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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
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Outline Why aromatics SOA formation potential from aromatics Overall goal of my research
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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 10 6 to 2.4 x 10 6 tons/year.
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Why aromatics? Composition, Chemistry, and Climate of the Atmosphere; New York, 1995
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Why aromatics? Toluene 23.5% m,p-Xylene12.6%1,2,4-Trimetylbenzene8.5% Benzene 7.4% Composition, Chemistry, and Climate of the Atmosphere; New York, 1995
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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)
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SOA Formation Potential of Aromatics
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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.
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Evidences for Polymer Formation in SOA from the Photo-oxidation of Aromatics/NOx System
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FTIR Spectra of Toluene and Glyoxal Aerosols Slide from Dr. Myoseon Jang Slide from Dr. Myoseon Jang
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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)
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LDI-TOFMS Spectrum of SOA from Photo-oxidation of 1,3,5- Trimethylbezene
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Time Evolution of Polymer in SOA Measured by LDI-MS
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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.
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Overall Approach Kinetic mechanism development Outdoor chamber experiments Simulation of chamber experiments
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Gas Phase Reactions
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Toluene react with OH
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Recent research from Mario Molina’s group has shown that the pathway to form epoxide radicals are neglectable.
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Existing Mechanisms Carbon Bond Carter’s Mechanism Master Chemical Mechanism
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Toluene react with OH
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'C7H8' + OH ----> 0.72*'CH3-C6H5(OH)-OO.' + 0.1*'C6H5CO-H' + 0.18*'CRESOL’ 0.1*'C6H5CO-H' + 0.18*'CRESOL’ +0.28*HO2 + 0.1*XO2 +0.28*HO2 + 0.1*XO2 @ 1.18E-12* EXP(338.0/TK) @ 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' + + 0.11*'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 0.45*'H-CO-CO-H'+ NO2 +HO @ 8.1E-12 @ 8.1E-12
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Reaction of 1 st Generation Product
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'CH3-CO-CH=CH-CO-H' + OH ----> 0.2*('CH3-CO-CH=CH-CO-O2.‘ +H2O) + 0.4*'OXOCYL_RAD' + +H2O) + 0.4*'OXOCYL_RAD' + 0.2*'CH3-CO-CH(OH)-CH(OO.)-CO-H' 0.2*'CH3-CO-CH(OH)-CH(OO.)-CO-H' + 0.2*'CH3-CO-CH(OO.)-CH(OH)-CO-H' + 0.2*'CH3-CO-CH(OO.)-CH(OH)-CO-H' @ 5.58E-11 @ 5.58E-11 'OXOCYL_RAD' + NO -O2-> 'Maleic anhydrid' + 'CH3.' + NO2 @ 3.0*k_MEO2_NO @ 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 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) + 0.5*('CH3-CO-CO-H'+ 'H-CO-CO-H'+ HO2) + 0.2*(C5OHALD+ HO2) + 0.2*(C5OHALD+ HO2) @ k_DEC @ k_DEC
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2 nd Generation Gas Phase Products
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3 rd Generation Gas Phase Products
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Simulation Results of Gas Phase Chemistry
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Particle Formation Processes G/P Partitioning Particle Phase Reactions
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G/P Partitioning K p =k on /k off = 7.501RTf om /(10 9 Mwp 0 L ) k off =k b T/h exp(-E a /RT) k b T/h = 6.2110 12 sec -1 at 298K Relate E a to log p o L k on =K P k off
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To Represent These Processes in the Mechanism
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C4OHALD gas + SEED ----> C4OHALD part + SEED @ kon @ kon C4OHALD gas + TSP ----> C4OHALD part + TSP @ kon @ kon C4OHALD part ----> C4OHALD gas @ koff
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Particle Phase Reactions
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GlyP + H2O ----> Gly2OHP @ kpart1 Gly2OHP + H2O ----> Gly4OHP @ kpart2 Gly4OHP + GlyAcidP ----> pre-Poly1 @ kpart3 Pre-Poly1 + C4OHALD ----> Poly1 @ kpart4 Do these reactions well represent what really happens in the particle phase? Particle phase reaction rate coefficients
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Outdoor Chamber Experiments
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The Outdoor Chamber Reactor System
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Hanging Teflon
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Dual 270m 3 chamber fine particle t 1/2 >17 h
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Product Analysis
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Toluene/propylene/NOx/sunlight chamber experiments were carried out with neutral seed and acidic seed.
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Analytical Methods Derivatization methods to identify the precursors of polymers. LC-ESIMS/MS to identify structure of polymers.
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PFBHA O-(2,3,4,5,6- pentafluorobenzyl) -hydroxylamine for carbonyl groups
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PFBBr, Pentafluorobenzyl bromide derivatization for carboxylic and aromatic-OH
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The three slides are from Prof. Rich Kamens The three slides are from Prof. Rich Kamens BSTFA for hydroxyl, and/or carboxylic groups BSTFA ROH carboxylic acid or alcohol CN Si(CH 3 ) 3 CF 3 O (CH 3 ) 3 Si R O (CH 3 ) 3 Si
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BF 3 -CH 3 OH + BSTFA Derivatization Method GC-ITMS analysis - electron impact ionization (EI) - methane chemical ionization (CI-methane) - tandem mass spectrometry (MS/MS) Slide from Dr. Mohammed Jaoui Citramalic acid
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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.
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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
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Overall Approach Kinetic mechanism development Outdoor chamber experiments Simulation of chamber experiments
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Future Plan Methylglyoxal experiments in this summer Some of the toluene/NO x chamber experiments Proposal at the end of this summer
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Thank you for your time
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