Development and Application of CACM/MPMPO
Development and Application of CACM/MPMPO
Development and Application of CACM/MPMPO
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<strong>Development</strong> <strong>and</strong> <strong>Application</strong> <strong>of</strong><br />
<strong>CACM</strong>/<strong>MPMPO</strong><br />
R.J. Griffin 1 , J. Chen 1 , C.E. Jordan 1 , H. Mao 1 , R.W.<br />
Talbot 1 , S. Vutukuru 2 , <strong>and</strong> D. Dabdub 2<br />
1<br />
UNH, 2 UCI<br />
December 6, 2006<br />
International Conference on Atmospheric Chemical<br />
Mechanisms
Polycyclic<br />
Low Y<br />
Functionalized Hydrocarbons<br />
Primary<br />
VOC<br />
Aromatic<br />
Non-Arom.<br />
Aromatic<br />
Non-Arom.<br />
Monoaromatic<br />
Alkanes<br />
Alkenes<br />
Biogenics<br />
Phenolic<br />
Aldehydic<br />
Acidic<br />
Carbonyls<br />
Ethers<br />
High Y<br />
C 2 -C 6<br />
C 6 -C 12<br />
C 13 +<br />
Ethene<br />
C 3 -C 6<br />
C 7 +<br />
Terpenes<br />
Isoprene<br />
Aldehydes<br />
Ketones<br />
MeOH<br />
EtOH<br />
α-Pinene<br />
β-Pinene<br />
d-Limonene<br />
Low Y<br />
High Y<br />
HCHO<br />
CH 3 CHO<br />
C 3 +<br />
C 3 -C 6<br />
Alcohols<br />
C 3 +<br />
C 7 +
Surrogate Determination<br />
Example:<br />
AROL – low SOA yield aromatics: two or more methyl<br />
substituents<br />
3 xylene isomers<br />
3 TMB isomers<br />
3 TetMB isomers<br />
More highly substituted}<br />
Average C#: ~9 TMB<br />
1,2,3-TMB<br />
k OH<br />
,<br />
prevalence
The Mechanistic Approach<br />
A + ox<br />
α RP/UR 1<br />
}<br />
if α, β, <strong>and</strong> γ have<br />
β RP/UR 2 been determined<br />
γ RP/UR 3<br />
ox<br />
…<br />
(1−α−β−γ) RO 2 i<br />
NO<br />
ξ ROi + ξ NO2 + (1-ξ) APi<br />
OH<br />
RP/UR<br />
isomerization<br />
decomposition<br />
reaction with O 2<br />
RP/UR
Example Chemistry<br />
Now over 500 reactions to describe the formation <strong>of</strong> SOA precursors,<br />
ozone, <strong>and</strong> other photochemical pollutants (Griffin et al., 2002, 2005;<br />
Chen <strong>and</strong> Griffin, 2005)
Formation <strong>of</strong> SOA<br />
VOC + ox <br />
P 1 , P 2 , …P n<br />
G 1 ,G 2 ,...,G n<br />
A 1 ,A 2 ,...,A n<br />
AQ 1 ,AQ 2 ,...,AQ n<br />
K om,i<br />
Partitioning Theory<br />
A i<br />
/ M o<br />
= ∼<br />
G i<br />
Griffin et al. (2003, 2005)<br />
RT<br />
p o L,i MW om γ i<br />
Henry’s Law <strong>and</strong><br />
Dissociation<br />
H i<br />
= γ i<br />
aq<br />
AQ i<br />
/G i<br />
AQ i AQ i - AQ i<br />
2-<br />
Inorganics using ISORROPIA
Simulation <strong>of</strong> Chamber Experiments<br />
700<br />
70<br />
NO, NO 2 <strong>and</strong> O 3 mixing ratio (ppb)<br />
600<br />
500<br />
400<br />
300<br />
200<br />
100<br />
0<br />
d-limonene<br />
NO<br />
0 30 60 90 120 150 180<br />
Time (min)<br />
O 3<br />
NO 2<br />
60<br />
50<br />
40<br />
30<br />
20<br />
10<br />
0<br />
d-limonene mixing ratio (ppb) -<br />
Experiment: Griffin et al. (1999)<br />
Simulation: Chen <strong>and</strong> Griffin (2005)
Simulation <strong>of</strong> Chamber Experiments<br />
SOA (µg m -3 )<br />
40<br />
30<br />
20<br />
10<br />
Predicted<br />
Observed<br />
0<br />
0 100 200 300<br />
Time (min)<br />
Experiment (α-pinene + O 3 ): Griffin et al. (1999)<br />
Simulation: Chen <strong>and</strong> Griffin (2005)
Simulation <strong>of</strong> Chamber Experiments<br />
Predicted SOA / Observed SOA<br />
3.0<br />
2.0<br />
1.0<br />
0.0<br />
α-pinene<br />
β-pinene<br />
d-limonene<br />
1 10 100 1000<br />
Observed SOA (µg/m 3 )<br />
Experiments: Odum et al. (1996); H<strong>of</strong>fmann et al. (1997); Griffin et al. (1999)<br />
Simulations: Chen <strong>and</strong> Griffin (2005)
Implementation into CMAQ<br />
Caltech Atmospheric<br />
Chemistry Mechanism<br />
Updated with α-Pinene,<br />
β-Pinene & d-Limonene<br />
Chemistry<br />
H 2<br />
SO 4<br />
,HNO 3<br />
NH 3<br />
ISORROPIA Inorganic<br />
Aerosol Module<br />
H 2<br />
O, H +<br />
SOA<br />
Precursors<br />
POA<br />
Model to Predict the<br />
Multi-phase<br />
Partitioning <strong>of</strong> Organics<br />
SOA Output
Model<br />
Domain<br />
62 x 66 cells<br />
36km resolution<br />
21 vertical layers<br />
Dates: August 3-4, 2004<br />
August 1-2 spin-up<br />
(ICARTT)<br />
Meteorological fields:<br />
MM-5<br />
Emissions: 1999 NEI/BEIS3<br />
Circles: IMPROVE<br />
Star: AIRMAP<br />
Triangles: SEARCH
Example Gas-Phase Results: AI*<br />
160<br />
Observation<br />
120<br />
<strong>CACM</strong><br />
CB4_1<br />
O 3 Mixing Ratio (ppb)<br />
80<br />
40<br />
0<br />
2004-8-3 0:00 2004-8-3 12:00 2004-8-4 0:00 2004-8-4 12:00 2004-8-5 0:00<br />
Time (UTC)<br />
*Appledore Isl<strong>and</strong>, ME Chen et al., 2006
Aerosol-Phase Results: Domain<br />
18<br />
Concentration (µg/m 3 )<br />
16<br />
14<br />
12<br />
10<br />
8<br />
6<br />
Measured<br />
<strong>CACM</strong>/<strong>MPMPO</strong><br />
CB4/SORGAM<br />
4<br />
2<br />
0<br />
PM2.5 Sulfate Nitrate Ammonium EC OC<br />
24-hour filter measurements; ions by IC, EC <strong>and</strong> OC by thermo-optical method<br />
Chen et al., 2006
Aerosol-Phase Results: TF*<br />
12.0<br />
AMS measured<br />
6.0<br />
Measured OC (µg/m 3 )<br />
10.0<br />
8.0<br />
6.0<br />
4.0<br />
2.0<br />
<strong>CACM</strong>/<strong>MPMPO</strong><br />
CB4/SORGAM<br />
4.0<br />
2.0<br />
Modeled OC (µg/m 3 )<br />
0.0<br />
8-3 0:00 8-3 12:00 8-4 0:00 8-4 12:00 8-5 0:00<br />
Time (UTC)<br />
0.0<br />
Data from an Aerodyne Q-AMS (Cottrell et al., 2006, in prep.)<br />
*Thompson Farm, NH<br />
Chen et al., 2006
Domain-Wide Results: SOA<br />
<strong>CACM</strong>/<strong>MPMPO</strong><br />
CB4/SORGAM<br />
Chen et al.,<br />
2006
Chen et al., 2006<br />
Aqueous-Phase SOA
Other Recent <strong>Application</strong>s<br />
•Study <strong>of</strong> dynamics <strong>of</strong> SOA in the SoCAB (Vutukuru et al.,<br />
2006)<br />
• SOA source apportionment in the SoCAB (Ying et al.,<br />
2006; Kleeman et al., 2006)<br />
• SOA study in southern France (high contribution <strong>of</strong><br />
diesel!; Tulet et al., 2006)<br />
• Photochemical formation <strong>of</strong> CO in the eastern US <strong>and</strong> the<br />
SoCAB (Griffin et al., 2006)<br />
• Photochemical modeling <strong>of</strong> peroxy radicals for φ<br />
calculations in New Engl<strong>and</strong> (Griffin et al., 2006)
Hot Off the Press (1) – In-cloud<br />
Chen et al.<br />
poster here!
Hot Off the Press (2) - Alkanes<br />
Jordan et al.<br />
poster here!
Hot Off the Press (3) - Dynamics<br />
Vutukuru et al.<br />
AAAR poster
Example Strengths <strong>and</strong><br />
Weaknesses<br />
Strengths<br />
• Not specific to one set <strong>of</strong> chamber conditions<br />
• Chemical <strong>and</strong> phase specificity<br />
• Appropriate NO x<br />
dependence (though not strong enough)<br />
• A dynamic duo<br />
Weaknesses<br />
• Missing SOA sources (i.e., isoprene, sesquiterpenes,<br />
organic-sulfate interactions including aldehydes, ?, etc.)<br />
• Computationally expensive<br />
• Specificity <strong>of</strong> emissions is somewhat burdensome<br />
• POA <strong>and</strong> vapor pressure characterization<br />
• Biased to SoCAB?
What’s Next?<br />
• Missing chemistry<br />
– Isoprene <strong>and</strong> sesquiterpenes<br />
– Particle-phase/heterogeneous reactions (organicsulfate,<br />
peroxides)<br />
–Low-NO x chemistry<br />
– Ammonia-acid interactions<br />
– Cl-VOC chemistry for application to the MBL
Thanks to…<br />
• My co-authors<br />
• Laura Cottrell, Luke Ziemba, Pieter Beckman<br />
(AMS data)<br />
• Additional collaborators (Meteo France, UCD,<br />
UCR)<br />
• NOAA, EPA, NSF, & EPRI for funding<br />
• The organizers