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Near-Infrared Photochemistry of Atmospheric Nitrites Paul Wennberg, Coleen Roehl, Geoff Blake, and...
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![Page 1: Near-Infrared Photochemistry of Atmospheric Nitrites Paul Wennberg, Coleen Roehl, Geoff Blake, and Sergey Nizkorodov California Institute of Technology.](https://reader037.fdocuments.us/reader037/viewer/2022100307/5a4d1b6c7f8b9ab0599b39c1/html5/thumbnails/1.jpg)
Near-Infrared Photochemistry of Atmospheric Nitrites
Paul Wennberg, Coleen Roehl, Geoff Blake, and Sergey Nizkorodov
California Institute of Technology
Ross Salawitch, Geoff ToonJet Propulsion Laboratory
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Stratospheric Ozone Photochemistry
Courtesy NASA Goddard
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HO2 + O3 OH + O2 + O2
OH + O3 HO2 + O2
O3 + O3 O2 + O2 + O2
Catalytic destruction of Ozone by HOx
Wennberg et al., Science, 266, 398, 1997
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HOx PhotochemistrySources:
O3 + hν (< 314 nm) O (1D) + O2 O (1D) + H2O 2 OH
Sinks (Direct):OH + HO2 H2O + O2
Sinks (Indirect):OH + NO2 HONO2
OH + HONO2 H2O + O3
HO2 + NO2 HO2NO2
OH + HOONO2 H2O + O2 + NO2
OH HO2
NO, O3
O 3
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Tro
posp
heri
c O
3 Pr
oduc
tion OH + CO CO2 + HO2
HO2 + NO NO2 + OH NO2 + hν (< 450 nm) NO + O
O + O2 O3 Net: CO + 2 O2 O3 + CO2
More O 3 production
Less O3 production
Jaegle et al., J. Geophys. Res., 105, 3877-3892, 2000.
O2
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The Color of Sunlight
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Peroxy Nitric Acid (HO2NO2)Donaldson et al. (1997) proposed that dissociative excitation of OH vibrational overtones in H2O2, HNO3, and HO2NO2 is an additional source of OH in the atmosphere
Wennberg et al. (1999) found unknown photochemical source of OH in the mid-latitude stratosphere with photolysis > 650 nm and suggested HO2NO2 as the carrier
D. J. Donaldson et al., Geophys. Res. Lett. 24, 2651 (1997)
P. O. Wennberg et al., Geophys. Res. Lett. 26, 1373 (1999)
Solar Flux
Wavelength [nm]1000
Sola
r Fl
ux [P
hoto
ns c
m-2
s-1 n
m-1
]
1012
1013
1014
1015
SZA = 0ºSZA = 86º
300 400 500 700
Near IR solar flux is orders of magnitude higher than UV flux
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Approach
HO2NO2 + h HO2 + NO2
HO2 + NO OHOH + NO2
1. IR-photodissociation2. Conversion into OH3. Detection of OH
Vibrational Dissociation Spectroscopy
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Experiment
• Direct overtone pumping of CH / OH stretches in PAN / PNA / HOONO• Chemical conversion of photodecomposition products into OH radicals• LIF detection of OH in a single photon counting regime
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Wavenumber [cm-1]6000 7000 8000 9000 10000
31
21
21+3
1+23
Sample action and FTIR spectra of PNA
D0
Action Spectra
• Different relative band intensities in FTIR and action spectra • Dissociation quantum yields determined by comparing spectra• Initial internal energy responsible for dissociation below D0
absdissPNAaction σφρ S
absPNAFTIR σρ S
(21, 240 K)=14%
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Phot
odis
soci
atio
n C
ross
Sec
tion
(cm
2 mol
ecul
e-1 c
m-1
)
10-20
10-19
10-18
Qua
ntum
Yie
ld
0.1
1
Dissociation Cross-Sections and Quantum Yields
10-21
10-20
10-19
0.1
1
1000/T (K-1)3.4 3.6 3.8 4.0 4.2 4.4
10-22
10-21
10-20
0.01
0.1
2+
2
+2
Temperature-Dependent Action Spectra of PNA
Wavenumber [cm-1]650067507000725097501000010250
Inte
nsity
[a.u
.]
31
224 K
244 K
283 K
21
• Relative band intensities in action spectra of PNA are T-dependent
• {diss(31) = 1} Absolute photodissociation cross sections and quantum yields for other bands
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MkIV HO2NO2 Observations
Frequency (cm-1)
Inte
nsity
R
esid
ual (
%)
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OH + NO2 ??• The Reaction of OH with NO2 is among the
most important reactions in Earth’s atmosphere. By sequestering both HOx and NOx it essentially shuts down reactive photochemistry.
• It is assumed by all models that the only product formed is nitric acid
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Part II. HOONO
• Suspected intermediate of the OH + NO2 association reaction
• Proposed intermediate of liquid phase reactions of peroxynitrite ion (ONOO-)
• Observed in rare-gas matrices in 1991 Cheng et al. J. Phys. Chem. 95, 2814 (1991)
• Extensively studied by theory– At least three stable conformers– Bound by 19 kcal/mol
• Never observed in the gas phase
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HOONO Atmospheric Significance Reaction Intermediates
HO + NO2
HOONO-19
(3 isomers)
HONO2
+7
-48
0
HO2 + NO
HONO2 HOONOIrreversible Reversible
Removal of HOx and NOx
No effect
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Produce HOONOHOONO directly in the gas-phase
H2 + μwave discharge 2 H
H + NO2 OH + NO
OH + NO2 + M HNO3 + M
OH + NO2 + M HOONO OONO + M
Photofragment:
HOONO OONO + hν OH + NO2
Detect OH by LIF
Preparation
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Observed Spectra
Stronger peaks assigned to HOONO 21 overtones and combination bands
Assignment for weaker bands remains ambiguous
Intensities affected by photodissociation dynamicsD0
21
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Observed HOONO Yield
• HOONO lifetime unknown lower limit• Different conditions incomparable• Higher yield expected for upper troposphere
This work(253 K, 20 Torr)
Burkholder et al.
Dransfield et al.
Hippler et al.
> 5 3 % (after 300 ms)
< 5 % < 10 % Unpublished
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Future Projects• Photochemistry of reaction intermediates
– HOCO– HOOOCl– CH3OONO
• Chemistry and kinetics of weakly-bound molecules– CH3OONO2
– CH3C(O)OONO2– HOONO– HO2NO2
• UV photodissociation spectroscopy of atmospheric molecules– CH3OOH– HO2NO2
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Thanks
• Funding by NASA and NSF• Support for Sergey Nizkorodov (just
appointed assistant professor of chemistry UC-Irvine) from the Dreyfus foundation.
• You for your attention!