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SP2-AMS
AMS User Meeting 2008, Manchester
Achim M. Trimborn, Timothy B. Onasch, John T. Jayne, Sally NgLeah Williams, Douglas R. Worsnop
Aerodyne Research, Inc.
Gregory L. Kok, Darrel BaumgardnerDroplet Measurement Technologies
Eben Cross, Billy Wrobel, Adam Ahern, Paul DavidovitsBoston College
ICCPA August 2008
Happy Birthday
Astrid
Need for new soot particle instruments
Black carbon (BC) particles− Absorb light efficiently, contributing to radiative forcing − Significant anthropogenic sources
BC particles typically coated in the atmosphere− Primary combustion products− Secondary organic and inorganic condensates− Compositions and fate of BC containing particles are not well
knownNeed new instruments capable of measuring the refractory and non-refractory mass, size and composition of soot containing particles
Instrument conceptSP2 + AMS => SP2-AMS
SP2: Single Particle Soot Photometer(Droplet Measurement Technologies)
- little information on absorbed compounds, particle chemistryAMS: Aerosol Mass Spectrometer (Aerodyne Research, Inc.)
- Lack of sensitivity to refractory particles (i.e. black carbon soot)
SP2-AMS: new combined instrument− Intracavity laser vaporization of the coatings and refractory
cores of absorbing (λ = 1 µm) particles − Electron impact ionization− Measures both the non-refractory components of the
coatings (e.g. organics, sulfates, nitrates, etc.) and the refractory carbon cores (i.e. black carbon) via Time-of-Flight mass spectrometry
AMS Schematic
Measures non-refractory aerosol chemical composition and massInsensitive to refractory aerosol (e.g. black carbon)
How to build a SP2-AMS
Remove vaporizer
SP2-AMS schematic
Install SP2 module
Schematic of the SP2-AMS module
Absorbing particles (coating and core) vaporize in laserVapor is ionized by electron impact ionizationDetection of the ions by Time-of-Flight mass spectrometryReadily installed in any exiting AMS instrument
0
Coating Evaporating
Coated Soot Particle
Laser Beam
Core Evaporating
Transit of Soot Particles Across Laser
Beam5-20 microsecond
evaporation time
Coatings evaporate first at relatively low temperatures (<600oC) potentially dependent upon vapor pressures
Core evaporates last at high temperature (>1000oC) under SP2-like incandescence conditions
Coating and core material ionized and detected with mass spectrometry
20Gao et al. 2007
Oil Lamp Soot Particles
Obtain chemical information on elemental carbon clusters and organic compounds coating the soot cores
70x103
60
50
40
30
20
10
0
Sig
nal
10080604020m/z
C8m/z=96
C7m/z=84
Air Beam Organics Elemental Carbon
C6m/z=72
C5m/z=60
C3m/z=36
C4m/z=48
C2m/z=24
C1m/z=12
H2Om/z=18
N2m/z=28
8
4
0
(µg/
m3 ) /
(dlo
gDva
)
2 3 4 5 6 7 8100
2 3 4 5 6 7 81000
Dva (nm)
8
4
0
8
4
0
Size Distributions for uncoated and coated particles
Obtain chemical mass distribution information for both carbon and organic signals
PTOF show size and particle mass signals increasing with particle coatings
225 nm Glassy Carbon Spheres uncoated and coated with DEHS oil
No coating
3 nm coating
50 nm coating Organics / 15
` organic signal
carbon signa;
6
4
2
0
µg/m
3
102 3 4 5 6 7 8 9
1002 3 4 5 6 7 8 9
10002
PToF size, nm
0.10
0.08
0.06
0.04
0.02
0.00
Time delay for fullerenes
Cn
fullerenes
H2SO4coating
Coating Signals: DEHS Mass Spectra
Less fragmentation in SP2-AMS than in AMSLarge parent ion signal and fragmentation pattern more similar to
NIST data base spectrumMost of the coating material evaporates at temperatures < 600oC
Vaporized from laser-heated soot particles
Vaporized from600oC vaporizer
NIST database
Carbon Signals: Fullerene Series4000
3000
2000
1000
0
Ion
rate
(Hz
s-1)
120010008006004002000m/z
C32 C50 C60 C70
small medium large carbon cluster ionsfullerenesmedium carbonclusters
small carbonclusters
10-1
100
101
102
103
104
105
106
Ion
rate
(Hz
s-1)
Fullerene Soot
10-1
100
101
102
103
104
105
106
Ion
rate
(Hz
s-1)
Premixed Ethylene Flame Soot
10-1
100
101
102
103
104
105
106
Ion
rate
(Hz
s-1)
3500300025002000150010005000m/z
Cabot Regal Black Pigment
‘Black Carbon’ Chemical Composition
0.0 0.2 0.4 0.6 0.8 1.0
Regal black
Flame soot
Fullerenesoot
Bla
ck c
arbo
n ty
pe
Fraction
FullereneMedium carbon clustersSmall carbon clusters
Ambient Measurements
Quantification and Detection LimitsCarbon Signal vs Laser Power
6x10-6
5
4
3
2
1
0
Blac
k ca
rbon
sig
nal
1086420
Laser Power
Hyperbolic tangent functionf(x) = b*((exp(a*x)-exp(-a*x))/(exp(a*x)+exp(-a*x))) Coefficient values ± one standard deviation
a =0.32 ± 0.05b =5.4 ± 0.3e-6
SP2 instruments operate at laser powers of ~2
Higher laser powers required in SP2AMS due to faster particle velocities
157 nm (1 fg) Ethylene Flame Soot
Carbon Signal vs MAAP CBC10x103
8
6
4
2
0
AMS
Car
bon
Sign
al
50403020100MAAP CBC (ug/m3)
NoritSXNoritSXNoritSXNoritSXNoritSXNoritSX
CarbonNanoCarbonNanoCarbonNanoCarbonNanoCarbonNanoCarbonNanoCarbonNanoCarbonNano
GlassyCarbonGlassyCarbonGlassyCarbonGlassyCarbonGlassyCarbonGlassyCarbonGlassyCarbon
PSLPSL
SP2-AMS vs MAAP V_Pr= 0.962059
a = -23.695 ± 26.7 b = 176.82 ± 8.02
V_Pr= 0.930573 a = -40.253 ± 29.6 b = 194.62 ± 3.01
V_Pr= 0.70619 a = 4.3244 ± 26.2 b = 204.01 ± 7.74
Total carbon signal is constant for different monodisperse soot particles
2 .5
2 .0
1 .5
1 .0
0 .5
Org
sig
nal
1 0 08 06 04 02 00C o a t i n g th ic k n e s s ( n m )
8 x 1 0- 3
6
4
2
FR
sig
nal
1 0 08 06 04 02 00C o a t in g t h i c k n e s s ( n m )
Signal vs coating thickness
10-10
10-9
10-8
10-7
10-6
10-5
10-4
10-3
10-2
10-1
100
101
Run
136
, no
coat
ing
10-10
10-9
10-8
10-7
10-6
10-5
10-4
10-3
10-2
10-1
100
101
Run 141, coating = 105 nm
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111112
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Coefficient values ± one standard deviationa =0 ± 0b =1.0112 ± 0.000623
SummarySP2AMS: Successfully adapted SP2 module into AMS− Separate volatilization and ionization mechanisms− Only sensitive to absorbing particles (soot or metals) − Chemical and size information obtain for elemental carbon cores and non-
refractory organic coatingsMeasure of organic coating mass and size− Shows less fragmentation than standard AMS spectra
Measure of particulate elemental carbon mass and size− Provides chemical information on ‘black carbon’ particles− Linear correlation between MAAP absorption and carbon cluster ion signals from
SP2-AMS for several different types of soot particles− Fully vaporizes 160 nm (~1 fg) soot particles under higher laser powers
Quantification studies have been carried out and are being analyzed− Boston College – Aerodyne Soot Project 2
Department of Energy (DOE) SBIR