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Richard J. Tropp Judith C. Chow John G. Watson Desert Research Institute, Reno, NV Presented at: EPA’s National Ambient Air Monitoring Conference Atlanta, GA August 11-14, 2014 Improved Optical and Chemical Characterization Methods for PM 2.5 Source Apportionment

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Richard J. Tropp

Judith C. Chow

John G. Watson

Desert Research Institute, Reno, NV

Presented at:

EPA’s National Ambient Air Monitoring Conference

Atlanta, GA

August 11-14, 2014

Improved Optical and Chemical

Characterization Methods for PM2.5

Source Apportionment

Objectives

• Review common chemical analyses for

PM2.5/PM10 networks

• Give overview of characterization methods for

more specific source markers

• Give examples of source markers to better

validate source apportionment results

• Goal is to provide additional information at

minimal additional cost

Major PM components are commonly characterized, but

more specific markers are needed

• Organic Carbon

• Elemental Carbon

• Nitrate

• Sulfate

• Ammonium

• Geological Material

• Sea Salt

• Liquid Water

• Other

U.S. EPA Staff Paper (2005)

PM0.1 (ultrafine PM) PM2.5 (fine PM) PM10-2.5 (coarse PM)

Los Angeles Supersite

Chemical composition differs by PM size fraction

U.S. long-term chemical speciation networks obtain filter

samples for PM2.5 mass, elements, ions, and carbon

IMPROVE (2014). Interagency Monitoring of Protected Visual Environments. prepared by National Park Service, Ft. Collins, CO,

http://vista.cira.colostate.edu/IMPROVE.

U.S.EPA (2014). Chemical speciation. prepared by U.S. Environmental Protection Agency, Research Triangle Park, NC,

http://www.epa.gov/ttn/amtic/speciepg.html.

Interagency Monitoring of PROtected Visual

Environments (IMPROVE) NetworkChemical Speciation Network (CSN)

URG

MASSAndersen

RAAS

MetOne

SASS

URG

3000N

R&P

Partisol

IMPROVE

Current speciation networks use up to three filter

channels for mass, elements, ions, and carbon fractions

Size-selective Inlet Size-selective Inlet Size-selective Inlet

HNO3 Denuder

Teflon-membrane filter

GRAV for mass

XRF for elements

Nylon-membrane filter

IC, AC, and AAS for

water-soluble ions

Quartz-fiber filter

TOR/TOT for OC, EC,

carbon fractions, and

carbonate

Quartz-fiber backup filter

Assess OC adsorption

artifact

Methods: AAS: Atomic absorption spectrophotometry

AC: Automated colorimetry

GRAV: Gravimetry (filter weighing)

IC: Ion chromatography with conductivity

detector

TOR/TOT: Thermal-optical reflectance and

transmittance

XRF: X-ray fluorescence

Size-selective Inlet Size-selective Inlet Size-selective Inlet

HNO3 Denuder

Teflon-membrane filter

GRAV for mass

XRF for elements

Nylon-membrane filter

IC, AC, and AAS for

water-soluble ions

Quartz-fiber filter

TOR/TOT for OC, EC,

carbon fractions, and

carbonate

Quartz-fiber backup filter

Assess OC adsorption

artifact

Methods: AAS: Atomic absorption spectrophotometry

AC: Automated colorimetry

GRAV: Gravimetry (filter weighing)

IC: Ion chromatography with conductivity

detector

TOR/TOT: Thermal-optical reflectance and

transmittance

XRF: X-ray fluorescence

Size-selective Inlet Size-selective Inlet Size-selective Inlet

HNO3 Denuder

Teflon-membrane filter

GRAV for mass

XRF for elements

Nylon-membrane filter

IC, AC, and AAS for

water-soluble ions

Quartz-fiber filter

TOR/TOT for OC, EC,

carbon fractions, and

carbonate

Quartz-fiber backup filter

Assess OC adsorption

artifact

Methods: AAS: Atomic absorption spectrophotometry

AC: Automated colorimetry

GRAV: Gravimetry (filter weighing)

IC: Ion chromatography with conductivity

detector

TOR/TOT: Thermal-optical reflectance and

transmittance

XRF: X-ray fluorescence

Size-selective Inlet Size-selective Inlet Size-selective Inlet

HNO3 Denuder

Teflon-membrane filter

GRAV for mass

XRF for elements

Nylon-membrane filter

IC, AC, and AAS for

water-soluble ions

Quartz-fiber filter

TOR/TOT for OC, EC,

carbon fractions, and

carbonate

Quartz-fiber backup filter

Assess OC adsorption

artifact

Methods: AAS: Atomic absorption spectrophotometry

AC: Automated colorimetry

GRAV: Gravimetry (filter weighing)

IC: Ion chromatography with conductivity

detector

TOR/TOT: Thermal-optical reflectance and

transmittance

XRF: X-ray fluorescence

Most source profiles report similar measurements of elements,

ions, and carbon, but these are insufficient for separating many

sources from each other

Watson and Chow (2007) 279–316

Organic components

help with modern

source apportionment,

but source and receptor

measurements are

limited

Watson et al., 2008, JAWMA

Additional speciation can be applied to obtain marker

compounds as part of the original analyses or on archived

filters

Size-selective Inlet Size-selective Inlet Size-selective inlet

HNO3 denuder VOC denuder

Teflon-membrane filter

GRAV for mass

XRF for elements

FTIR for organic functional groups

UV-VIS for light transmittance/ reflectance

ICP-MS for rare-earth elements and isotopes (acid extract)

Quartz-fiber filter

TOR/TOT for OC, EC, carbon fractions, and carbonate

TGA for volatile mass, moisture, fixed carbon, and ash

TD-GC/MS or non-polar compounds

D-TD-GC/MS for polar (oxygenated) compounds

Quartz-fiber filter (water extract)

IC, AC, and AAS for anions and cations

TOC for total Water Soluble Organic Carbon (WSOC)

HPLC-TOC for neutral and basic WSOC classes

HPLC-SEC-ELSD-UV-VIS for humic-like substances (HULIS)

IC-PAD for sugars and sterols

IC-ECD for organic acids

Impregnated cellulose-fiber filters

(water extract)

NH3 as NH4+ by IC

SO2 as SO4= by IC

NO2 as NO2- by IC

Impregnated cellulose-fiber filter

(water extract)

HNO3 as NO3- by IC

Quartz-fiber filter

TOR/TOT for OC artifact assessment

Methods: AAS: Atomic absorption

spectrophotometry AC: Automated colorimetry D-TD-GC/MS: Derivitized-thermal

desorption-gas chromatography/mass spectrometry

FTIR: Fourier Transform Infrared spectroscopy

GRAV: Gravimetry (filter weighing) HPLC-SEC-ELSD-UV-Vis: HPLC-

size-exclusion chromatography-evaporative light scattering detector-ultraviolet-visible light spectrometry

IC: Ion chromatography with conductivity detector

IC-ECD: IC-electrochemical detection

IC-PAD: IC with pulsed amperometric detection

ICP-MS: Inductively coupled plasma-MS

TD-GC/MS: Thermal desorption-gas chromatography/MS

TGA: Thermogravimetric analysis TOC: Total organic carbon analysis TOR/TOT: Thermal-optical

reflectance and transmittance UV-Vis: Ultraviolet-visible light

spectrometry (λ=250–1100 nm) XRF: X-ray fluorescence

Biomass

burningDust

Acetylene

soot

Diesel

soot

PALAS arc

generator soot

More information can be obtained from Teflon-

membrane filters than mass concentration

Filter transmittance (or reflectance as in British Smoke) has been

added to mass as a soot indicator correlated with elemental carbon

Densitometer (TBX; Tobias Instruments,

Ivyland, PA)

Dual wavelength light transmission through

filters allows the separation of biomass

smoldering (370 nm) from flaming/engine exhaust (880 nm)

Optical Transmissometer, (Magee Scientific, Berkeley, CA, USA)

Integrated sphere method quantifies light

absorption/transmission at 250–1000 nm

UV/VIS spectrometer, (Lambda 35 , PerkinElmer,

Waltham, MA, USA) 0

20

40

60

80

100

120

140

100 200 300 400 500 600 700 800 900 1000

Lig

ht

Ab

so

rpti

on

Eff

icie

nc

y (

m2

g-1

)

Wavelength (nm)

Smoldering Biomass

Diesel Exhaust

Flaming Biomass

Organic functional groups can be quantified

by Fourier-transform infrared (FTIR)

spectrometryFunctional group

Absorbance peaks and/or region cm-1

Teflon peaks1150-1300 (1156,1212), 640, 554, 517

H2OSharp peaks 1300-1950, 3480-3960

CO2 Sharp peaks 665-672, 2280-2390

Particle H2O 1620-1640, 3350-3750

Aliphatic C-HSharp peaks 1370-1480, 2850-2950

Alkene C-H 2900-3100

Aromatic C-H 1000-1290, 3000-3100

Carbonyl C=O Sharp peaks 1640 - 1850

Aldehyde -CHO 2700 - 2860

Alcohol/Phenol O-HBroad peak 3200 – 3550, 1350, 650±50

Carboxylic acid C-OH Broad peak 2500 - 3000

Organonitrate Sharp peak 860, 1278, 1631

Organosulfur Sharp peak 876

Sulfate SO42- 612-618, 1080-1140

Ammonium NH+ 1400-1470, 2800-3400

Silicate SiO3 772-812, 1000-1200

Nitrate NO3- 720, 840-810, 1340-1400

Fourier-transform infrared spectroscope

(Vertex 70 FTIR; Bruker Biosciences

Corporation, Billerica, MA, USA)

Absorbance for some blank filters can be as high as the actual signal from

sample filters. Subtracting an average can create a problem.

Functional group vary by pollution source and there is

useful source apportionment information in unidentified

parts of the spectrum

Biomass Burning

Paved Road Dust

Acetylene Flame

Pellet Dust

De-Icing Material

Electric Arc

Paved

roadParking

lot

De-icing

material

Taconite

dust

IR and UV-VIS spectra for

fugitive dustIR and UV-VIS spectra for

biomass burning

Litter Duff Squaw Bitterbrush

X-ray Fluorescence (XRF) is non-

destructive and acquires 51 elements (from Na to U)

X-ray Fluorescence analyzer (PANalytical Model

Epsilon 5, Boulder, CO, USA)

silic

on

sulfur

chlo

rine

pota

ssiu

m

calc

ium

excitation p

eak

calc

ium

excitation p

eak

Elemental detection sensitivity is optimized by excitation condition and analysis

time. Longer analysis times reduce detection limits by (tusual/tenhanced)0.5

Rare-earth elements and isotopes can be

quantified by Inductively-coupled Plasma-Mass

Spectrometry (ICP-MS) but acid digestion destroys

the filter Rare Earth Elements

Cesium (Cs)

Barium (Ba)

Lanthanum (La)

Cerium (Ce)

Praseodymium (Pr)

Neodymium (Nd)

Samarium (Sm)

Europium (Eu)

Gadolinium (Gd)

Terbium (Tb)

Dysprosium (Dy)

Holmium (Ho)

Erbium (Er)

Thulium (Tm)

Ytterbium (Yb)

Lutetium (Lu)

Inductively-coupled Plasma-Mass Spectrometry (Nexlon 300D ICP-MS; PerkinElmer, Waltham, MA, USA)

Isotopes

Lead: Strontium:

204Pb 86Sr

206Pb 87Sr

207Pb

208Pb

Detection limits for ICP-MS are lower than

those of XRF for several elements

ICP-MS has difficulty detecting Si due to high background levels caused by the acid matrix

Instrument Detection Limit

0.01

0.1

1

10

100

Al Si K Ca V Mn Fe Ni Cu Br Pb

Elements

Min

imu

m D

ete

cti

on

Lim

it (

ng

cm

-2)

XRF

ICP/MS

Thermal/optical reflectance/transmittance carbon

analysis provides several carbon fractions

Thermal/Optical Analyzer (DRI Model

2001, Atmoslytics, Calabasas, CA)

Chow et al. (2007) JAWMA

°C Analysis Atmosphere

OC1 140 100% He (99.99% Purity)

OC2 280 100% He (99.99% Purity)

OC3 480 100% He (99.99% Purity)

OC4 580 100% He (99.99% Purity)

OP Return to original reflectance/transmittance value

EC1 580 98% He/2% O2

EC2 740 98% He/2% O2

EC3 840 98% He/2% O2

TC OC (OC1+OC2+OC3+OC4+OP) + EC (EC1+EC2+EC3-OP)

0

100

200

300

400

500

600

700

800

900

1000

0 200 400 600 800 1000 1200 1400 1600 1800 2000

FID

, L

as

er

Re

fle

ct

& L

as

er

Tra

ns

(re

lati

ve

un

its

)

Te

mp

era

ture

(°C

)

Time (sec)

IMPROVE_A Thermal/Optical Carbon Analysis Protocola

100% He 98% He/2% O2

EC by reflectance

OC1 OC2 OC3 OC4 EC1 EC2 EC3CH4

CAL

EC by transmission

reflectance

transmission

IMPROVE_A Thermal/Optical Protocol

Abundances of thermal carbon fractions vary

by source type

0%

10%

20%

30%

40%

50%

60%

70%

80%

90%

100%

Die

se

l @

4kW

D.R

. ~

40

Wo

od

sm

oke

,

Dilu

tion

Ra

tio

20

-

12

0

Ace

tyle

ne

Fla

me

(2")

; D

.R.

~1

6.5

PA

LA

S @

95

0

str

om

cu

rre

nt

Ma

ss P

erc

en

tag

e (

%) OC1

OC2

OC3

OC4

OPR

EC1-OPR

EC2

EC3

Ele

ctr

ic A

rc @

950

Chow et al. (2007) J. Environ. Sci. Health

• OC1–OC4 are evolved at 140, 280, 480, and 580 °C in a 100% helium atmosphere

• EC1–EC3 are evolved at 580, 740, and 840 °C in a 98% helium/2% oxygen atmosphere

• OPR is pyrolyzed carbon by reflectance

Thermal/optical analyzers can be adapted to obtain multiple

wavelength information related to black and brown carbon

Quartz Light

Pipes

Filter Sample

Heated up to

900 °C

Lasers

405 –1000 nm8-Leg

Optical Fibers

Reflectance

Photodiode

Tranmittance

Photodiode

Time (sec)

0 500 1000 1500 2000 2500

Ion

Sig

nal

(a.u

.)

0

200

400

600

800

1000

1200

1400

1600

1800

Oven

Tem

pera

ture

(°C

)

0

2

4

6

8

10

12

14

R 405nm

R 455nm

R 532nm

R 635nm

R 780nm

R 808nm

R 980nm

T 405nm

T 455nm

T 532nm

T 635nm

T 780nm

T 808nm

T 980nm

CalibrationCH

4 Injection

Temperature

100% He 98% He / 2% O2

140°C

480°C

580°C

740°C

840°C

280°CFID

Transmittance

Reflectance

Smoldering Flaming Diesel

• Using laser diodes, λ are 405,

445, 532, 635, 780, 808, and 980 nm

• Transmittance (T) and reflectance (R) analysis are normalized to the blank filter at end of analysis

•Black and brown carbon will be quantified for different temperature fractions

Light absorption patterns can be obtained as part

of the normal carbon analysis

The product of absorption optical depth (AbOD) and wavelength () accounts for

scattering within the filter media

Can obtain H, N, S, and O along with OC, EC, and

thermal fractions with the same analysis

Flow Control

NetworkCHNS Reactor

(MnO2)

C→CO2, H→H2O,

N→NOx/N2, S→SO2

NDIR CO2

Detector

Carrier/Reaction

Gases

98

% H

e,2

% O

2

He

He

, C

H4

He

, O

2, N

O, S

O2

Calibration

Gases

Oven

Filter Loading

Push Rod

UV-VIS-NIR

Light Source

(λ=400-1000 nm) Reflectance

Dector

Transmittance

Detector

Optical

Fibers

Filter

Filter

Holder

Thermocouple

Heated Fused

Silica Capillary

Mass

Spectrometer

Vent

Four-Way

Solenoid Valve

Flow

Splitter

Outputs:

Reflectance/

Transmittance

Spectra

O

Mass Spectra

C, H, N, S

O Reactor

(Ni/C)

O→CO

Oxidation

Oven

(CuO)

CO→CO2

Oxidation

Reactor

C→CO2

FIDMethanator

CO2→CH4

From

Oven

DRI Model 2001 Carbon Analyzer

C

DRI Model 2001

Carbon Analyzer

Outputs:

Thermal

Fragmentation

Oven

650°C

Flow Control

NetworkCHNS Reactor

(MnO2)

C→CO2, H→H2O,

N→NOx/N2, S→SO2

NDIR CO2

Detector

Carrier/Reaction

Gases

98

% H

e,2

% O

2

He

He,

CH

4

He

, O

2, N

O,

SO

2

Calibration

Gases

Oven

Filter Loading

Push Rod

UV-VIS-NIR

Light Source

(λ=400-1000 nm) Reflectance

Dector

Transmittance

Detector

Optical

Fibers

Filter

Filter

Holder

Thermocouple

Heated Fused

Silica Capillary

Mass

Spectrometer

Vent

Four-Way

Solenoid Valve

Flow

Splitter

Outputs:

Reflectance/

Transmittance

Spectra

O

Mass Spectra

C, H, N, S

O Reactor

(Ni/C)

O→CO

Oxidation

Oven

(CuO)

CO→CO2

Oxidation

Reactor

C→CO2

FIDMethanator

CO2→CH4

From

Oven

DRI Model 2001 Carbon Analyzer

C

DRI Model 2001

Carbon Analyzer

Outputs:

Thermal

Fragmentation

Oven

650°C

Flow Control

NetworkCHNS Reactor

(MnO2)

C→CO2, H→H2O,

N→NOx/N2, S→SO2

NDIR CO2

Detector

Carrier/Reaction

Gases

98

% H

e,2

% O

2

He

He

, C

H4

He,

O2,

NO

, S

O2

Calibration

Gases

Oven

Filter Loading

Push Rod

UV-VIS-NIR

Light Source

(λ=400-1000 nm) Reflectance

Dector

Transmittance

Detector

Optical

Fibers

Filter

Filter

Holder

Thermocouple

Heated Fused

Silica Capillary

Mass

Spectrometer

Vent

Four-Way

Solenoid Valve

Flow

Splitter

Outputs:

Reflectance/

Transmittance

Spectra

O

Mass Spectra

C, H, N, S

O Reactor

(Ni/C)

O→CO

Oxidation

Oven

(CuO)

CO→CO2

Oxidation

Reactor

C→CO2

FIDMethanator

CO2→CH4

From

Oven

DRI Model 2001 Carbon Analyzer

C

DRI Model 2001

Carbon Analyzer

Outputs:

Thermal

Fragmentation

Oven

650°C

More information on PM can be gained from thermal/optical analyses with different detectors

Time (min)

20 40 60 80

Ion

Sig

na

l (a

.u.)

0.0

2.0e+4

4.0e+4

6.0e+4

8.0e+4

1.0e+5

1.2e+5

8.0e+5

1.0e+6

1.2e+6

Ove

n T

em

pe

ratu

re (

°C)

0

200

400

600

800

1000

m/z=44 (CO2

+)

m/z=18 (H2O+) m/z=30 (NO

+)

m/z=64 (SO2

+)

CalibrationCH

4 Injection

Temperature

100% He 98% He / 2% O2

140°C

280°C

480°C

580°C

740°C

840°C

(a)

m/z=28 (CO+, N

2

+)

time vs Temp

Time vs m/z18

Time vs m/z28

Time vs m/z30

Time vs m/z64

Time (min)

20 40 60 80

ND

IR S

ign

al

(mV

)

40

60

80

100

400500

Oven

Tem

pera

ture

(°C

)

0

200

400

600

800

1000

140°C

280°C480°C

580°C

CalibrationO

2 Injection

NDIR

Temperature

100% He(b)

y = 0.926x - 0.104

R² = 0.989

0

1

2

3

4

5

6

0 1 2 3 4 5 6

Car

bo

n M

ass

by

Elem

enta

l An

alyz

er (µ

g)

Carbon Mass by Carbon Analyzer (µg)

EC1

OC3

OC2OC4

OC1

EC2EC3

1:1 Line

C, H, N, S, and O can be quantified for each

temperature fraction

Thermogram of Fresno ambient

aerosol sample for (a) CHNS, and

(b) O following the IMPROVE_A

protocol.

Comparison of carbon fractions

measured by elemental analyzer

and DRI Model 2001 carbon

analyzer

Mass spectrometer signals are linear with C, H, N,

and S quantities for calibration chemicals

Sulfanilamide: C6H8N2O2S; L-Cystine: C6H12N2O4S2

Evolved carbon as a function of temperature

can be quantified by thermogravimetric

analyzer (TGA) on quartz-fiber filter remnants

• Percent Moisture

• Percent Volatile Matter

• Percent Fixed Carbon

• Percent Ash

Thermal Gravimetric Analyzer (TGA/DSC-1 Mettler-

Toledo International, Inc., Columbus, OH, USA)

Thermal desorption-Gas Chromatography/Mass

Spectrometry (TD-GC/MS) can provide ~110 non-polar

organic compoundsa

• 37 Polycyclic aromatic hydrocarbons (PAHs)

• 26 n-alkanes

• 10 iso/anteiso-alkanes

• 2 methyl-alkanes

• 3 branched-alkanes

• 5 cycloalkanes

• 1 alkene

• 18 hopanes

• 12 steranes

Gas Chromatography with Mass Spectrometric

Detector (Model 6890 /Model 5975C, Agilent

Technologies, Santa Clara, CA, USA)

a Using ~1–2 cm2 of filter aliquot without solvent extraction

Acenapthene

Fluorene

Phenanthrene

Fluoranthene

Anthracene

Benzo(B)fluoranthene

Benzo(j+k)fluoranthene

Perylene

Water- and acid-extracted solutions

can be used for multiple analyses

Ultra-sonication

Sonicator (Branson Model

5200 Danbury, CT)

Mechanical Shaking

Sample shaker (Cole-Parmer Model

51401-00, Vernon Hills, IL)

Microwave Extraction(MCEM Mars 5, Matthews, NC)

Acid Digestion

Hot block digestor

(Environmental Express,

Ventura, CA)

More ions can be quantified with the same

analysis (Ion Chromatography with conductivity detector [IC-CD])

• Chloride (Cl-)

• Bromide (Br-)

• Nitrite (NO2-)

• Nitrate (NO3-)

• Phosphate (PO43-)

• Sulfate (SO4=)

• Ammonium (NH4+)

• Soluble Sodium (Na+)

• Soluble Magnesium (Mg2+)

• Soluble Potassium (K+)

• Soluble Calcium (Ca2+)

Ion Chromatograph (Dionex Model ICS

3000, Sunnyvale, CA, USA

NH4+

Mg2+

Ca2+

Na+

K+

Cl-

Br- NO3-

PO43- SO4

=

Water-soluble organic carbon (WSOC) is related to cloud

condensation nuclei, biomass burning, SOAa, and health

effects

Total WSOC by TOC and WSOC classes

• Neutral Compounds by HPLC-TOCa

• Mono- and Di-carboxylic acids by IC-PADa

• Humic-like substances by HPLC-SEC-ELSD-UV/VISa

Total Organic Carbon Analyzer

(Model TOC-L, Shimadzu

Corporation, Kyoto, Japan)

a SOA: Secondary Organic Aerosol; HPLC-TOC: High-performance Liquid Chromatography with Total Organic

Carbon; IC-PAD: Ion Chromatography with Pulsed Amperometric Detector, HPLC-SEC-ELSP-UV-VIS: HPLC with Size

Exclusion Chromotography and Evaporative Light Scattering Detector with Ultraviolet and Visible Light wavelengths

High Performance Liquid

Chromatography System (A200

Series , Agilent Technologies, Santa

Clara, CA, USA)

Carbohydrates are related to biomass

burning and bioaerosols (Ion Chromatography-Pulsed

Amperometric Detector [IC-PAD])

Carbohydrates

• Glycerol (C3H8O3 )

• Inositol (C6H12O6)

• Erythritol (C4H10O4 )

• Xylitol (C5H12O5 )

• Levoglucosan (C6H10O5 ); Biomass burning marker

• Arabitol (C5H12O5 ); Fungal biomarker

• Sorbitol (C6H14O6 )

• Mannosan (C6H10O5)

• Mannitol (C6H14O6) ;Fungal biomarker

• Glucose (C6H12O6 )

• Xylose (C5H10O5 )

• Fructose (C6H12O6 )

• Trehalose (C12H22O11 )

• Arabinose (C5H10O5 )

• Galactose (C6H12O6 )

• Maltitol (C12H24O11 )

IC-PAD (Model ICS 3000 Dionex, Sunnyvale,

CA, USA)

levoglucosan

arabitol

mannitol

Organic acids are related to biomass

burning and cooking emissions

Monocarboxylic acids:

• Lactic acid (C3H6O3 )

• Acetic acid (C2H4O2)

• Formic acid (CH2O)

• Methanesulfonic acid (CH4SO3 )

Dicarboxylic acids:

• Glutaric acid (C5H8O4 )

• Succinic acid (C4H6O4)

• Malonic acid (C3H4O4 )

• Maleic acid (C4H4O4)

• Oxalic acid (C2H2O4)

Ion Chromatography with Electrochemical

Detector (IC-ECD, Dionex Model ICS 2100 Ion

Chromatograph, Sunnyvale, CA, USA)

Formate

Succinate

Oxalate

Elemental analysis quantifies total C, H, N, S,

and O for OM to OC ratios on liquids and

quartz-fiber filters

• Carbon (C)

• Hydrogen (H)

• Nitrogen (N)

• Sulfur (S)

• Oxygen (O)

Elemental Analyzer (FlashEA 1112 , Thermo Fischer

Scientific, Waltham, MA, USA)

Conclusions

• A large variety of analyses, especially for organic compounds, can be applied to recent or archived samples to verify source contribution estimates

• Teflon-membrane filters can yield much information from non-destructive IR and UV-VIS analysis. Rare-earth elements and some isotopes can be determined by ICP-MS after acid extraction

• Quartz-fiber filters can yield more optical and chemical information from routine thermal/optical analyses with multi-wavelength lasers and multi-elemental detectors. TD-GC/MS is an established and efficient method for non-extraction organic marker analysis

• Water extracts are amenable to several analyses for polar organics, including biomass burning and secondary organic aerosol markers

Challenges for Enhanced Chemical

Characterization of Filter Samples

• Perfecting, evaluating, and making more efficient procedures for

additional characterization

• Modifying instrumentation and procedures to incorporate more

specific analyses methods into long-term chemical speciation

networks to obtain more information from existing samples

• Maintaining continuity and consistency with the long-term

trends data sets

• Developing more detailed source profiles with these methods

for speciated inventories and source apportionment

Questions?