Constraining Condensed-Phase Kinetics of Secondary Organic Aerosol Components from Isoprene Epoxydiols Theran Riedel, Ying-Hsuan Lin, Zhenfa Zhang, Kevin.

Slides:



Advertisements
Similar presentations
High-Order DDM Sensitivity Analysis of Particular Matter in CMAQ Wenxian Zhang, Shannon Capps, Yongtao Hu, Athanasios Nenes, and Armistead Russell Georgia.
Advertisements

Office of Research and Development National Exposure Research Lab, Atmospheric Modeling and Analysis Division 28 October 2013 H. O. T. Pye, R. Pinder,
PHOTOPRODUCTION OF VOLATILE ORGANIC COMPOUNDS FROM SECONDARY ORGANIC AEROSOLS: AN UNEXPLAINED SOURCE? Kurtis Malecha Nizkorodov Group September 4, 2014.
Development of a Secondary Organic Aerosol Formation Mechanism: Comparison with Smog Chamber Experiments and Atmospheric Measurements Luis Olcese, Joyce.
FINE AEROSOL COMPOSITION IN NORTH AMERICA Annual mean PM 2.5 concentrations (NARSTO, 2004) Current air quality standard is 15  g m -3.
Modeled Trends in Impacts of Landing and Takeoff Aircraft Emissions on Surface Air-Quality in U.S for 2005, 2010 and 2018 Lakshmi Pradeepa Vennam 1, Saravanan.
Havala O. T. Pye 1, Rob Pinder 1, Ying Xie 1, Deborah Luecken 1, Bill Hutzell 1, Golam Sarwar 1, Jason Surratt 2 1 US Environmental Protection Agency 2.
Incorporation of the Model of Aerosol Dynamics, Reaction, Ionization and Dissolution (MADRID) into CMAQ Yang Zhang, Betty K. Pun, Krish Vijayaraghavan,
Evaluation of Secondary Organic Aerosols in Atlanta
A new parameterization of biogenic SOA formation based on smog chamber data: 3D testing in CMAQ Manuel Santiago 1, Ariel F. Stein 2, Marta G. Vivanco 1,
Secondary Organic Aerosols: What we know and current CAM treatment Chemistry-Climate Working Group Meeting, CCSM March 22, 2006 Colette L. Heald
Christian Seigneur AER San Ramon, CA
The Framework of Modeling SOA Formation from Toluene Oxidation Di Hu and Richard Kamens Department of Environmental Sciences and Engineering, University.
Developing Secondary Organic Aerosol (SOA) Code for the MCM David Johnson (Mike Jenkin and Steve Utembe) Department of Environmental Science and Technology,
Atmospheric Heterogeneous Chemistry of HO 2 Joel Thornton and Jonathan Abbatt Department of Chemistry University of Toronto $$ Natural Sciences and Engineering.
The Contribution of Marine Organic Emissions to Coastal Air Quality Brett Gantt Advisor: Nicholas Meskhidze Co-Author: Annmarie Carlton (EPA) North Carolina.
1 Huff Hartz Research Group What are aerosol yields from a precursor mixture that reflects the complexity of atmospheric emissions? Do the aerosol yields.
Modeling Elemental Composition of Organic Aerosol: Exploiting Laboratory and Ambient Measurement and the Implications of the Gap Between Them Qi Chen*
Background Air Quality in the United States Under Current and Future Emissions Scenarios Zachariah Adelman, Meridith Fry, J. Jason West Department of Environmental.
1 Influence of dilution and particle fractal dimension of diesel exhaust on measured SOA formation in a smog chamber Shunsuke Nakao (1,
Status and Plans of the CLOUD Experiment Urs Baltensperger Laboratory of Atmospheric Chemistry Paul Scherrer Institute, 5232 Villigen, Switzerland SPSC.
Biogenic Aerosol Studies Smog chamber studies >Aerosol yields (humidity, temperature, seed) >Product identification and quantification (GCMS, LCMS, TDPBMS)
Organic aerosol and its climate impact Min Zhong and Myoseon Jang Sept. 24, 2013 Department of Environmental Engineering Sciences University of Florida.
Gas, Cloudwater, and Rain Hydrogen Peroxide and Methylhydroperoxide Measurements in RICO Brian G. Heikes, Center for Atmospheric Chemical Studies, Graduate.
Office of Research and Development National Exposure Research Laboratory Atmospheric Modeling Division, Research Triangle Park, NC September 17, 2015 Annmarie.
Trees, Volatile Organic Compounds, and Fine Organic Aerosol Formation: Implications for Air Quality, Climate and Public Health in the Southeastern U.S.
Modeling and measurements of oxygen isotope tracers of sulfate formation: Implications for the sulfur budget in the marine boundary layer Becky Alexander,
School of something FACULTY OF OTHER 1 Lecture 2: Aerosol sources and sinks Ken Carslaw.
Yuzhi Chen 13th CMAS Assessment of SAPRC07 with Updated Isoprene Chemistry against Outdoor Chamber Experiments Yuzhi Chen a, Roger Jerry a, Kenneth Sexton.
EVALUATION AND IMPROVEMENT OF GAS/PARTICLE MASS TRANSFER TREATMENTS FOR 3-D AEROSOL SIMULATION AND FORECAST Xiaoming Hu and Yang Zhang North Carolina State.
Trees, Volatile Organic Compounds, and Fine Organic Aerosol Formation: Implications for Air Quality, Climate and Public Health in the Southeastern U.S.
The Use of Source Apportionment for Air Quality Management and Health Assessments Philip K. Hopke Clarkson University Center for Air Resources Engineering.
1 Comparison of CAMx and CMAQ PM2.5 Source Apportionment Estimates Kirk Baker and Brian Timin U.S. Environmental Protection Agency, Research Triangle Park,
Charmex workshop Trieste 1/Total Working sesssion « chemical processes » overview Relevant questions : -VOC reactivity, oxidized.
Sensitivity Evaluation of Gas-phase Reduction Mechanisms of Divalent Mercury Using CMAQ-Hg in a Contiguous US Domain Pruek Pongprueksa a, Che-Jen Lin a,
Regional and temporal trends in semi-empirical estimates of aerosol water concentration in the continental U.S. Thien Khoi V. Nguyen 1 Annmarie G. Carlton.
Gas and Aerosol Partitioning Over the Equatorial Pacific Wenxian Zhang April 21, 2009.
Parameterization of Global Monoterpene SOA formation and Water Uptake, Based on a Near-explicit Mechanism Karl Ceulemans – Jean-François Müller – Steven.
Karl Ceulemans– Steven Compernolle – Jean-François Müller
The Land Breeze and ClNO 2 production over Santa Monica Bay Nick Wagner, Steven S. Brown, William P. Dubé, Brian M. Lerner, Eric J. Williams, Wayne Angevine,
Model Evaluation Comparing Model Output to Ambient Data Christian Seigneur AER San Ramon, California.
Secondary Organic Aerosols
Detection of Nitrooxypolyols in Secondary Organic Aerosol |Formed from the Photooxidation of Conjugated dienes under High- NOx Conditions Kei Sato, Atmospheric.
Eric Edgerton, ARA, Inc. PM Model Performance Workshop Chapel Hill, NC February 10, 2004 SEARCH: Overview of Data for Model Performance Evaluation Photo.
William G. Benjey* Physical Scientist NOAA Air Resources Laboratory Atmospheric Sciences Modeling Division Research Triangle Park, NC Fifth Annual CMAS.
1 On the relationship between nitryl chloride (ClNO 2 ) and molecular chlorine (Cl 2 ) in coastal California Joel Thornton and Theran Riedel Department.
Simulating the Oxygen Content of Organic Aerosol in a Global Model
Extending Size-Dependent Composition to the Modal Approach: A Case Study with Sea Salt Aerosol Uma Shankar and Rohit Mathur The University of North Carolina.
1 Role of Glyoxal in SOA Formation from Aromatic Hydrocarbons SHUNSUKE NAKAO, Yingdi Liu, Ping Tang, Chia-Li Chen, David Cocker AAAR 2011.
1 Prakash Karamchandani 1, David Parrish 2, Lynsey Parker 1, Thomas Ryerson 3, Paul O. Wennberg 4, Alex Teng 4, John D. Crounse 4, Greg Yarwood 1 1 Ramboll.
Yunseok Im and Myoseon Jang
Multiscale Predictions of Aircraft-Attributable PM 2.5 Modeled Using CMAQ-APT enhanced with an Aircraft-Specific 1-D Model for U.S. Airports Matthew Woody,
Oxygen isotope tracers of atmospheric sulfur/oxidant chemistry Becky Alexander Harvard University NOAA Postdoctoral Fellow ACCESS, September 2003.
SOA derived from isoprene epoxydiols: Insights into formation, aging and distribution over the continental US from the DC3 and SEAC 4 RS campaigns Pedro.
Template Comparison of PM Source Apportionment and Sensitivity Analysis in CAMx Bonyoung Koo, Gary Wilson, Ralph Morris, Greg Yarwood ENVIRON Alan Dunker.
W. T. Hutzell 1, G. Pouliot 2, and D. J. Luecken 1 1 Atmospheric Modeling Division, U. S. Environmental Protection Agency 2 Atmospheric Sciences Modeling.
Secondary Aerosol Formation from Atmospheric Gas and Particle Phase Reactions of Toluene Department of Environmental Science and Engineering, UNC, Chapel.
2008 CMAS Conference Poster Session October 7, Interactions of Air Quality and Regional Climate and Intercontinental Transport of Air Pollutants.
EPA STAR Grants Contribution to the SOAS Campaign SHERRI HUNT Office of Research and Development, U.S. Environmental Protection Agency;
Understanding the impact of isoprene nitrates and OH reformation on regional air quality using recent advances in isoprene photooxidation chemistry Ying.
Havala O. T. Pye1 With contributions from:
Organic Aerosol is Ubiquitous in the Atmosphere
Yongtao Hu, Jaemeen Baek, M. Talat Odman and Armistead G. Russell
Secondary Organic Aerosol Contributions during CalNex – Bakersfield
Oxygen isotope tracers of atmospheric sulfur/oxidant chemistry
Aerosol Optical Thickness
Secondary Organic Aerosols Enhancement by Sulfuric Dioxide
Methylfuran Oxidation by Nitrate Radical
University of Alaska Fairbanks
Potential Anthropogenic Controls on Biogenic Organic Aerosol
Presentation transcript:

Constraining Condensed-Phase Kinetics of Secondary Organic Aerosol Components from Isoprene Epoxydiols Theran Riedel, Ying-Hsuan Lin, Zhenfa Zhang, Kevin Chu, Joel Thornton, William Vizuete, Avram Gold, and Jason Surratt Dept. of Environmental Sciences and Engineering The Gillings School of Global Public Health University of North Carolina at Chapel Hill CMAS Conference October 5,

isoprene epoxydiols (IEPOX) and SOA 2 Aerosol Phase “tracers”  aerosol products from IEPOX that contribute to SOA mass ~50% of isoprene  IEPOX (rural) ~500 Tg/year isoprene even at low conversion (urban) lots of potential mass to aerosols Gas Phase

IEPOX-tracer formation 3 Gaston et al., ES&T 2014; Riedel et al., ES&TL 2015 Eddingsaas et al., JPCA 2010; Cole-Filipiak et al., ES&T 2010; Piletic et al., PCCP 2013 k het =  S a  /4 k  9e-4 M -2 s -1 k  2e-4 M -2 s -1 k = ?? Recent interest in explicit modeling of SOA formation due to model-measurement deviations GAMMA: McNeill et al., ES&T 2012 CMAQ: Pye et al., ES&T 2013; Karambelas et al., ES&TL 2014 Need for more constraints on SOA formation kinetics experiments and modeling

4 IEPOX chamber SOA experiments 10 m 3 teflon chamber RH: < 5% aerosol seed: (NH 4 ) 2 SO 4 + H 2 SO 4 IEPOX injected: 600 ppbv seed injection and stabilization IEPOX injection Filter collection SOA Total SOA growth: 170  g m -3

IEPOX-tracer quantification 5 GC/MS: 2-methyltetrols, C 5 -alkene triols, 3-MeTHF-3,4-diols, IEPOX-dimer LC/ESI-MS : IEPOX-OS, IEPOX-dimerOS other SOA “other SOA”  IEPOX-SOA products not quantified through offline measurements

explicit chamber-SOA modeling 6 0-D time-dependent box model Model run time = experiment duration Initialize model with: chamber measured seed aerosol [S a ] and [mass] E-AIM calculated seed aerosol composition [SO 4 2- ], [HSO 4 - ], [H 2 O], [H + ] Explicitly track: IEPOX (g), IEPOX (aq) 2-methyltetrols, organosulfate, C 5 -alkene triols, 3-MeTHF-3,4-diols, IEPOX dimer, IEPOX dimer organosulfate, other SOA [SO 4 2- ], [HSO 4 - ] Vary model aqueous rate constants to minimize difference between model output and filter measurements

explicit chamber-SOA modeling 7 IEPOX (g) IEPOX (aq) 2-methyltetrol dimer organosulfate C 5 -alkene triol 3-MeTHF-3,4-diol dimer OS H +, SO 4 2- H +, H 2 O H+H+ H+H+ H +, IEPOX other SOA H+H+ volatile products SOA yield (  SOA ) < 1, so invoke volatile product formation

model output 8

9

model-estimated rate constants 10

molar SOA yield (  SOA ) 11 Riedel et al., ES&TL 2015:  SOA = 0.1 – 0.12

atmospheric-type simulation 12 Total predicted SOA mass = 0.37  g m -3 Initialize with: 500 pptv IEPOX ammonium bisulfate aerosol 250  m 2 /cm 3 aerosol S a 50% RH 6-hour processing time 2-methyltetrols288 ng/m 3 IEPOX-OS52 ng/m 3 C 5 -alkene triols25 ng/m 3 3-MeTHF-3,4-diols7.4 ng/m 3 IEPOX-dimer0.1 ng/m 3 IEPOX-dimerOS0.1 ng/m 3 other SOA0.6 ng/m 3

atmospheric-type simulation 13 Look Rock, TN (Budisulistiorini et al., ACP 2015) Yorkville, GA (Lin et al., ES&T 2012)  tracers = ng m -3 study mean (ng m -3 ) Total predicted SOA mass = 0.37  g m -3  tracers = ng m -3

final thoughts estimated formation rate constants for IEPOX-SOA tracers that have yet to be constrained by bulk measurements –agreed well with experimentally obtained estimates (2-methyltetrols and IEPOX-OS) can be extended to other SOA production systems (i.e.,  -pinene) important to test that current understanding can account for SOA production in simple systems recently this work submitted to ACPD 14

acknowledgements UNC Surratt Group Jason Surratt Ying-Hsuan Lin Matthieu Riva Sri Hapsari Budisulistiorini Xinxin Li Maiko Arashrio Tianqu Cui Weruka Rattanavaraha Kevin Chu UNC Gold Group Avram Gold Zhenfa Zhang Funding: University of Washington Joel Thornton Cassandra Gaston NSF: CHE and Texas Commission on Environmental Quality

16 the end… thanks!

17 junk slides

model output: titration of aerosol sulfate 18 Low-NO x isoprene oxidation (IEPOX formation) with acidified ammonium sulfate seed aerosol from Surratt et al., ES&T, 2007 Model output (this study):

19

20 Recent interest in explicit modeling of SOA formation due to model-measurement deviations GAMMA: McNeill et al., ES&T 2012 CMAQ: Pye et al., ES&T 2013; Karambelas et al., ES&TL 2014 Need for more constraints on SOA formation kinetics experiments and modeling