Determination of Gas/Particle Partitioning of Glyoxal and Other Bifunctional Species using the Annular Denuder-Filter Sampling Technique
|
|
- Irma Todd
- 5 years ago
- Views:
Transcription
1 Determination of Gas/Particle Partitioning of Glyoxal and Other Bifunctional Species using the Annular Denuder-Filter Sampling Technique Simon Ip, Hilda Huang, Jian Zhen Yu Hong Kong University of Science and Technology May, 2010
2 Introduction OUTLINE Sources and abundance of glyoxal Secondary organic aerosols from glyoxal Literature of Gas/Particle measurements of glyoxal Experimental Sulfite-coated method H 2 O 2 vs. Barium Chloride Recovery and Collection Efficiency Results G/P measurements of glyoxal in Hong Kong Gas/particle partition coefficients from field study Estimated Effective Henry s law constant of glyoxal from field study Conclusions 2
3 Introduction
4 Sources of glyoxal VOC precursors Isoprene Terpenes Benzene Toluene Xylene Ethylene O glyoxal O 18 mm 20 C 4
5 Why glyoxal is special? No growth is observed for most carbonyls studied, even at high conc. (500 ppb to 5 ppm) At RH = 12%, no growth was observed at conc. as high as ~1 ppm of glyoxal Increase in particle volume was observed only when RH was higher than 40% No change in particle volume INCREASE in particle volume Liquid Water Content is Important! Kroll et al., JGR, ppb 2,4-hexadienal at t = 50 min 200 ppb glyoxal at t = 53 min 5
6 Knowledge Gap: SOA Model vs. Measurement Volkamer et al., GRL, 2006 Large Gap between modeled and measured SOA formation Current model parameterizations based on G/P thermodynamic partitioning of semi-volatile species of VOC oxidation underestimate OC aerosol concentrations as a function of photochemical age. 6
7 Available Literature for gas/particle glyoxal Matsunaga et al., Ortiz et al., Ortiz et al., Denuder XAD-7 XAD-4 coating + PFBHA + method BHA PFBHA Particle type PM4 PM2.5 TSP P, ng m G, ng m P/(P+G) 46% 80% 58% Flow rate 10 L/min 16.7 L/min 16.7 L/min Sampling Duration 3.5 hr 5.5 hr min 7
8 Experimental Methods
9 Annular Denuder-Filter Setup Quartz Filter Air Flow Denuder coated with sorbent KI-coated Denuder Cyclone XAD-7 Types of sorbents 1. XAD-4 2. XAD-4 + PFBHA 3. XAD-7 + OBE 4. PFBHA only XAD-4 9
10 The Use of Sulfite Coating Carbonyls + S(IV) Carbonyls S(IV) adduct Volatile Non-volatile Advantages Unlimited sulfite can be used for coating The reaction between sulfite and aldehydes is generally fast Carbonyl S(IV) adducts are non-volatile and therefore the effective sampling time is longer Disadvantages Removed by precipitation Not applicable for every carbonyl species The reaction between sulfite and ketone is generally much slower than aldehyde S(IV)-adduct formation 10
11 Extraction Procedures for Sulfite-Coated Denuder The denuder were extracted with DI water x 3 BaCl 2 is added into the sample extract The mixture is then centrifuged at RT for 30min Acidified PFBHA is added The extract was extracted x 3 with DCM Purged to near dryness under N 2 Reconstitution with Hexane and DCM Then 100 µl of BSTFA is added Baked at 60 C for an hour GC-MS analysis 11
12 Sulfite coated vs. XAD coated denuder This study XAD coated Sampling time Integrity of GC mass spectrum Coating and extraction Procedure Loading derivatizing reagent, mole 12 hours Clean Simple 0.24 Sulfite 5.5 hours Collection efficiency a ~85% ~ 60% Deteriorated Tedious PFBHA a Average collection efficiencies for glyoxal, methylglyoxal, glycoaldehyde, glyoxylic acid and pyruvic acid 12
13 Gas Chromatogram Glycoaldehyde Relative Abundance Hydroxyacetone Glyoxylic acid Pyruvic acid Glyoxal Methylglyoxal Time (min) Relative Abundance Glycoaldehyde Hydroxyacetone Glyoxylic acid Pyruvic acid Glyoxal Methylglyoxal Time (min) Figure 2. Total ion chromatogram (Top) and m/z = 181 ion chromatogram (bottom) of daytime denuder sample on 15 th January,
14 Sampling at Air Pollution Monitoring Site Important gas-phase species (CO, NO x, O 3, SO 2, etc.) and PM 10 - EPD PM 2.5 OC, EC Ionic species (SO 4 2-, NO 3-, Cl -, oxalate, Na +, NH 4+, K +, Ca 2+, Mg 2+, and other dicarboxylic acid) Sampling at Tsuen Wan Gas- and particle-phase carbonyl species 14
15 Results and Discussion
16 Gas/Particle Distribution in Hong Kong Maximum, minimum, average, and median of individual bifunctional carbonyl concentrations in the gas phase. Summer Gas phase (µg m -3 ) Winter Gas phase (µg m -3 ) Max. Min. Median Mean Max. Min. Median Mean Glycoaldehyde (MW: 60.05) Glyoxylic acid (MW: 74.04) Pyruvic acid (MW: 88.06) Glyoxal (MW: 58.04) Methylglyoxal (MW: 72.06) Maximum, minimum, average, and median of individual bifunctional carbonyl concentrations in the particle phase. Summer Particle phase (ng m -3 ) Winter Particle phase (ng m -3 ) Max. Min. Median Mean Max. Min. Median Mean Glycoaldehyde (MW: 60.05) 39.8 LOD Glyoxylic acid (MW: 74.04) Pyruvic acid (MW: 88.06) Glyoxal (MW: 58.04) Methylglyoxal (MW: 72.06)
17 Literature vs. Findings Matsunaga et al., Ortiz et al., Ortiz et al., This Study This Study Summer Winter Denuder XAD-7 XAD-4 Sulfite Sulfite coating + PFBHA method BHA PFBHA Glycerol Glycerol [Glyoxal] particle, ng m [Glyoxal] gas, ng m P/(P+G), % 46% 80% 58% 2.8% 3.4% Flow rate 10 L min L min L min -1 5 L min -1 5 L min -1 Sampling Duration 3.5 hr 5.5 hr min 12hr 12hr 17
18 Partition coefficient, K p Compounds Summer K p,i (n=17) (theoretical) Summer K p,i (n=17) (experimental) Winter K p,i (n=20) (theoretical) Winter K p,i (n=20) (experimental) Glyoxal (3.95±0.96)x10-10 (1.43±1.33)x10-3 (3.37±1.07)x10-10 (1.18±1.12)x10-3 Methylglyoxal (9.11±2.23)x10-10 (4.62±2.82)x10-4 (7.79±2.48)x10-10 (2.98±5.04)x10-3 Glycoaldehyde (5.33±1.30)x10-8 (6.48 ±5.74)x10-2 (4.56±1.45)x10-8 (2.30±3.47)x10-3 Glyoxylic Acid (5.83±1.42)x10-7 (1.63±1.33)x10-3 (4.98±1.59)x10-7 (1.82±2.19)x10-2 K K Pyruvic Acid (1.43±0.32)x10-7 (1.27±0.89)x10-2 (1.23±0.39)x10-7 (0.68±1.16)x10-2 C p, i (exp erimental = (Odum et al., 1996) C FSP p, i ) p, i ( theoretical) = MW g, i 760RTf om om 6 10 ζ p i L, i (Pankow, 1994a; Pankow, 1994b) 18
19 Experimental H eff of glyoxal Compounds Glyoxal Methylglyoxal Glycoaldehyde Glyoxylic Acid Pyruvic Acid a [Ip et al., 2009] b [Betterton and Hoffmann, 1998] c [Khan et al., 1995] Summer Effective K H in Wet Aerosols, M atm -1 (1.21 ± 1.36)x 10 9 (1.66 ± 1.42)x 10 8 (8.50 ± 7.90)x 10 7 (1.78± 1.30)x 10 8 (1.61 ± 1.30)x 10 9 Winter Effective K H in Wet Aerosols, M atm -1 (1.40 ± 0.85)x 10 9 (3.90 ± 8.86)x 10 8 (2.06 ± 2.89)x 10 8 (1.81 ± 1.72)x 10 9 (0.85 ± 1.21)x 10 9 Effective K H in Pure Water, M atm x 10 5a 3.7 x 10 3b 4.1 x 10 4b 1.1 x 10 4a 3.1 x 10 5c K H = FP ( 1 F) RT ( LWC) F = C p, i ( C p, i + Cg, i ) (Seinfeld and Pandis, 1998) where C g,i and C p,i are the concentrations of one species in gas phase and particle phase, respectively (µg m -3 ), R is the ideal gas constant ( m 3 Pa K -1 mol -1 ), P is the atmospheric pressure (Pa), T is the temperature (K) and LWC is aerosol liquid water content (µg m -3 ) calculated by AIM III. Experimental temperatures were used for calculations. 19
20 Summary CE prove that sulfite-coated denuder is capable of performing 12 hours Recovery studies prove that S(IV) precipitation by BaCl would not cause artifact Large gap between experimental K p and theoretical K P suggested that g/p partition theory cannot fully explain the partition pathways of glyoxal Estimated H eff from field study (1.12 x 10 9 M atm -1 ) are in agreement to H eff measured in acidic solution (>10 9 M atm -1, Ip et al., 2009). More studies are needed to investigate the effect of ionic strength, acidity and other major aerosol components on H eff of methylglyoxal, glyoxylic acid, pyruvic acid and glycoaldehyde, etc. 20
21 Acknowledgement Prof. Jianzhen YU Hilda Huang Dr. Eric Wan and Dr. Steven Ho ENVF Staffs Mr. To, Mr. Tsui, Ah Pong, Waiman, Ah Man Group Mates Elber Sit, Emily Au, Yu Huan, Li yun chun, Hu Di, Tony So, Wu Cheng, Huang xiao feng, Yuan zibing, Eric Xue, Lin Peng Thank you! Q & A 21
Gas Particle Partitioning to OA
Gas Particle Partitioning to OA Advanced Atmospheric chemistry CHEM 5152 Prof. J.L. Jimenez Last updated: Spring 2017 1 Gas Phase vs Aerosol Compounds For monofunctional compounds, alkanes beyond C 20
More informationGas/particle partitioning of water-soluble organic aerosol in Atlanta
Atmos. Chem. Phys., 9, 3613 3628, 09 www.atmos-chem-phys.net/9/3613/09/ Author(s) 09. This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Chemistry and Physics Gas/particle
More informationPolycyclic Aromatic. atmosphere of Guangzhou,
Size distributions of Polycyclic Aromatic Hydrocarbons in the urban atmosphere of Guangzhou, China Huan Yu and Jian Zhen Yu Dept of Chemistry Hong Kong University of Science and Technology yuhuan@ust.hkhk
More informationAqueous-Phase Chemistry in TM4-ECPL: SOA Formation via Cloud Processes Stelios Myriokefalitakis 1 Kostas Tsigaridis 2,3 Maria Kanakidou 1
TM meeting, Heraklion, June 2010 Aqueous-Phase Chemistry in TM4-ECPL: SOA Formation via Cloud Processes Stelios Myriokefalitakis 1 Kostas Tsigaridis 2,3 Maria Kanakidou 1 1 Environmental Chemical Processes
More informationAerosol Formation in the Cyclohexene-Ozone System
Environ. Sci. Technol. 2000, 34, 4894-4901 Aerosol Formation in the Cyclohexene-Ozone System M. KALBERER, J. YU, D. R. COCKER, R. C. FLAGAN, AND J. H. SEINFELD* Department of Chemical Engineering and Environmental
More informationThe Effect of Future Climate Change on Aerosols: Biogenic SOA and Inorganics
The Effect of Future Climate Change on Aerosols: Biogenic SOA and Inorganics GCAP Phase 2 Science Team Meeting October 12, 2007 Havala O. T. Pye 1, Hong Liao 2, John Seinfeld 1, Shiliang Wu 3, Loretta
More informationSecondary organic aerosol from low-volatility and traditional VOC precursors
Secondary organic aerosol from low-volatility and traditional VOC precursors Havala Olson Taylor Pye 1,2 and John H. Seinfeld 1 1 Department of Chemical Engineering, California Institute of Technology
More informationPutting Secondary Organic Aerosol in Global Models. Issues and Approaches
Putting Secondary Organic Aerosol in Global Models (and FRP s) Issues and Approaches Dean Hegg (University of Washington) Walter Sessions (NRL Monterey) Outline of Talk 1. The necessity of dealing with
More informationSupplement of Secondary formation of nitrated phenols: insights from observations during the Uintah Basin Winter Ozone Study (UBWOS) 2014
Supplement of Atmos. Chem. Phys., 16, 2139 2153, 2016 http://www.atmos-chem-phys.net/16/2139/2016/ doi:10.5194/acp-16-2139-2016-supplement Author(s) 2016. CC Attribution 3.0 License. Supplement of Secondary
More informationStable carbon isotope ratios of ambient secondary organic aerosols in Toronto
Atmos. Chem. Phys., 15, 1825 1838, 215 www.atmos-chem-phys.net/15/1825/215/ doi:1.5194/acp-15-1825-215 Author(s) 215. CC Attribution 3. License. Stable carbon isotope ratios of ambient secondary organic
More informationH SO2 EFFECT ON SECONDARY ORGANIC AEROSOL FORMATION: EXPERIMENTAL AND MODELLED RESULTS
H14-196 SO2 EFFECT ON SECONDARY ORGANIC AEROSOL FORMATION: EXPERIMENTAL AND MODELLED RESULTS Manuel Santiago 1, Marta G. Vivanco 1 and Ariel F. Stein 2 1 Unidad de Modelización y Ecotoxicidad de la Contaminación
More informationTropospheric OH chemistry
Tropospheric OH chemistry CO Oxidation mechanism: CO + OH CO 2 + H, H + O 2 + M HO 2 + M, HO 2 + NO OH + NO 2 NO 2 + hν (+O 2 ) NO + O 3 Initiation step Propagation Net: CO + 2 O 2 CO 2 + O 3 HO 2 + HO
More informationIncremental Aerosol Reactivity: Application to Aromatic and Biogenic Hydrocarbons
Environ. Sci. Technol. 1999, 33, 2403-2408 Incremental Aerosol Reactivity: Application to Aromatic and Biogenic Hydrocarbons ROBERT J. GRIFFI, DAVID R. COCKER III, AD JOH H. SEIFELD*, Department of Chemical
More informationFine Particles: Why We Care
Fine Particles: Why We Care Visibility/Radiative Forcing Health Effects A function of chemical composition PM2.5 Mostly 1) Sulfate 2) Carbonaceous - Organic - Elemental (Soot) 3) Metals, minerals, Metals,
More informationThe Atmospheric Chemistry and Physics of Ammonia
The Atmospheric Chemistry and Physics of Ammonia Russell Dickerson Dept. Meteorology, The University of Maryland Presented at the National Atmospheric Deposition Program Ammonia Workshop October 23, 2003
More informationChamber Studies of Secondary Organic Aerosol Growth by
90 Chapter 4 Chamber Studies of Secondary Organic Aerosol Growth by Reactive Uptake of Simple Carbonyls * * This chapter is reproduced by permission from Chamber studies of secondary organic aerosol growth
More informationSecondary Organic Aerosol Formation from Acetylene (C 2 H 2 ): seed effect on SOA yields due to organic photochemistry in the aerosol aqueous phase
Atmos. Chem. Phys., 9, 197 1928, 9 www.atmos-chem-phys.net/9/197/9/ Author(s) 9. This work is distributed under the Creative Commons Attribution 3. License. Atmospheric Chemistry and Physics Secondary
More informationDetermination of Total Volatile Organic Compounds in Indoor Air Using Agilent 7667A mini TD and 7820A GC
Determination of Total Volatile Organic Compounds in Indoor Air Using Agilent 77A mini TD and 70A GC Application Note Environmental Authors Tingting Bu, Xiaohua Li Agilent Technologies (Shanghai) Co.,
More informationModeling secondary organic aerosol formation from isoprene oxidation under dry and humid conditions
Atmos. Chem. Phys., 11, 893 909, 2011 doi:10.5194/acp-11-893-2011 Author(s) 2011. CC Attribution 3.0 License. Atmospheric Chemistry and Physics Modeling secondary organic aerosol formation from isoprene
More informationTHERMODYNAMIC MODELING OF ORGANIC AEROSOL
THERMODYNAMIC MODELING OF ORGANIC AEROSOL Thesis by Chinghang Tong In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy California Institute of Technology Pasadena, California
More informationMathematical Modelling of Partitioning Processes of Polycyclic Aromatic Hydrocarbons as Gas Waste
Mathematical Modelling of Partitioning Processes of Polycyclic Aromatic Hydrocarbons as Gas Waste Jelena Radonić a, Mirjana Vojinović Miloradov a, Maja Turk Sekulić a, Ivan Holoubek b and Maja Đogo a a
More informationSimultaneous study of gas phase and secondary organic aerosols chemical composition
Simultaneous study of gas phase and secondary organic aerosols chemical composition Stéphanie Rossignol, Laura Chiappini, Jean-François Doussin, Emilie Perraudin To cite this version: Stéphanie Rossignol,
More informationOxidation Chemistry and Evolving Volatility of Organic Aerosol
Oxidation Chemistry and Evolving Volatility of Organic Aerosol Neil M. Donahue Carnegie Mellon University Center for Atmospheric Particle Studies US - Nordic Workshop on Secondary Organic Aerosols 2 Jul
More informationCURRENT STATUS OF THE DEVELOPMENT AND EVALUATION OF AN UPDATED DETAILED MECHANISM FOR VOC OXIDATION
CURRENT STATUS OF THE DEVELOPMENT AND EVALUATION OF AN UPDATED DETAILED MECHANISM FOR VOC OXIDATION William P. L. Carter Statewide Air Pollution Research Center and College of Engineering, Center for Environmental
More informationDetermination of r- and β-hydroxycarbonyls and Dicarbonyls in Snow and Rain Samples by GC/FID and GC/MS Employing Benzyl Hydroxyl Oxime Derivatization
Anal. Chem. 2000, 72, 4742-4746 Determination of r- and β-hydroxycarbonyls and Dicarbonyls in Snow and Rain Samples by GC/FID and GC/MS Employing Benzyl Hydroxyl Oxime Derivatization Sou Matsunaga and
More informationImplementation and Testing of EQUISOLV II in the CMAQ Modeling System
Implementation and Testing of EQULV II in the CMAQ Modeling System Yang Zhang North Carolina State University Mark Z. Jacobson Stanford University, Stanford, CA CMAQ, September 26-29, 25 Acknowledgments
More informationCAPRAM MODELLING OF THE PHYSICO-CHEMICAL CLOUD PROCESSING OF TROPOSPHERIC AEROSOLS
CAPRAM MODELLING OF THE PHYSICO-CHEMICAL CLOUD PROCESSING OF TROPOSPHERIC AEROSOLS A. Tilgner 1 *, R. Wolke 1 and H. Herrmann 1 1 Leibniz-Institut für Troposphärenforschung, Permoserstr. 15, D-04318 Leipzig,
More informationGlyoxal processing by aerosol multiphase chemistry: towards a kinetic modeling framework of secondary organic aerosol formation in aqueous particles
doi:10.5194/acp-10-8219-2010 Author(s) 2010. CC Attribution 3.0 License. Atmospheric Chemistry and Physics Glyoxal processing by aerosol multiphase chemistry: towards a kinetic modeling framework of secondary
More informationUnit - 2 SOLUTIONS VSA QUESTIONS (1 - MARK QUESTIONS) 1. Give an example of liquid in solid type solution.
Unit - 2 SOLUTIONS VSA QUESTIONS (1 - MARK QUESTIONS) 1. Give an example of liquid in solid type solution. 2. Which type of solid solution will result by mixing two solid components with large difference
More informationLISA, UMR CNRS 7583, IPSL, Université Paris Est Créteil and Université Paris Diderot, Créteil Cedex, France. 2
Exploration of the influence of environmental conditions on secondary organic aerosol formation and organic species properties using explicit simulations: development of the VBS-GECKO parameterization
More informationPDXScholar. Portland State University. Negar Niakan Portland State University. Fall Recommended Citation
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses Fall 1-24-2013 Effects of Molecular Structure of the Oxidation Products of Reactive Atmospheric Hydrocarbons on the
More informationRICE UNIVERSITY. Computational Simulation of Secondary Organic Aerosol (SOA) Formation from Toluene Oxidation. Ying Liu
RICE UNIVERSITY Computational Simulation of Secondary Organic Aerosol (SOA) Formation from Toluene Oxidation by Ying Liu A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE Master
More informationEffect of aging on cloud nucleating properties of atmospheric aerosols
Effect of aging on cloud nucleating properties of atmospheric aerosols Yan Ma Nanjing University of Information Science & Technology The 1st Regional GEOS-Chem Asia Meeting 2015 年 5 月 8 日 Indirect effect
More informationPaul Ziemann Department of Chemistry & CIRES University of Colorado at Boulder
Gas- and Particle-Phase Products and their Mechanisms of Formation from the Reactions of Monoterpenes with N 3 Radicals: Comprehensive Measurements and Modeling Paul Ziemann Department of Chemistry & CIRES
More informationContinuous measurement of airborne particles and gases
Continuous measurement of airborne particles and gases Jeff Collett and Taehyoung Lee Atmospheric Science Department Colorado State University Funding: USDA/AES and NPS Outline Why measure particles and
More informationA MEASUREMENT TECHNIQUE FOR HYDROXYACETONE
A MEASUREMENT TECHNIQUE FOR HYDROXYACETONE P. J. Klotz, E. S. C. Kwok, X. Zhou, J. H. Lee, and Y. -N. Lee Environmental Chemistry Division, Department of Applied Science Brookhaven National Laboratory,
More informationAnalysis of gaseous I 2 in the marine boundary layer
Analysis of gaseous I 2 in the marine boundary layer Thorsten Hoffmann, Ru-Jin Huang, Michael Kundel, Christopher Kampf TORERO workshop, NCAR, October 31 th, 2011 23.01.2012 1 Outline I. Introduction II.
More information1) REACTIONs: a) Al4C3(s) + H2O (l)=> Al(OH)3 (s) + CH4 (g) Solution : Al4C3(s) + 12 H2O (l)=> 4Al(OH)3 (s) + 3CH4 (g)
1) REACTIONs: a) Al4C3(s) + H2O (l)=> Al(OH)3 (s) + CH4 (g) Balance the reaction. Describe the chemical process represented by this reaction. Write the name of each single reactant and product. First,
More informationAEROSOL-FORMING POTENTIAL OF ATMOSPHERIC ORGANIC COMPOUNDS
AEROSOL-FORMING POTENTIAL OF ATMOSPHERIC ORGANIC COMPOUNDS John H. Seinfeld 1, Prasad Pai 2, and David Allen 3 1 California Institute of Technology 2 AER, San Ramon, CA 94583 3 The University of Texas,
More informationSecondary Organic Aerosol Formation Mechanisms and Source Contributions in Europe
International Institute for Applied Systems Analysis Schlossplatz 1 A-2361 Laxenburg Austria Telephone: (+43 2236) 807 342 Fax: (+43 2236) 71313 E-mail: publications@iiasa.ac.at Internet: www.iiasa.ac.at
More informationMeasurement Techniques Formation of aqueous-phase α-hydroxyhydroperoxides (α-hhp): potential atmospheric impacts
Sciences ess doi:10.5194/acp-13-5857-2013 Author(s) 2013. CC Attribution 3.0 License. Atmospheric Chemistry and Physics Atmospheric Measurement Techniques Formation of aqueous-phase α-hydroxyhydroperoxides
More informationFlorian Couvidat 1, Marta G. Vivanco 2, and Bertrand Bessagnet 1
Simulating secondary organic aerosol from anthropogenic and biogenic precursors: comparison to outdoor chamber experiments, effect of oligomerization on SOA formation and reactive uptake of aldehydes Florian
More information1. Introduction. 2. Description of Model Approaches
GEOPHYSICAL RESEARCH LETTERS, VOL. 40, 978 982, doi:10.1002/grl.50203, 2013 Secondary organic aerosol formation from semi- and intermediatevolatility organic compounds and glyoxal: Relevance of O/C as
More informationSupplement for Understanding primary and secondary sources of. ambient carbonyl compounds in Beijing using the PMF model
1 2 3 4 5 6 7 8 9 Supplement for Understanding primary and secondary sources of ambient carbonyl compounds in Beijing using the PMF model W. T. Chen 1, M. Shao 1, S. H. Lu 1, M. Wang 1, L. M. Zeng 1, B.
More informationInteractive comment on Reactive uptake of ammonia to secondary organic aerosols: kinetics of organonitrogen formation by Y. Liu et al.
Atmos. Chem. Phys. Discuss., 15, C7412 C7424, 215 www.atmos-chem-phys-discuss.net/15/c7412/215/ Author(s) 215. This work is distributed under the Creative Commons Attribute 3. License. Atmospheric Chemistry
More informationChange of aerosol and precipitation in the mid troposphere over central Japan caused by Miyake volcano effluents
Change of aerosol and precipitation in the mid troposphere over central Japan caused by Miyake volcano effluents H. Ueda 1, M. Kajino 1 & H. Satsumabayashi 2 1 Disaster Prevention Research Institute, Kyoto
More information2B Technologies, Inc. An InDevR Company
2B Technologies, Inc. An InDevR Company Technical Note No. 40 UV-Absorbing Interferences in Ozone Monitors Date: 22 April 2015 Author: John Birks Background Ozone measurements by absorbance of the 253.7-nm
More informationDevelopment of a Sampling and Analysis Method for the Measurement of Hexavalent Chromium in Ambient Air
Development of a Sampling and Analysis Method for the Measurement of Hexavalent Chromium in Ambient Air Zhihua (Tina) Fan, Ph.D. Environmental and Occupational Health Sciences Institute UMDNJ and Rutgers
More informationRapid formation and evolution of an extreme haze episode in
Supplementary Information Rapid formation and evolution of an extreme haze episode in Northern China during winter 1 Yele Sun 1,*, Chen Chen 1,, Yingjie Zhang 1,, Weiqi Xu 1,3, Libo Zhou 1, Xueling Cheng
More informationName Section Number TA. 1. You may use crib sheets which you prepared in your own handwriting. This may be up to
1. You may use crib sheets which you prepared in your own handwriting. This may be up to five 8-1/2 by 11 inch sheets of paper with handwriting only on one side. This corresponds to one page each for Chapters
More informationDETERMINATION OF UPTAKE RATES FOR VOCs IN AMBIENT AIR BY USING AXIAL TYPE THERMAL DESORPTION PASSIVE TUBES
DETERMINATION OF UPTAKE RATES FOR VOCs IN AMBIENT AIR BY USING AXIAL TYPE THERMAL DESORPTION PASSIVE TUBES Mihriban Yılmaz Civan, Öznur Kuntasal and Gürdal Tuncel 1 1 OUTLINE Introduction Importance and
More informationMolality. Molality (m) is the number of moles of solute per kilogram of solvent. mol of solute kg solvent. Molality ( m) =
Molality Molality (m) is the number of moles of solute per kilogram of solvent. Molality ( m) = mol of solute kg solvent Sample Problem Calculate the molality of a solution of 13.5g of KF dissolved in
More informationJOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113, D10301, doi: /2007jd008726, 2008
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113,, doi:10.1029/2007jd008726, 2008 Box model studies of the secondary organic aerosol formation under different HC/NO x conditions using the subset of the Master
More informationKinetic Study of Esterification of Sulfuric Acid with Alcohols in Aerosol Bulk Phase. Supplementary Materials
Kinetic Study of Esterification of Sulfuric Acid with Alcohols in Aerosol Bulk Phase Jiaying Li and Myoseon Jang Department of Environmental Engineering Sciences P.O. Box 116450, University of Florida,
More informationApplication Note 116 Monitoring VOCs in Ambient Air Using Sorbent Tubes with Analysis by TD-GC/MS in Accordance with Chinese EPA Method HJ
Application Note Monitoring VOCs in Ambient Air Using Sorbent Tubes with Analysis by TD-GC/MS in Accordance with Chinese EPA Method HJ -3 Application Note Abstract This application note demonstrates the
More informationIMPROVE Sampling & Analysis: Evaluation & Development
IMPROVE Sampling & Analysis: Evaluation & Development Chuck McDade Crocker Nuclear Laboratory University of California, Davis Okefenokee, Georgia October 2008 AEROSOL GENERATION CHAMBER Selected Species
More information1. Glyoxal consists of 41.4% C, 3.5% H, and 55.1% O by mass. What is the empirical formula of glyoxal? (A) CHO (B) CH 2 O (C) CH 2 O 2 (D) C 12 HO 16
1 ACS Final Review **Questions are taken from actual past ACS USNCO exams. It is an overview of the topics that will be covered on the exam based on `materials covered. Please continue to study and review
More informationANALYTICAL METHOD DETERMINATION OF VOLATILE ALDEHYDES IN AMBIENT AIR Page 1 of 11 Air sampling and analysis
DETERMINATION OF VOLATILE ALDEHYDES IN AMBIENT AIR Page 1 of 11 Replaces: Dated: Author: Date: AM-No.: New New Nils Arne Jentoft 18.06.2014 0 CHANGES This procedure is new. 1 SCOPE This document describes
More informationDetermination of trace amounts of formaldehyde in acetone
analytica chimica acta 604 (2007) 134 138 available at www.sciencedirect.com journal homepage: www.elsevier.com/locate/aca Determination of trace amounts of formaldehyde in acetone X.H. Hilda Huang a,
More informationHeterogeneous Process Studies on the Formation of Secondary Aerosol
2016 BC workshop Heterogeneous Process Studies on the Formation of Secondary Aerosol Maofa Ge Institute of Chemistry Chinese Academy of Sciences June-27-2016 Aerosol Heterogeneous Chemistry Atmospheric
More informationChemistry. TOPIC : Solution and colligative properties
TOPIC : Solution and colligative properties Date : Marks : 20 mks Time : ½ hr. If 5.85 g of NaCl (molecular weight 58.5) is dissolved in water and the solution is made up to 0.5 litre, the molarity of
More informationA simplified description of the evolution of organic aerosol composition in the atmosphere
A simplified description of the evolution of organic aerosol composition in the atmosphere The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story
More informationSimulation and analysis of secondary organic aerosol dynamics in the South Coast Air Basin of California
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111,, doi:10.1029/2005jd006139, 2006 Simulation and analysis of secondary organic aerosol dynamics in the South Coast Air Basin of California Satish Vutukuru, 1 Robert
More informationReceived 23 April 2012; revised 11 September 2012; accepted 9 December 2012; published 30 January 2013.
JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES, VOL. 118, 507 519, doi:10.1029/2012jd017985, 2013 Relative contributions of secondary organic aerosol formation from toluene, xylenes, isoprene, and monoterpenes
More informationAEROSOL FORMATION FROM THE REACTION OF α-pinene AND OZONE USING A GAS PHASE KINETICS-PARTICLE PARTITIONING MODEL
AERSL FRMATIN FRM THE REACTIN F α-pinene AND ZNE USING A GAS PHASE KINETICS-PARTICLE PARTITINING MDEL R.M. Kamens, M. Jaoui, S. Lee, C.J.Chien Department of Environmental Sciences and Engineering, University
More informationSupplement of Modeling organic aerosol composition at the puy de Dôme mountain (France) for two contrasted air masses with the WRF-Chem model
Supplement of Atmos. Chem. Phys. Discuss., 1, 19 1, 01 http://www.atmos-chem-phys-discuss.net/1/19/01/ doi:10.19/acpd-1-19-01-supplement Author(s) 01. CC Attribution.0 License. Supplement of Modeling organic
More informationChapter 11 Review Packet
Chapter 11 Review Packet Name Multiple Choice Portion: 1. Which of the following terms is not a quantitative description of a solution? a. molarity b. molality c. mole fraction d. supersaturation 2. Which
More informationThermochemistry and Thermodynamics. What is the standard heat of formation of methane, H f CH 4 (g), as calculated from the data above?
Thermochemistry and Thermodynamics 38% 1. H 4 (g) + 2 O 2 (g) O 2 (g) + 2 H 2 O(l); = - 889.1 kj H f H 2 O(l) = - 285.8 kj / mole H f O 2 (g) = - 393.3 kj / mole What is the standard heat of formation
More informationSupplemental Material for Elemental Composition and Oxidation of Chamber Organic Aerosol
Supplemental Material for Elemental Composition and Oxidation of Chamber Organic Aerosol P. S. Chhabra 1,N.L.Ng 2, M. R. Canagaratna 2, A. L. Corrigan 3, L. M. Russell 3, D. R. Worsnop 2, R. C. Flagan
More informationAtmospheric Analysis Gases. Sampling and analysis of gaseous compounds
Atmospheric Analysis Gases Sampling and analysis of gaseous compounds Introduction - External environment (ambient air) ; global warming, acid rain, introduction of pollutants, etc - Internal environment
More informationc. K 2 CO 3 d. (NH 4 ) 2 SO 4 Answer c
Chem 130 Name Exam 2, Ch 4-6 July 7, 2016 100 Points Please follow the instructions for each section of the exam. Show your work on all mathematical problems. Provide answers with the correct units and
More information1 Introduction. PM 2.5 is reasonably well established and the sources
Atmos. Chem. Phys., 12, 8711 8726, 2012 doi:10.5194/acp-12-8711-2012 Author(s) 2012. CC Attribution 3.0 License. Atmospheric Chemistry and Physics The formation of SOA and chemical tracer compounds from
More informationSupporting Information for. Development of Solid Ceramic Dosimeter for the Time Integrative Passive. Sampling of Volatile Organic Compounds in Waters
1 2 3 4 Supporting Information for Development of Solid Ceramic Dosimeter for the Time Integrative Passive Sampling of Volatile Organic Compounds in Waters 5 6 Riza Gabriela Bonifacio 1, Go-Un Nam 1, In-Yong
More informationSulfuric Acid-Catalyzed Conversion of Alkynes to Ketones in an Ionic Liquid Medium under Mild Reaction Conditions
Sulfuric Acid-Catalyzed Conversion of Alkynes to Ketones in an Ionic Liquid Medium under Mild Reaction Conditions Wing-Leung Wong, Kam-Piu Ho, Lawrence Yoon Suk Lee, Kin-Ming Lam, Zhong-Yuan Zhou, Tak
More informationInfluence of Organic-Containing Aerosols on Marine Boundary Layer Processes
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Influence of Organic-Containing Aerosols on Marine Boundary Layer Processes John H. Seinfeld California Institute of Technology,
More informationSolution KEY CONCEPTS
Solution KEY CONCEPTS Solution is the homogeneous mixture of two or more substances in which the components are uniformly distributed into each other. The substances which make the solution are called
More informationLab 4 Major Anions In Atmospheric Aerosol Particles
Georgia Institute of Technology School of Earth and Atmospheric Sciences EAS 4641 Spring 2008 Lab 4 Major Anions In Atmospheric Aerosol Particles Purpose of Lab 4: This experiment will involve determining
More informationAerosol modeling with WRF/Chem
Aerosol modeling with WRF/Chem Jan Kazil University of Colorado / NOAA Earth System Research Laboratory WRF/Chem Tutorial, 3 August 2015 (WRF/Chem 3.7) Part I - Introduction Overview of... Aerosol Aerosol
More informationDownloaded from
: Bhubaneswar Region CHAPTER 2-SOLUTIONS 1 MARK QUESTIONS 1 What is molarity? 2 What do you understand by saying that molality of a solution is 0.2? 3 Why is the vapour pressure of a liquid remains constant
More information8.2 Tropospheric ozone
8.2 Tropospheric ozone Prev Chapter 8. Ozone Next 8.2 Tropospheric ozone Tropospheric ozone is only about 10% of the total amount of ozone contained in a vertical column in the atmosphere. However, this
More informationFormation, Speciation, and Chemical Processing of Atmospheric Particulate Matter Kara E. Huff Hartz
Formation, Speciation, and Chemical Processing of Atmospheric Particulate Matter Kara E. Huff Hartz Department of Chemistry and Biochemistry Southern Illinois University Carbondale Carbondale, IL USA khuffhartz@chem.siu.edu
More informationSurface Ozone Problem in Two Polluted Regions in China and VOGA-NCP 2013 Summer Campaign
Surface Ozone Problem in Two Polluted Regions in China and VOGA-NCP 2013 Summer Campaign Liang Ran Key Laboratory of Middle Atmosphere and Global Environment Observation (LAGEO) Institute of Atmospheric
More informationCharacterization of Volatilization of Filter-Sampled PM 2.5 Semi-Volatile Inorganic Ions Using a Backup Filter and Denuders
Aerosol and Air Quality Research, 15: 814820, 2015 Copyright Taiwan Association for Aerosol Research ISSN: 1680-8584 print / 2071-1409 online doi: 10.4209/aaqr.2014.09.0213 Characterization of Volatilization
More informationSOA formation from the atmospheric oxidation of 2-methyl-3-buten-2-ol and its implications for PM 2.5
doi:10.5194/acp-12-2173-2012 Author(s) 2012. CC Attribution 3.0 License. Atmospheric Chemistry and Physics SOA formation from the atmospheric oxidation of 2-methyl-3-buten-2-ol and its implications for
More informationSupplement of Temporal variability and sources of VOCs in urban areas of the eastern Mediterranean
Supplement of Atmos. Chem. Phys., 1, 1 1, 1 http://www.atmos-chem-phys.net/1/1/1/ doi:1.19/acp-1-1-1-supplement Author(s) 1. CC Attribution. License. Supplement of Temporal variability and sources of VOCs
More information2,4-Toluene Diisocyanate Detection in Liquid and Gas Environments Through. Electrochemical Oxidation in an Ionic Liquid
Electronic Supplementary Material (ESI) for Analyst. This journal is The Royal Society of Chemistry 216 2,4-Toluene Diisocyanate Detection in Liquid and Gas Environments Through Electrochemical Oxidation
More informationP T = P A + P B + P C..P i Boyle's Law The volume of a given quantity of gas varies inversely with the pressure of the gas, at a constant temperature.
CHEM/TOX 336 Winter 2004 Lecture 2 Review Atmospheric Chemistry Gas Chemistry Review The Gaseous State: our atmosphere consists of gases Confined only by gravity force of gas on a unit area is due to the
More informationStructure-activity relationships for the development of MCM/GECKOA mechanisms
Atmospheric Chemical Mechanisms, Davis, December 2018 Structure-activity relationships for the development of MCM/GECKOA mechanisms Acknowledgement: Bernard Aumont Richard Valorso, Marie Camredon LISA
More informationChapter 5 Conclusions and Future Studies
177 Chapter 5 Conclusions and Future Studies 178 Conclusions and Future Studies The results of the studies presented in this thesis confirm that ambient and laboratory-generated aerosols exhibit complex
More informationWP3: In-situ chemical, physical and optical properties of aerosols. WP4: Trace gases networking: Volatile organic carbon and nitrogen oxides
WP3: In-situ chemical, physical and optical properties of aerosols WP4: Trace gases networking: Volatile organic carbon and nitrogen oxides WP3: In-situ chemical, physical and optical properties of aerosols
More informationChapter Four: Laboratory Characterisation of the Aerodyne Aerosol Mass Spectrometer
24 PhD Thesis 79 Chapter Four: Laboratory Characterisation of the Aerodyne Aerosol Mass Spectrometer Laboratory characterisation of the Aerodyne aerosol mass spectrometer has been an important part of
More informationFall 2011 CHEM Test 4, Form A
Fall 2011 CHEM 1110.40413 Test 4, Form A Part I. Multiple Choice: Clearly circle the best answer. (60 pts) Name: 1. The common constituent in all acid solutions is A) H 2 SO 4 B) H 2 C) H + D) OH 2. Which
More informationSecondary Organic Aerosol Formation from m-xylene,
241 Chapter 8 Secondary Organic Aerosol Formation from m-xylene, Toluene, and Benzene * * This chapter is reproduced by permission from Secondary organic aerosol formation from m-xylene, toluene, and benzene
More informationOnline Quantification of Gaseous Amines using the HR-ToF-AMS and artificially generated Particles
Online Quantification of Gaseous Amines using the HR-ToF-AMS and artificially generated Particles Moritz J. D. Mann, Michael Kundel, Anne-Kathrin Bernhammer and Thorsten Hoffmann Institute of Inorganic
More information2.444 A FEASIBILTY STUDY OF THE MARGA TOOL AS AN AEROSOL ANALYZER
2.444 A FEASIBILTY STUDY OF THE MARGA TOOL AS AN AEROSOL ANALYZER Rufus Ty White ac, Dr. Vernon Morris abc Department of Chemistry a, Program in Atmospheric Science b, NOAA Center for Atmospheric Science
More informationTM4-ECPL modeling activities
TM-meeting, 30-31 May 2011, ISPRA TM4-ECPL modeling activities Stelios Myriokefalitakis, Nikos Daskalakis, Kanakidou Maria Environmental Chemical Process Laboratory (ECPL), Department of Chemistry, University
More informationUnit 10: Solutions. soluble: will dissolve in miscible: refers to two liquids that mix evenly in all proportions -- e.g., food coloring and water
Unit 10: Solutions Name: Solution Definitions solution: a homogeneous mixture -- -- e.g., alloy: a solid solution of metals -- e.g., solvent: the substance that dissolves the solute soluble: will dissolve
More informationComparing Modal and Sectional Approaches in Modeling Particulate Matter in Northern California
Comparing Modal and Sectional Approaches in Modeling Particulate Matter in Northern California K. Max Zhang* [1], Jinyou Liang [2], Anthony S. Wexler [1], and Ajith Kaduwela [1,2] 1. University of California,
More informationSupporting Information
Supporting Information An L-proline Functionalized Metallo-organic Triangle as Size-Selective Homogeneous Catalyst for Asymmertry Catalyzing Aldol Reactions Xiao Wu, Cheng He, Xiang Wu, Siyi Qu and Chunying
More informationI. (40 points) A. (11 points) 1. Write the ions present in solution after Ba(OH) 2 reacts completely with nitric acid
I. (40 points) A. (11 points) 1. Write the ions present in solution after Ba(OH) 2 reacts completely with nitric acid 2. Write balanced net ionic equations for the reactions between aqueous solutions of
More information