Computational Simulation of Secondary Organic Aerosol (SOA) Formation from Toluene Oxidation

dc.contributor.advisorGriffin, Robert J.en_US
dc.contributor.committeeMemberCohan, Daniel S.en_US
dc.contributor.committeeMemberWong, Michael S.en_US
dc.creatorLiu, Yingen_US
dc.date.accessioned2012-09-06T04:47:10Zen_US
dc.date.accessioned2012-09-06T04:47:12Zen_US
dc.date.available2012-09-06T04:47:10Zen_US
dc.date.available2012-09-06T04:47:12Zen_US
dc.date.created2012-05en_US
dc.date.issued2012-09-05en_US
dc.date.submittedMay 2012en_US
dc.date.updated2012-09-06T04:47:13Zen_US
dc.description.abstractToluene is one of the most prevalent aromatic volatile organic compounds (VOCs) in the atmosphere and has large secondary organic aerosol (SOA) yields compared to many other aromatic VOCs. Recent photo-oxidation studies highlight that toluene oxidation produces more SOA than observed previously, particularly at low levels of nitrogen oxides (NOx). This study focuses on: 1.) the development of a gas-phase chemical mechanism describing toluene oxidation by hydroxyl radicals (OH); 2.) the prediction of SOA formation from toluene oxidation products; and 3.) the impact of NOx level on SOA formation. The oxidation mechanism, which includes multiple pathways after the initial OH attack, has been incorporated into the Caltech Atmospheric Chemistry Mechanism (CACM). Toluene concentrations simulated in chamber experiments by the updated CACM as a function of time are typically within 5% of observed values for most experiments. Predicted ozone and NO2 concentrations are typically within 15% of the experimental values. The gas-phase mechanism indicates the importance of bicyclic peroxy radical reactions in determining the product distribution and thus the likelihood of SOA formation. A gas-aerosol partitioning model is used in conjunction with the gas-phase mechanism to simulate SOA formation. Predicted SOA concentrations are typically within 15% of the experimental values. Under low NOx conditions, simulation shows that more than 98% of SOA mass is contributed by bicyclic products from reactions between bicyclic peroxy radicals and other peroxy radicals. Increasing NOx levels cause bicyclic peroxy radicals to react with NO or nitrate radical, leading to fragmentation products that are less likely to form SOA. SOA yield dropped from 19.26% with zero initial NOx to 13.27% with 100 ppb initial NO because of the change in the amount of toluene consumed. Composition of NOx also has an impact on SOA yield and formation, showing that NO has a greater impact on SOA yield and formation than NO2.en_US
dc.format.mimetypeapplication/pdfen_US
dc.identifier.citationLiu, Ying. "Computational Simulation of Secondary Organic Aerosol (SOA) Formation from Toluene Oxidation." (2012) Master’s Thesis, Rice University. <a href="https://hdl.handle.net/1911/64711">https://hdl.handle.net/1911/64711</a>.en_US
dc.identifier.slug123456789/ETD-2012-05-188en_US
dc.identifier.urihttps://hdl.handle.net/1911/64711en_US
dc.language.isoengen_US
dc.rightsCopyright is held by the author, unless otherwise indicated. Permission to reuse, publish, or reproduce the work beyond the bounds of fair use or other exemptions to copyright law must be obtained from the copyright holder.en_US
dc.subjectSecondary organic aerosolsen_US
dc.subjectFormationen_US
dc.subjectSimulationen_US
dc.subjectTolueneen_US
dc.subjectOxidationen_US
dc.titleComputational Simulation of Secondary Organic Aerosol (SOA) Formation from Toluene Oxidationen_US
dc.typeThesisen_US
dc.type.materialTexten_US
thesis.degree.departmentCivil and Environmental Engineeringen_US
thesis.degree.disciplineEngineeringen_US
thesis.degree.grantorRice Universityen_US
thesis.degree.levelMastersen_US
thesis.degree.nameMaster of Scienceen_US
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