Aerosol Formation in the Atmosphere

advertisement

Aerosol Formation in the

Atmosphere

David Cocker

Department of Chemical and

Environmental Engineering

CE-CERT

Program Goal

• Development of a detailed chemical mechanism for the prediction of ozone, toxics, and secondary organic aerosol(SOA) formation within the atmosphere

– Studies of ozone and SOA at VOC and NO x similar to the urban atmosphere levels

– Investigation of gas-particle partitioning of semivolatile compounds in the presence of ambient particle loadings

– Improved interpretation of ambient data obtained using aerosol mass spectrometers

Ozone

• Created by a chemical reaction between volatile organic compounds (VOCs) and oxides of nitrogen (NO x

) in the presence of sunlight.

VOC + NO x

+ sunlight

Ozone

• Lung irritant

• Permanent lung damage

• Asthmatic trigger asthma

• Reduced lung function

• Increased respiratory illnesses.

• Plant and ecosystem damage.

U.S. Counties in non-attainment for Phase II Ozone Rule, 2005

(0.08 ppm for 8 hr standard) www.epa.gov

Fine Particulate Matter

• Microscopic liquids and/or solids sufficiently small to deeply penetrate the lungs.

• Study Motivated by Clean Air Rules, 2004

– Health-based Standards

• Linked to premature death

• Aggravation of cardiovascular and respiratory disease

• Decreased lung function

• Asthmatic triggers

• Coughing/wheezing/difficulty breathing

• Many counties in most populous regions within the

United States designated as non-attainment areas

U.S. Counties in non-attainment for fine particle standard, 2005

(65

µ g m -3 for 8 hr standard) www.epa.gov

Fine Particulate Matter

• Secondary aerosol can contribute to the majority of fine particulate mass concentrations in polluted regions

• SOA significant contributor to fine particle concentrations in urban airsheds

– Up to 80% of urban organic carbon attributed to secondary organic aerosol

Sources of PM

2.5

in Western Riverside County

R 2 = 0.91

χ 2 = 0.53

% MB = 115.9

Aerosol Round The World

Q. Zhang, et al.GRL, 34:L13801, 2007

Fine particulate matter

• Visibility reduction:

Pasadena, CA

Fine particulate matter

• Global radiative forcing (direct and indirect) thereby affect global climate change

How does Aerosol Affect us?

Health Effect

Regional

Air Quality

Climate

Effect

Impacts of PM

2.5

Pollution in South Coast Basin

“ Exposures to air pollution can shorten life by about 14 years for people who die prematurely”

— CARB 2007

Source: California Air Resources Board, 2007; 1999-2000 Air Quality Data

Air Quality Modeling Overview

Scenario

Emissions

Control

Conditions Strategies

Air Quality Model

Other Model

Components

Chemical

Mechanism

Critical to predicting secondary pollutants

Air Quality

Predictions

Health and Social

Impacts

Source Characterization

International Shipping Trade Routes infranetlab.org/blog/2008/10/goodbye-global/

Ports of Los Angeles and Long Beach

• Nation’s largest container cargo port complex

•>40 % of nation’s containerized imports arrive here

Various Port Sources

Engines on OGVs

• Main Propulsion Engine

– Two Stroke

– Displacement > 1000 liters/Cyl

(6-12 cyl)

– 54,000 kW, 90 rpm Main Engine Cylinder

• Auxiliary Engine

– Four Stroke

– Displacement > 10 liters/Cyl

(6cyl)

– 900 kW, 900 rpm

Test Fuels

• Heavy Fuel Oil (HFO)

– Commonly known as bunker fuel or residual oil

– Residual fraction from crude refining

– Used on main engine and boiler

– Very high viscosity and high sulfur content (2.6% m/m)

• Marine Gas Oil and Marine Distillate Oil

– Refined fraction from crude distillation

– Used on auxiliary engine

– Lower sulfur content (0.16 %m/m)

21

Sulfuric Acid – Stack Damage

23

Photograph taken of the container ship from the cabin of the CIRPAS Twin

Otter

Particle Size

• Soot (D primary

~30nm)

• Nanoparticles(5-8nm)

• Unknown particles( 30-80nm)

• EDS found V and S both from nanoparticles and unknown particles.

Comparison of PM Emissions (g/kg

CO

2

)

3

2.5

1

0.75

0.5

0.25

0

HDD trucks Switching

Locomotives

Ship Main

Engine

Ship Auxiliary

Engine

Yard Tractor BUG Aircraft

Total Hydrocarbon Emissions (g/kg

CO

2

)

3

1.25

1

0.75

`

0.5

0.25

0

HDD trucks Switching

Locomotives

Ship Main

Engine

Ship Auxiliary

Engine

Yard Tractor BUG Aircraft

Comparison of PM Emissions

(g/mile/ton)

0.035

0.03

0.025

0.02

0.015

0.01

0.005

0

1994-97 1998

HDD Trucks

1999-

2002

SD-18 SD-20 SW-

1200St1

SW-

1200St2

Locomotive

Main

Engine

Auxiliary

Engine

Ships

Moving From Primary to Secondary

Pollutants

• Ozone: only formed in atmosphere

• Particulate matter: 80% formed in the atmosphere

Mechanism Development

Theory and

Estimations

Basic Lab.

Data

Chemical

Characterization

Instrumentation

Chemical Mechanism

Simulation of Experiments

No

Consistent?

No

Atmospheric

Simulation

Experiments

(Environmental

Chamber Data)

Yes

Mechanism Might be satisfactory for air quality modeling

Environmental Chamber Research

Secondary Organic Aerosol (SOA) Formation

Heterogeneous

Volatile Organic

Chemistry

Compound

Condensation

Oxidation

(OH,O

3

,NO

3

) Evaporation

Nucleation

Fine Particles Coarse Particles

0.01 0.3 2 10

Particle Diameter (

µ m)

SOA Theory: Equilibrium Partitioning of

HC + Oxidant

Semi-Volatile Compounds

α i

P i

P i

= A i

+ G i

K om,i G

1

, G

2

,…,G n

A

1

, A

2

,…,A i

A i

– Aerosol Products

G i

– Gaseous Products

M o

– Mass of Organic in Aerosol

K om

– Gas Partitioning Coefficient

A i

/

M o

R – Ideal Gas Constant

K om,i

=

γ

– Activity Coefficient G i p o

Li

– Sub cooled saturation liquid vapor pressure

α

– Mass based stoichiometric coefficient

Y

=

M o

ΔHC

= ∑ i

Y i

=

M o

∑ i

1

+

α i

K om, i

K om, i

M o

(Odum et al., 1996)

=

RT

MW om

γ i p o

L,i

=

M o

α

1

+

K

K om om

M o

Single Product Model

UCR Chamber Facility

UC Riverside/CE-CERT

Environmental Chamber

Air handler circulation system

Purified air flushed 450 m 3 enclosure

Descending frames to maintain positive pressure

Argon arc lamp

Dual 90 m 3

Teflon reactors

Particle free two chamber humidifier

Black lights

Dual SMPS’s

Injection and sample ports

TDMA – Hygroscopicity Measurement

SOA formation potential

60

50

40

30

20

PM Volume(corrected)

PM Volume(uncorrected)

Hydrocarbon

10

0

0 100

Y

=

ΔM o

ΔROG

=

200

∑ i

Y i

500 600 300 400

Time (minute)

=

M o

∑ i

1

+

α i

K om, i

K om, i

M o

0

2

12

10

8

6

4

SOA Formation Potential (yield) as Function of Aerosol Mass (m-Xylene)

0.20

0.18

Traditional Smog

Chamber Experiments

0.12

0.10

0.08

0.06

0.04

0.02

0.00

0 50 100

M o

(

150

µ g/m

3

)

200

HCo:Nox>8.0

HCo:NOx<5.5

250 300

Aerosol Mass vs. Reacted HC

400

350

300

250

25

20

15

10

5

α

1

α

2

=0.049, Κ

1

=0.178, Κ

2

=0.301

=0.008

Semi-

Empirical

Model

Estimates

0

0

200

150

100

100 200

ΔHC( µ g/m

3

)

Low

NO x

300

α

1

α

2

=0.024, Κ

1

=0.152, Κ

2

=0.229

=0.004

High

NO x

50

HCo:NOx>8.0

HCo:NOx<5.5

0

0 200 400 600 800 1000

ΔHC( µ g/m

3

)

1200 1400 1600 1800 2000

Detailed chemical speciation needed to identify key oxidation products; chemical mechanism based model needed to predict impacts of NOx and other atmospheric species on SOA formation

What can we do here?

• There are many individual and team projects that lead to the results shown above

– What do the particles formed look like?

• What are their chemical characteristics?

• What are their physical characteristics?

• What is their atmospheric behaviour?

– What hazardous air pollutants are released?

• By whom? Where? Who is impacted?

– Lots of instruments, lots of students to work with, lots of questions to address……

Chemical Instrumentation

AMS

VOCs

+

Oxidants

CRDS

IR-CRDS

Intermediates

Products

(aerosol)

Products

(gases)

LCMS

PTR-MS

GC-FID

Aerosol Instrumentation

Atmospheric reactor

SOA

SMPS

(Size

Distribution)

(CCN)

Cloud particle activation

CPC

(Number

Concentration)

Aerosol

Mass

Produced

APM

(Single

Particle Mass)

Download