosols
UR - https://www.webofscience.com/wos/woscc/full-record/WOS:000082480000003
UR - https://openalex.org/W1521360580
UR - https://www.scopus.com/pages/publications/0032857444
U2 - 10.1023/A:1006254930583
DO - 10.1023/A:1006254930583
M3 - Journal Article
SN - 0167-7764
VL - 34
SP - 207
EP - 258
JO - Journal of Atmospheric Chemistry
JF - Journal of Atmospheric Chemistry
IS - 2
ER -