Characterization of dimers of soot and non-soot

Similar documents
ACTRIS Workshop on the Reference method for Multi-Wavelength Absorption

Single particle characterization using SP-AMS with light scattering module in urban environments

Physical and chemical properties of freshly emitted and aged particles determined from mobile measurements in the Po Valley

Supplement of The influence of photochemical aging on light absorption of atmospheric black carbon and aerosol single-scattering albedo

Chamber Studies of Diesel Aerosol

Choosing the proper technique for measuring the particle light absorption

AMS Introduction Doug Worsnop. AMS Users Meeting

AMS CE for Chamber SOA

Optical, physical, and chemical characterization of marine Black Carbon

Analysis of Data from the 2009 SOOT Experiment

SootParticle-AMS or LaserVaporizer-AMS. Aerodyne Research, Inc. et al.

Sensitivity of the Single Particle Soot Photometer to different black carbon types

Collection Efficiency: A summary of what we know so far.

Preliminary testing of new approaches to retrieve aerosol properties from joint photometer-lidar inversion

B C, a byproduct of combustion, has a unique role as a climate forcing agent. It absorbs the most solar light per

SootParticle-AMS. LaserVaporizer-AMS. Aerodyne Research, Inc. et al.

Comparison of AERONET inverted size distributions to measured distributions from the Aerodyne Aerosol Mass Spectrometer

Optical properties of atmospheric constituents

Coatings and their enhancement of black carbon light absorption in the tropical atmosphere

Effect of aging on cloud nucleating properties of atmospheric aerosols

Supplementary Table 1. Geometry and flow rate of the individual components of the aerosol sampling system used in the A-FORCE 2013W campaign.

Supplement of Quantification of black carbon mixing state from traffic: implications for aerosol optical properties

Helsinki, Finland. 1 Aerodyne Research Inc., Billerica, MA, USA. 2 Chemistry Department, Boston College, Chestnut Hill, MA, USA

SATELLITE AEROSOL COMPOSITION RETRIEVAL

Aerosol Optical Properties

Aerosols and climate. Rob Wood, Atmospheric Sciences

Lecture 26. Regional radiative effects due to anthropogenic aerosols. Part 2. Haze and visibility.

Supplementary information

ATOC 3500/CHEM 3152 Week 9, March 8, 2016

This is a repository copy of Black-carbon absorption enhancement in the atmosphere determined by particle mixing state.

Modeling of Mature Soot Dynamics and Optical Properties

Soot Particle Aerosol Mass Spectrometer: Development, Validation, and Initial Application

Effect of Fuel to Oxygen Ratio on Physical and Chemical Properties of Soot Particles

Chapter 5 Conclusions and Future Studies

Aerosol Composition and Radiative Properties

Investigation of Optical Properties of Size-Selected Black Carbon Under Controlled Laboratory Conditions. Thesis

Aerosol Effects on Water and Ice Clouds

Experimental Investigation of the Collection Efficiencies of the AMS Aerodynamic Focusing Lens

Benjamin A. Nault, Pedro Campuzano-Jost, Doug A. Day, Hongyu Guo, Jason C. Schroder, Jose L. Jimenez, and the Science Teams from KORUS-AQ and ATom

Single Particle Soot Photometer intercomparison at the AIDA chamber

Supplement of Evaluation of the performance of a particle concentrator for online instrumentation

UKCA_RADAER Aerosol-radiation interactions

Comparison Among DMS 500, EEPS SMPS, MSS, EC/OC, CPMA, Using Laboratory Soot Particles

7. Aerosols and Climate

An Investigation on Secondary Organic Aerosol Induced Restructuring in Soot Aggregates. Kaiser K Leung

Physio-chemical and Optical Characterization of Anthropogenic and Natural Aerosol: Implications for Assessing Global Effects

TNA User Report The completed and signed form below should be returned by to pec.fr

Optical properties of absorbing and non-absorbing aerosols retrieved by cavity ring down (CRD) spectroscopy

Top-of-atmosphere radiative forcing affected by brown carbon in the upper troposphere

Indices of Refraction of Absorptive Aerosol Their Importance and Complexity

Light scattering and absorption by fractal-like carbonaceous chain aggregates: comparison of theories and experiment

CHAPTER 8. AEROSOLS 8.1 SOURCES AND SINKS OF AEROSOLS

Rapid Measurements of Aerosol Size Distributions Using a Fast Integrated Mobility Spectrometer (FIMS)

The Pennsylvania State University. The Graduate School. Department of Chemistry MORPHOLOGY AND OPTICAL PROPERTIES OF AEROSOL PARTICLES

Three-dimensional (3-D) radiative transfer codes are mainly used in cloud studies (e.g., LES models) and vegetation studies.

Diesel soot aging in urban plumes within hours under cold dark and humid conditions

Jianfei Peng et al. Correspondence to: Jianfei Peng Min Hu and Renyi Zhang

Observation of Smoke and Dust Plume Transport and Impact on the Air Quality Remote Sensing in New York City

Measurements of submicron aerosols in Houston, Texas during the 2009 SHARP field campaign

Direct radiative forcing due to aerosols in Asia during March 2002

Atmospheric ice nuclei concentrations and characteristics constraining the role of biological ice nuclei

Influence of Organic-Containing Aerosols on Marine Boundary Layer Processes

Introduction Methodology Some early results Conclusion Questions. Production-tagged aerosols in NorESM

Particle scattering, backscattering, and absorption coefficients: An in situ closure and sensitivity study

Hygroscopic Growth of Aerosols and their Optical Properties

11/24/2003. Size-Distributions and Mixtures of Dust and Black Carbon Aerosol in Asian Outflow: Physio-chemistry and Optical Properties

SOP SMPS BaltimorePM supersite Version /29/01 Page 1 of 13 SMPS

Ocean Optics XIV Conference, Kona, Hawaii 1998

BC properties and its measurement techniques

Collection efficiency of the soot-particle aerosol mass spectrometer (SP-AMS) for internally mixed particulate black carbon

Spatial Variability of Aerosol - Cloud Interactions over Indo - Gangetic Basin (IGB)

Multiple scattering of light by water cloud droplets with external and internal mixing of black carbon aerosols

Evolution of mixing state of black carbon in polluted air from Tokyo

Supporting Material for Preparation of colloidal organosilica spheres through spontaneous emulsification

Introduction to Dynamic Light Scattering for Particle Size Determination

OPTIMAL WAVELENGTH SELECTION ALGORITHM OF NON-SPHERICAL PARTICLE SIZE DISTRIBUTION BASED ON THE LIGHT EXTINCTION DATA

Outline. December 14, Applications Scattering. Chemical components. Forward model Radiometry Data retrieval. Applications in remote sensing

Why is the sky blue?

Supplementary information

Standardization of Optical Particle Counters

PSAP corrections. Observations Based Research. OBR Technical Note No th August Kate Turnbull. Amendment to MRF Technical Note No.

Supporting Information

Satellite remote sensing of aerosols & clouds: An introduction

Design and Application of a Pulsed Cavity Ring- Down Aerosol Extinction Spectrometer for Field Measurements

How good are our models?

PMP Meeting. May 16th Presented on behalf of PEMS4NANO by Les Hill HORIBA Europe May

Slides partly by Antti Lauri and Hannele Korhonen. Liquid or solid particles suspended in a carrier gas Described by their

Review of the IMPROVE Equation for Estimating Ambient Light Extinction

Projects in the Remote Sensing of Aerosols with focus on Air Quality

Conceptual models of ultrafine particles from combustion sources Benefits from integrating studies of ultrafine particles with nanotoxicology

Can a change of single scattering albedo in Amami-Oshima in a low pressure condition be explained by GCM simulations?

Development, Characterization, and Application of a Light Scattering Module within the Aerodyne AMS

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, NO. D15, 4248, /2001JD001110, 2002

4 th AMS Users Meeting Brainstorming on (1) Experiments to Nail our Absolute Quantification (2) Best Operating Procedures

What are Aerosols? Suspension of very small solid particles or liquid droplets Radii typically in the range of 10nm to

Aerosol Dynamics. Antti Lauri NetFAM Summer School Zelenogorsk, 9 July 2008

The AMS as a Single Particle Mass Spectrometer

Imholt 1. Optical properties of secondary organic aerosols using ultraviolet/visible spectroscopy. Felisha Imholt

THESIS THE ROLE OF AEROSOLS IN VISIBILITY DEGRADATION DURING TWO FIELD CAMPAIGNS. Submitted by. Ezra J.T. Levin. Department of Atmospheric Science

Accounting for the effects of nonideal minor structures on the optical properties of black carbon aerosols

Transcription:

Characterization of dimers of soot and non-soot particles formed by charged coagulation Boston College and Aerodyne Leonid Nichman, Paola Massoli, Yue Zhang, Tim Onasch, Doug Worsnop, Paul Davidovits MTU Janarjan Bhandari, Claudio Mazzoleni 6/26/2018 Cambridge particle meeting 2018

Here Soot = Black Carbon (BC) Focus of experiments in our lab 1. Ice nucleation on BC particles under cirrus cloud conditions 2. Optical properties (i.e., absorption) of BC containing particles Internal and external mixtures of BC containing particles Bond et al., 2013 6/26/2018 Cambridge particle meeting 2018 2

Absorption enhancement (lensing) Lack et al., 2009 light soot coating Dioctyl sebecate (DOS) coated absorbing PSL particles well characterized by core-shell Mie theory Non-soot material on soot particles increase optical cross sections 6/26/2018 Cambridge particle meeting 2018 3

Discrepancy between ambient/source and core-shell results Ambient vs Laboratory Biomass burning source Cappa et al., 2012 McMeeking et al., 2014 Gap between well-characterized laboratory and field (ambient and biomass burning) measurements, either due to particle variability or population mixing 6/26/2018 Cambridge particle meeting 2018 4

Particle morphology versus population mixing Core-Shell structure has an increased optical cross section which enhances the absorption of light Core-shell is the most common representation in models Liu et al., 2015 - Mich. Tech. Univ. Other types of internal and external mixtures are prevalent in the atmosphere What are the relative effects of morphology versus population mixing? 6/26/2018 Cambridge particle meeting 2018 5

Objective study coagulated BC particle types Refractive Org dimer Engulfed soot Core shell Bare soot, thinly coated and thickly coated were extensively studied in previous campaigns Compact soot agglomerate Data is scarce for the dimer structure of coagulated particles (complex experiments) 6/26/2018 Cambridge particle meeting 2018 6

Characteristic times of bipolar coagulation Known challenges 1. Coagulation slow process 2. Low number concentrations of dimers generated, near detection limit of optical measurements Kim et al. 2005 For mono >1*10 5 cm -3 Petters & Rothfuss (2016) 6/26/2018 Cambridge particle meeting 2018 7

Charge-enhanced coagulation Process steps 1. Generation of two polydispersed particle distributions 2. Size select monodisperse particle distributions with opposite charges 3. Neutralization of the charge by Coagulation 4. Removal of all remaining charged particles i.e. separation of the dimer 5. Recharging the neutral particles to detect the neutral dimer with a CPMA (Centrifugal Particle Mass Analyser, Cambustion Ltd.) 6. Measuring optical properties of dimer particles! 6/26/2018 Cambridge particle meeting 2018 8

Experimental setup (1) Finding dimer mass (2) Measuring optical properties Non-soot particle generation (DiOctyl Sebacate) 6/26/2018 Cambridge particle meeting 2018 9

Experimental plan DOS-DOS (liquid-liquid) experiments Optimize experiments Assess methodologies DOS-Soot experiments over Region of Interest in NR-PM/BC ratio and E abs space Study more interesting mixtures, including ammonium sulfate-soot and secondary organic aerosol (SOA)-soot 6/26/2018 Cambridge particle meeting 2018 10

dn/dlogm p (cm -3 ) Identification of mass-distribution peaks (re-neutralized positive monodispersed particles) Mixing time DOS-DOS 0 min 11 min 3.5 h C dimer C monomer 0.05 % 2.6 % 3 % (for identical conditions) DOS-DOS Soot-DOS Soot-A.S C dimer C monomer 4 % 6 % 3.5% Monodispersed D m (Mass scan) Recharging Mass (fg) Monodispersed mobility diameter (Mass scan) m1/(q=1)=1 m2/(q=2)=1.7 m3/(q=3) 2.6 6/26/2018 Cambridge particle meeting 2018 11

DOS-DOS liquid coalescence optimized conditions (-) particles (+) particles (0) neutral coagulated Clear confirmation of coalescence of two particles at higher mass (grey) Preliminary experiments show a clear peak for coalesced negatively charged 0.9 fg DOS with positively charged 1.2 fg DOS particles at a mass of 2.15 fg 6/26/2018 Cambridge particle meeting 2018 12

Concentration [# cm -3 ] Soot-DOS coagulation 100 2.19, 51.79 2.00, 32.03 2.52, 56.97 4.42, 43.44 Clear coagulated (doubled) neutral mass observed! Negative neutral DOS 2.5fg 10 Positive neutral Soot 2fg coag DOS+Soot 1 0.1 1 10 M p [fg] 6/26/2018 Cambridge particle meeting 2018 13

Optical detection (DOS-Soot) using CAPS PMssa Soot 2.4fg Absorption Mass (Incadescence) SSA DOS ~1.9fg Soot-DOS 1:1 (Soot 2.6fg) CAPS zero During baseline measurements, CAPS signal is zero 20% Absorption enhancement (Eabs) was calculated for the dimer Single Scattering Albedo is higher than for pure soot and lower than for pure DOS 6/26/2018 Cambridge particle meeting 2018 14

Preliminary results SSA of coagulated dimers are similar ot higher than pure soot particles, as expected MAC of coagulated dimers and pure soot particles are similar but in some cases are higher, which was unexpected Most data follow Mie theory with some exceptions Observation: DOS likely wetting soot particles on experimental time-frame 6/26/2018 Cambridge particle meeting 2018 15

Summary Rarely studied coagulation of monomers was achieved and reproduced in a laboratory setup The process was optimized to allow shorter coagulation time Several types of monomers were coagulated (DOS-DOS, Soot-DOS, Soot- A.S, Soot-A.N, Soot-SOA) The process was optimized to allow optical detection (CAPS-PMssa, SP2) Preliminary results of Eabs, MAC and SSA for uniform distribution of Soot-DOS dimers are reported 6/26/2018 Cambridge particle meeting 2018 16

Future work Higher Rbc ratios viscous aerosols (e.g. SOA) to reduce core shell structures Include coagulated dimers into population mixing studies Study humidity influence on coagulation efficiency 6/26/2018 Cambridge particle meeting 2018 17

Acknowledgements Questions? 2017-2018 JakeMathews This work is supported by DOE award #DE-SC0011935, NSF award #1506768, the Boston College Undergraduate Research fund and the Boston College Postdoctoral Association Knowledge Dissemination Program 6/26/2018 Cambridge particle meeting 2018 18

6/26/2018 Cambridge particle meeting 2018 19 bc.edu/aerosol

Extra Slides 6/26/2018 Cambridge particle meeting 2018 20

Inverted Burner Soot Generator Argonaut Scientific Corporation 11119 50th Ave, Edmonton, Alberta, Canada 6/26/2018 Cambridge particle meeting 2018 21

Soot Photometer (SP2) Organics scatter light, black carbon incandesce Determination of soot core mass for coated particles by temporal separation between scattering and incandescence signals Onasch et al., 2012 6/26/2018 Cambridge particle meeting 2018 22

CAPS PM ssa Monitor Scattering and Extinction Extinction Cavity Attenuated Phase Shift Technique Scattering Inverse Integrating Nephelometer Integrating Sphere with Lambertian Surface Minimal Bias w.r.t. Scattering Angle PMT Aerosol Sci. and Technol. 49:267-272 (2015)

Ammonium sulphate + soot dimers SEM sample collection dimers 6/26/2018 Cambridge particle meeting 2018 24

Dioctyl sebacate oil 6/26/2018 Cambridge particle meeting 2018 25