snowpack photochemistry - focused on the pan(peroxyacetyl nitrate) in summit greenland
DESCRIPTION
Snowpack photochemistry - focused on the PAN(Peroxyacetyl Nitrate) in Summit Greenland. 19 April 2004. Saewung Kim. Is (Ant)Arctic region photochemically DEAD?. Synthetic image (Apr. 7 10am EST). Probably YES - too remote - low solar intensity. It seems still alive!. - PowerPoint PPT PresentationTRANSCRIPT
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Snowpack photochemistry - focused on the PAN(Peroxyacetyl Nitrate)
in Summit Greenland
Saewung Kim
19 April 2004
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Is (Ant)Arctic region photochemically DEAD?
Probably YES - too remote - low solar intensity
Synthetic image(Apr. 7 10am EST)
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It seems still alive!
Species Predicted by gas phase chemistry
Actual Measurement
HCHO 70 pptv 200 pptv
CH3CHO 40 pptv 80 pptv
NOx 1 pptv 25 pptv
HONO 1 pptv 20 pptv
HOx 0.9 pptv 3.7 pptv(Domine and Shepson, 2002)
Summit, Greenland region
-Measurement data could not be explained by gas phase only prediction-The difference of each species seems non-linear the difference is not just come from the numerical calculation. We can assume some other chemical mechanism would be going on the snowpack region.
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What is the invisible hand?
HETEROGENEOUS chemistry insideof the snowpack!
(Domine and Shepson, 2002)
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Snowpack photochemistry
Red arrow : Inside of snowpackGreen arrow : Gas phase Chem.
-Nitrate photo dissociationNO3
-+h NO2- + O (3P)
h NO2- + O-
-O- ChannelO- + H+ OHNO2
- + H+ HONONO2
- + h NO + O-
-O(3P) ChannelO(3P) + O2 O3
O(3P),OH,O3 + DOM Carbonyl Compound
(Domine and Shepson, 2002)
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Is this mechanism really big deal?? I
Sure!! in two aspects
First nearly 50% of N Hem.is covered by snow(Robinson et al., 1993)
The global budget of photochemically active species would be significantly affected
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Is this mechanism really big deal?? II
If ion species is perturbed by the heterogeneous mechanism, what we understand of the paleo-environment reconstructed by icecore interpretation would be wrong.
Ice core research homepagehttp://www.secretsoftheice.org/icecore/
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Importance of PAN in arctic environment I
-PAN in the snowpack environment will be studied
◉ PAN is the product of peroxy radical came from VOC and NOx CH3CH(O)OO + NO2+M CH3CH(O)OONO2+M
CxHy NOx HNO3
PAN
PAN
NOx HNO3
Long-range transportat low T
Deposition
ThermalDecompo.
NOx Source Region Remote Region
CH3CHO + OH -> CH3CO + H2OCH3CO + O2 + M -> CH3C(O)OO + M
CH3C(O)OO+NO2+M -> PAN + M
PAN -> CH3C(O)OO + NO2
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Source of nitrate ion in the snowapck HNO3 : Easily soluble. But concentration is too low to explain the high concentration of nitrate ion in the snowpack.
Then what is the most abundant reactive nitrogen species (NOy) in arctic environment - PAN
PAN is most abundant species in the Arctic region, so the mechanism for dissolution to snow of PAN have been studied but the processes are not clearly understood (Ford et al, 2002)
Simple box-model for PAN in the Summit Greenland region-Understand of PAN budget in the Arctic region-How much of PAN could contribute for nitrate in the snow
Importance of PAN in arctic environment II
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Box model-step I No icepack chemistry
Snowpack
Boundary layer
PAN(133pptv)
Long range transport (T)
Thermal decomposition(lifetime 76day at 255K)
Adsorption to snow(lifetime 1.3 day at 255k)
Wang et al(1998)- global Chem-Transport model
July August
133ppt 132ppt
Steady-State Assumption
d[PAN]/dt = (Long range transport) – (Thermal decomp.) – ( Ads. to snow) = 0
(Long range transport) = 1.1910-3 ppt/sec
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Box model-step II With icepack chemistry
Snowpack
Boundary layer
PAN(75pptv)
Long range transport (T)
TD
ADS
Production from snowpack2.0 10-2ppt/sec
Missing Sink
Ford et al(2002)-Measured PAN: 74pptv-Production from snowpack : 2.0X10-2 ppt/sec
d[PAN]/dt = (Long range transport) – (Thermal decomp.) – ( Ads. to snow) +(Production from snowpack) -(Missing sink) = 0
(Deposition) = 1.1910-3 ppt/sec
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Deposition velocity of PAN based onbox-model calculation
Snowpack
Boundary layer = 100m(Helmig et al,2002)
-Deposition velocity : how fast molecules will be deposited at given flux and concentration.
(column height) = (boundary layer height)=100 m
Calculated result = 3 cm/sec
Huge value compared with HNO3 deposition velocity 0.5 cm/sec(Seinfeld and Pandis, 1997)
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Summary and conclusion
-Snow covered region in high latitude could be important role in global perspective photochemistry
-PAN is the most abundant species in Summit Greenland region, and also important NOy species in other (Ant) Arctic environment.
-PAN could be role of the dominate nitrate source in Greenland region from the box model.
-More study is needed specific physical-chemical mechanism of PAN dissolution on ice.