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![Page 1: Characterization of gas and particle emissions in the greater Houston area using the Aerodyne mobile laboratory Ezra Wood, Scott Herndon, Luwi Oluwole,](https://reader036.fdocuments.in/reader036/viewer/2022070306/5519da3a550346d67b8b4614/html5/thumbnails/1.jpg)
Characterization of gas and particle emissions in the greater Houston area using the Aerodyne mobile laboratory
Ezra Wood, Scott Herndon, Luwi Oluwole, Simon Albo
T. Onasch1, E. Fortner1, J. Jayne1, J. Wormhoudt1, P. Massoli1, C. Kolb1, H. B. Lee2, M. Zavala3, L. T. Molina3, and W. B. Knighton4
6/21/2011FLAIR workshop, Austin TXAcknowledgments: TCEQ
Aerodyne Research, Inc., Harvard University, Molina Center for Energy & Environment,Montana State University
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CO, NO2, C2H4, HCHO (QC-TILDAS)
aromatic VOCs, 1,3-butadiene, OVOCs (PTR-MS/NO+MS)
O3, NO, CO2, SO2
PAN (GC), VOCs (canisters) (UH)
Size and chemically-speciated PM (Aerosol Mass Spectrometer) Particle number (CPC)Black Carbon (MAAP), extinctionPM size distribution (SMPS)
Wind speed/directionActinic fluxGPS position
Instrumentation
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Goal: Conduct measurements that support emissions characterization • quantification (pounds/hr) • location identification
Mobile sampling: Texas City, Mont Belvieu, Ship Channel
Stationary sites:Texas CityMont BelvieuU. Houston
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C2H4 and HCHO mapping in Mont Belvieu
WIND
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Quantification of emissions from “traditional” combustion source: fuel-based emission factors
Ship Channel May 28, 2009
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Carbon balance method
58 g NOx/kg fuel
18 ppb NOx / ppm CO2
x total fuel consumptionEmission
Inventory
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Ship emission factors
Plume time
Vessel name/type
NOx
g/kg fuel
dOx/dNOx
HCHOg/kg
CO g/kg
SO2
g/kg
10:04 Izumo Princess 58 0.1
10:26 Vega Spring 61 21
10:59 Odfjell Seachem 54 0.06 12 25
11:04 UBC Bremen? 80 0.08
11:05 Eitzen Chemical 50 0.11 0.19 48 34
11:17 Leyte Spirit 89 0.07 0.17 10 37
11:24 tug/ferry 55 0.12 0.40 12 1.2
11:36 tug/ferry 30 0.09 – 0.15
0.13
11:54 Petropavlovsk 44 0.07 0.16 17 30
Williams MSDc 61.5 0.15 11.0 6.3
Williams SSDb 79.6 0.15 11.8 27.8
HONO/NOx: 0.7 to 1.4% (similar to on-road diesel vehicles)-based on comparison with UCLA iDOAS HONO/NO2 ratios
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• Destruction Removal Efficiency (DRE) vs. fuel-based emission factors• Assumption that most C ends up as CO, CO2 not valid
Flares: use carbon balance method …
…with a few complications
TCEQ’s Comprehensive Flare StudySeptember 2010:
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Emissions observed with ARI mobile laboratoryduring FLAIR 2009:
1) Useful correlations between combustion tracers (CO, CO2) and VOCs
2) Obvious fugitive emissions
3) Unclear – no obvious correlation between combustion tracers and VOCs, but can’t rule it out
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1. (Useful VOC-COx correlations) Flare Emission Capture from Mobile Laboratory
Known Plant Flare P-200
Mobile Lab Maneuvered Here
Prevailing Wind
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Flare Emission Capture from Mobile Laboratory
Known Plant Flare P-200
Prevailing Wind
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Flare Emission Capture from Mobile Laboratory
Known Plant Flare P-200
Prevailing Wind
Carbon balance methods with a guess about vent gas composition:
DRE = 94% (88% - 96%)
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Large ethene leak, Winfree Rd
·Localized (<10 m)
· no CO/CO2/NOx3304
3303
UT
M N
orth
ing
(km
)
317316
UTM Easting (km)
2001000
C2H4 (ppbv)
2) obvious fugitive emissions / non-combustion source
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(5/19/2009, Mt. Belvieu)2) obvious fugitive emissions / non-combustion source
Unlit flare
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3) No obvious correlation between combustion tracers and VOCs, but can’t rule out low DRE flare vs. leak
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3) No obvious correlation between VOCs and COx – low DRE flares?
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The Aerodyne Inverse Modeling System (AIMS)
• Given knowledge of the wind history, determine emission source parameters that when applied in atmospheric dispersion model yield pollutant concentration profiles that are most consistent with observed profiles
Driver
SCIPUFF SCIPUFF TL/AdjointMinimizationalgorithm
• Obs. Data (MET, Sensors)
Aerodyne Research, Inc.
# of sources,Emission rates, Locations, Start and End times.
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WIND15 pounds/hr benzene sourceidentified by inversion model
Inversion model results
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Stationary data: SO2 “upwind” from courthouse site (TC)
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HCHO: same spatial signature filtered day/night
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Consistent HCHO/SO2 ratio
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HCHO: Primary vs. secondary?
C2H4 + OH → → 1.43 HCHO
42
42
1)(43.1
)(ln
][HCOHk
tHC
tHCHO
OHt
photochemical age (OH exposure):
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Primary HCHO in Texas City?
slope implies [OH] = 2 ×107 to 4 × 107 molecules/cm3
→ evidence for primary HCHO
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Primary HCHO from Chevron?
Slope and transit time imply [OH] = 1.33 × 106 molecules cm-3 at 07:20 CST
5/21/2009 → no evidence for primary HCHO
C2H4 (ppb)
HC
HO
(p
pb)
Slope = 0.02
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80400
1,3-butadiene (ppb)
WIND
1,3-butadiene mapping (Ship Channel)
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1,3-butadiene, styrene
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Summary• Mobile measurements useful for locating and quantifying emission sources
• Rich dataset:Marathon flare DREShip emission factorsWinfree road Ethylene leakPrimary HCHO emissions from Texas City facililtyEthylene, propylene emission from Chevron (Mont Belvieu)1,3-butadiene, styrene from Goodyear
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back-up slides
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Photochemistry
80
60
40
20
0
prop
ene
ppb
5:08 AM5/21/2009
5:12 AM 5:16 AM 5:20 AM
CST
300
200
100
0
C2H
4 pp
b
460
440
420
400
CO
2 pp
m
2000
1500
1000
500
0
CO
120
80
40
0
NO
x (p
pb)
0.8
0.6
0.4
0.2
0.0
P(H
Ox)
ppt
/s
12
8
4
0
m/z
57
bute
ne
P(HOx) from O3 + eth, prop, butenes
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P(OH) = L(OH)
][
]][[]][[][ 233
iXiOH
OHalkenesOSS Xk
NOHOkYalkenesOkOH
Total OH loss rate = 47.3 s-1, and is dominated by reaction with C2H4.This yields an OH concentation of 1.6 × 105 molecules/cm3. Since the HO2 + NO term is obviously not zero, this number should be considered a lower limit to the true OH concentration. This value is likely higher than the [OH] in non alkene plume air considering the time of day (06:12 local time). Further analysis will address the likely range of values for the HO2 + NO term.