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Secondary Organic Aerosol Formation from Gas and Particle Phase Reactions of Aromatic Hydrocarbons. Di Hu PhD Committee Meeting March 24, 2004. Outline. Why aromatics SOA formation potential from aromatics Overall goal of my research. Sources of Aromatics. Anthropogenic Sources
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Secondary Organic Aerosol Formation from Gas and Particle Phase Reactions of Aromatic Hydrocarbons Di Hu PhD Committee Meeting March 24, 2004
Outline • Why aromatics • SOA formation potential from aromatics • Overall goal of my research
Sources of Aromatics • Anthropogenic Sources Transportation Solvent use Fuel combustion • In the US, transportation sources contribute ~67% to the total aromatic emissions which range from 1.9 x 106 to 2.4 x 106 tons/year.
Why aromatics? • Composition, Chemistry, and Climate of the Atmosphere; New York, 1995
Toluene23.5% m,p-Xylene 12.6% 1,2,4-Trimetylbenzene 8.5% Benzene7.4% Composition, Chemistry, and Climate of the Atmosphere; New York, 1995 Why aromatics?
Jenkin et al. show that in their model calculations up to 40% of photochemically produced ozone can be attributed to emissions of aromatics in urban areas. (Atmos. Environ. 1996)
SOA Formation Potential of Aromatics Sunlight + OH highly oxygenated gas phase products NOx 2-hydroxy-3-oxobutanal Particle
SOA Formation Potential of Aromatics • Recent research has provided strong evidence for polymerization reactions on aromatic aerosols. • This results in a much lower volatility SOA material and higher aerosol yields than partitioning can predict.
Evidences for Polymer Formation in SOA from the Photo-oxidation of Aromatics/NOx System
FTIR Spectra of Toluene and Glyoxal Aerosols Slide from Dr. Myoseon Jang
Kalberer et al. recently have identified polymers as the main constituents of SOA formed from the photo-oxidation of 1,3,5-trimethylbezene, which account for about 50% of the aerosol mass after 30 hours of aging. (Science, 2004)
LDI-TOFMS Spectrum of SOA from Photo-oxidation of 1,3,5-Trimethylbezene
Time Evolution of Polymer in SOA Measured by LDI-MS 2.5hrs 3.5hrs 4.5hrs 6.5hrs methylglyoxal oligomers mixture of methylglyoxal, formaldehyde, 2,5-dimethylbenzaldehyde, and pyruvic acid
Overall Goal of This Project • Integrate particle phase heterogeneous processes with gas phase reaction as a unified, multi-phase, chemical reaction mechanism, which will ultimately permit the prediction of amounts of SOA that result from aromatics reacting in the atmosphere.
Overall Approach • Kinetic mechanism development • Outdoor chamber experiments • Simulation of chamber experiments
Toluene react with OH Epoxy Radical Isomerization Bicyclic Radical Bicyclic Alkoxy Radical 1st generation products
Recent research from Mario Molina’s group has shown that the pathway to form epoxide radicals are neglectable.
Existing Mechanisms • Carbon Bond • Carter’s Mechanism • Master Chemical Mechanism
Toluene react with OH Bicyclic Radical Bicyclic Alkoxy Radical 1st generation products
'C7H8' + OH ---->0.72*'CH3-C6H5(OH)-OO.' + 0.1*'C6H5CO-H' +0.18*'CRESOL’ +0.28*HO2+0.1*XO2 @ 1.18E-12* EXP(338.0/TK) 'CH3-C6H5(OH)-OO.' + NO ---->0.55*'H-CO-CH=CH-CO-H‘ +0.11*'CH3-CO-CH=CH-CO-H'+0.34*'H-CO-C(CH3)=CH-CO-H'+0.55*'CH3-CO-CO-H' + 0.45*'H-CO-CO-H'+ NO2 +HO @8.1E-12
'CH3-CO-CH=CH-CO-H' + OH ----> 0.2*('CH3-CO-CH=CH-CO-O2.‘ +H2O) + 0.4*'OXOCYL_RAD' + 0.2*'CH3-CO-CH(OH)-CH(OO.)-CO-H' + 0.2*'CH3-CO-CH(OO.)-CH(OH)-CO-H' @ 5.58E-11 'OXOCYL_RAD' + NO -O2-> 'Maleic anhydrid' + 'CH3.' + NO2 @ 3.0*k_MEO2_NO 'CH3-CO-CH(OH)-CH(OO.)-CO-H' + NO ---->0.13*C5OHNO3 + 0.87*('CH3-CO-CH(OH)-CH(O.)-CO-H' + NO2)@ 0.71*k_MEO2_NO 'CH3-CO-CH(OH)-CH(O.)-CO-H' + O2 ----> 0.3*(C4OHALD + CO + H2O) + 0.5*('CH3-CO-CO-H'+ 'H-CO-CO-H'+ HO2) + 0.2*(C5OHALD+ HO2) @ k_DEC
Particle Formation Processes • G/P Partitioning • Particle Phase Reactions
G/P Partitioning • Kp =kon/koff = 7.501RTfom/(109Mwgp0L) • koff=kbT/h exp(-Ea/RT) • kbT/h = 6.211012 sec-1 at 298K • Relate Ea to log poL • kon=KPkoff kon koff Particle
C4OHALDgas + SEED ----> C4OHALDpart+ SEED @ kon C4OHALDgas + TSP ----> C4OHALDpart + TSP @ kon C4OHALDpart ----> C4OHALDgas @ koff
Particle Phase Reactions big molecule
Particle Phase Reactions Polymers
GlyP + H2O ----> Gly2OHP @ kpart1 Gly2OHP + H2O ----> Gly4OHP @ kpart2Gly4OHP + GlyAcidP ----> pre-Poly1 @ kpart3Pre-Poly1 + C4OHALD ----> Poly1 @ kpart4 • Do these reactions well represent what really happens in the particle phase? • Particle phase reaction rate coefficients
Toluene/propylene/NOx/sunlight chamber experiments were carried out with neutral seed and acidic seed.
Analytical Methods • Derivatization methods to identify the precursors of polymers. • LC-ESIMS/MS to identify structure of polymers.
PFBHA O-(2,3,4,5,6-pentafluorobenzyl) -hydroxylamine for carbonyl groups aldehyde or ketone
P F B B r F F H C C H 3 3 O O H C H C O H C O F C H B r 2 2 F F F F H C C H O 3 3 O C H C O C H F H O C H B r 2 2 F F F F F F C H C H O O 3 3 C H C O C H F O C 2 H B r F C H 2 2 2 F F F F PFBBr, Pentafluorobenzyl bromide derivatization for carboxylic and aromatic-OH
B S T F A c a r b o x y l i c a c i d C F o r a l c o h o l 3 C N R O H S i ( C H ) ( C H ) S i 3 3 O 3 3 ( C H ) S i O 3 3 R BSTFA for hydroxyl, and/or carboxylic groups The three slides are from Prof. Rich Kamens
BF3-CH3OH + BSTFA Derivatization Method Citramalic acid GC-ITMS analysis - electron impact ionization (EI) - methane chemical ionization (CI-methane) - tandem mass spectrometry (MS/MS) Slide from Dr. Mohammed Jaoui
Particle Phase Reaction Rate Coefficients • Too ambitious to measure the rate coefficient of each single particle phase reaction. • Cross reaction of the multi-functional aldehydes • Many products are not commercially available.
Simple methyglyoxal experiments (daytime/NOx, nighttime) • Do chamber experiment with different toluene and NOx concentrations at different RH and temperature. • Measure particle mass, acidity and HNO3 in particle phase. • Explore relationships that influence rates of particle formation • particle HNO3 • RH and temperature