principle behind sp2 (single-particle soot photometer)

6
Scattering Incandescence Incident Laser Principle behind SP2 (Single-Particle Soot Photometer) Schwartz et al., 2006; Moteki & Kondo, 2007, Subramanian et al., 2010 Standard Data products: Time series: number conc; mass conc; Distributions: dN/dlogD p ; dM/dlogD p rBC Mixing State: Probe coating thickness: optical and BC mass equivalent diameters Examine temporal profiles of the scattering and incandescence signals High specificity towards ‘refractory’ black carbon (rBC) Particle-by-particle measurement scheme

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Page 1: Principle behind SP2 (Single-Particle Soot Photometer)

Scattering

Incandescence

Incident Laser

Principle behind SP2 (Single-Particle Soot Photometer)Schwartz et al., 2006; Moteki & Kondo, 2007, Subramanian et al., 2010

Standard Data products: ‣ Time series: number conc; mass conc; ‣ Distributions: dN/dlogDp; dM/dlogDp

rBC Mixing State: ‣ Probe coating thickness: optical and BC mass equivalent diameters‣ Examine temporal profiles of the scattering and incandescence signals

High specificity towards ‘refractory’ black carbon (rBC)Particle-by-particle measurement scheme

Page 2: Principle behind SP2 (Single-Particle Soot Photometer)

Probing Configurational Mixing State of rBCScattering and incandescence signals provides information ratio of aged/fresh rBC and fraction of off-center rBC-containing particles.

The Presence of Near-surface Black Carbon in Aerosol Particles

Arthur J. Sedlacek, III, Ernie R Lewis, and Lawrence Kleinman Brookhaven National Laboratory

Aerosol particles containing substances that absorb visible radiation have a strong effect on climate and also affect cloud formation and precipitation by altering the temperature profile of the atmosphere. Thus it is necessary to understand and parameterize properties and behavior of such particles for representation in global and regional climate models. Typically a conventional core-shell model has been assumed in which an absorbing spherical core is surrounded by a concentric shell of non-absorbing material. Such a configuration has been implicit in the interpretation of data from the Single-Particle Soot Photometer (SP2), which measures both scattering and incandescence of individual particles containing refractory black carbon (rBC). When a particle containing rBC enters the laser beam of the SP2 (which can be detected by a scattering signal), the rBC absorbs energy which it initially dissipates though evaporation of the non-refractory coating, and subsequently through incandescence. The time difference between the peak of the scattering signal and the incandescence signal has been used (together with the assumption of a core-shell geometry) to provide an estimate of the coating thickness; the greater the lagtime the greater the coating thickness. Recently Sedlacek et al. (2012) observed negative lagtimes in aerosol particles containing rBC; such behavior had not previously been reported in ambient conditions. In one time period the fraction of rBC-containing particles with negative lagtimes was greater than 60%. The occurrence of a negative lagtime would require that the rBC incandesced before the peak of the scattering signal, a situation seemingly not possible with the core-shell structure. To explain this behavior, Sedlacek et al. proposed that the rBC was near the surface in such particles, and that upon absorption of energy from the laser the particle fragmented because of the inability of the coating material to dissipate heat sufficiently rapidly through evaporation. This lagtime technique allows real-time analysis of rBC-containing particle structure and provides a way to distinguish those rBC-containing particles for which rBC is near the surface from those more closely resembling the conventional core-shell configuration. Additionally, this technique provides quantification of the fraction of near-surface rBC particles among all ambient rBC-containing particles, and thus yields insight into the processes of aerosols containing these particles. The occurrence of a large fraction of rBC-containing particles for which the rBC is near the surface has important implications for radiative forcing calculations that assume a core-shell model. Reference: Sedlacek, A. J., III, E. R. Lewis, L. Kleinman, J. Xu, & Q. Zhang, “Determination of and evidence for non-core-shell structure of particles containing black carbon using the single particle soot photometer (SP2),” Geophys. Res. Letts., 2012. doi:10.1029/2012GL050905

Sca

tterin

g S

igna

l

403020100

Elasped Time (µs)

Inca

ndes

cenc

e S

igna

l

Thick coating = Δτ ≈ 3 µs

Sca

tterin

g S

igna

l

403020100

Elasped Time (µs)

Inca

ndes

cenc

e S

igna

l

Thin coating = Δτ ≈ 0 µs

Sca

tterin

g S

igna

l

403020100Elapsed Time (µs)

Inca

ndes

cenc

e S

igna

l Δτ < 0 µs

SP2 incandescence and scattering signals for thinly-coated (top), thickly-coated (middle), and near-surface rBC-containing particles (bottom).

-8

-6

-4

-2

0

2

4

6

8La

gtim

e ( µ

s)

400300200100

BC MED (nm)

Plume A

-8

-6

-4

-2

0

2

4

6

8

Lagt

ime

( µs)

400300200100

BC MED (nm)

Plume B

Sedlacek et al., 2012

Δτ = τincandescence - τscattering = time to ‘boil off’ coating

Uncoated Black Carbon

(BC)

Page 3: Principle behind SP2 (Single-Particle Soot Photometer)

-8

-6

-4

-2

0

2

4

6

8

Lagtime/µs

3a

40003000200010000 cm-3

-8

-6

-4

-2

0

2

4

6

8

Lagtime/µs

400300200100

Dme,rBC/nm

3b

Near surface rBC-particles in biomass burns

0.7

0.6

0.5

0.4

0.3

0.2

0.1Frac

tion

with

nea

r-su

rface

BC

, Φns

00:008/2/11

06:00 12:00 18:00 00:008/3/11

Time (UTC)

0.008

0.007

0.006

0.005

0.004

0.003

Mass concentration ratio

C2H4O2+/Org (m/z=60)

C3H5O2+/Org (m/z=73)

Sedlacek et al., 2012Probing rBC Mixing State: Negative Lagtimes

B

B

AA

Page 4: Principle behind SP2 (Single-Particle Soot Photometer)

4000

3000

2000

1000

0

Altit

ude

(m)

-70.0 -69.5 -69.0 -68.5 -68.0 -67.5 -67.0

Long (deg)

Flight: 120717a4003002001000

rBC conc (ng/m3)

3.0

2.5

2.0

1.5

1.0

Aged/Fresh rBC

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-4

0

4

8

Lagt

ime

(µs)

500300100rBC MED (nm)

dN/dLogDp

dmean=103 nm

-8

-4

0

4

8

Lagt

ime

(µs)

500300100rBC MED (nm)

dN/dLogDp

dmean= 111 nm

-8

-4

0

4

8

Lagt

ime

(µs)

500300100rBC MED (nm)

dN/dLogDp

dmean=85 nm

-8

-4

0

4

8

Lagt

ime

(µs)

500300100rBC MED (nm)

dN/dLogDp

dmean=94 nm

TCAP: July 17, 2012 - preliminary

SP2 Lagtime analysis suggests significant variations in rBC-particle morphology. Variations in particle morphology accompanied by differing size distributions

Page 5: Principle behind SP2 (Single-Particle Soot Photometer)

Comparison of Lab and Field Lagtime Distributions

-8-6-4-202468

Δτ (

µsec

)

500300100rBC MED/nm

TCAP: 20120717a

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-6

-4

-2

0

2

4

6

8

Δτ

(µse

c)

500300100

rBC MED/nm

RB+NaCl coagulation

Initial comparisons between laboratory data and field measurements suggests variation in configuration mixing state

Preliminary data

-8-6-4-202468

Δτ (

µs)

500300100rBC MED/nm

RB+DOS coagulation

-8

-6

-4

-2

0

2

4

6

8

Δτ

(µse

c)

500300100rBC MED/nm

Bangalore: 2012-11-19

Page 6: Principle behind SP2 (Single-Particle Soot Photometer)

Compositional and Configurational Mixing State

TCAP and BBOP offer the opportunity to look at the relative importance of these two mixing states

TCAP: Urban emissions SPLAT provides chemical composition on rBC-containing particles SP2 provides configuration information on rBC-containing particles

BBOP: biomass burn emissions SP-AMS provides chemical composition on rBC-containing particles SP2 provides configuration information on rBC-containing particles

Closure through RrBC: non-refractory mass/rBC mass