air pollution research using chemical mass …air pollution research using chemical ionization mass...
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Air Pollution Research Using Chemical Ionization Mass Spectrometry (CIMS)Spectrometry (CIMS)
Jun Zheng, Ph.D.Jiangsu Key Laboratory of Atmospheric Environment
Monitoring and Pollution Control (AEMPC)Nanjing University of Information Science & Technology
Oct 26, 2012 Nanjing
Soft IonizationHigh Sensitivityg yHigh SelectivityVersatilityVersatility
Ion Chemistry: R(+/‐) + A P(+/‐) + BR(+/ ) + A P(+/ ) + B
Huey, L. G. (2007), Mass Spectrom. Rev., 26(2).Huey, L. G. (2007), Mass Spectrom. Rev., 26(2).
Applications of CIMS in Atmospheric h dChemistry Study
Fi ld t t f• Field measurements: trace gases, free radicals…
• Laboratory experiments:– Kinetics
– Uptake coefficient
– Chamber simulations…
1. Proton‐Transfer‐Reaction Mass ( )Spectrometry (PTR‐MS)
H3O+∙(H2O)n + R RH+ + H2O(n+1), (R = VOCs)3 ( 2 )n 2 (n+1), ( )
where n = 0, 1 and corresponding rate constants are k’0 and k’1, respectively.
[R] = [RH+] / (k’0[H3O+] + k’1[H3O+∙H2O])[R]t.
Ionicon Analytik Inc.
PTR‐MS Field Measurements
Toluene Styrene C2‐BenzeneToluene Styrene C2-Benzene
C3‐Benzene Methanol AcetaldehydeC3-Benzene Methanol Acetaldehyde
Atmos. Chem. Phys. 2009, 9, 467‐481.
VOCs Source Apportionments
VOC NOx
SO2 NOSO2 NOz
PTR‐MS for HCHO Measurements
H3O+ + HCHO H+HCHO + H2O
Zheng et al., Atmos. Environ. 2012, Accepted
Mobile VOCs Measurements
Case1: before vehicle control Case2: vehicle control before OlympicsCase3: Olympics Case4: between Olympics and Paralympics Case5: ParalympicsCase5: ParalympicsCase6: After vehicle controlCase7: National days
Atmos. Chem. Phys. 2009, 9, 8247‐8263.
2. Ion Drift – CIMS2. Ion Drift CIMS
•Bipolar detector•Well‐controlled ion‐molecular reactionC bl f d l t i•Capable of declustering
ID‐CIMSHNO3 Detection: SF6 + e‐ SF6‐
SF6‐ + SiF4 SiF5‐ + SF56 4 5 5SiF5‐ + HNO3 SiF5‐HNO3
N O Detection:N2O5 Detection: CF3I + e‐ I‐ + CF3I‐ + N2O5 NO3
‐ + INO2
ID‐CIMS
Lei, W. F., R. Y. Zhang, X. X. Tie, and P. Hess (2004), Chemical characterization of ozone formation in the Houston‐Galveston area: A chemical transport model study, J. Geophys. Res., 109(D12), D12301, 10.1029/2003jd004219
ID‐CIMS
HONO Detection: SF + e‐ SF ‐SF6 + e SF6SF6‐ + HONO HONOF‐ + SF5
(ppb
v)
30
40 ID-CIMSU. Miami LOPAP
ppbv)
HO
NO
(
10
20
HONO (p
CST
5/23 10:45 5/23 10:50 5/23 10:55 5/23 11:000
ID‐CIMS2000
ptv)
1500
2000
pptv) 2009 In Houston, Texas
HO
NO
(p
500
1000
HONO (p
CST4/20 00 4/27 00 5/4 00 5/11 00 5/18 00 5/25 00 6/1 000
2009 In Shanghai, China
3. Atmospheric Pressure IonizationID‐CIMS
Schematic diagram of the AP‐ID‐CIMS.
Chemical Scheme: NO - (HNO ) + H SO HSO - (HNO ) + HNO n = 0 1 2 Chemical Scheme: NO3 (HNO3)n + H2SO4 HSO4 (HNO3)n + HNO3, n = 0,1,2… Quantification: [H2SO4] = [HSO4
-HNO3] / (k∆t[NO3-HNO3])
By introducing a 4-in ID inlet for sampling, the wall losses can besignificantly decreased.
Well suited for the detection of ultra-trace atmospheric components, such asgaseous sulfuric acid (the detection limit as low as 0.01 ppt).
API‐ID‐CIMS
2008 Beijing2008 Beijing
API‐ID‐CIMSNucleation Events During CAREBeijing 2008
080717
4.E+04
5.E+04
6.E+04
(/cm
3 ) 2 .0E+06
2.5E+06
3.0E+06
H2 SO
4
N uc leation
H2SO4
Nucleation Events During CAREBeijing 2008
0.E+00
1.E+04
2.E+04
3.E+04
00 04 08 12 16 20 00T ime
N-
Nuc
(
0 .0E+00
5.0E+05
1.0E+06
1.5E+06
(/cm
3)
JT JT0([H2SO4 ] )a a ( RH )b b ( [NH3] )c c
a = 2.17 in Beijing, indicating 2 H2SO4 molecules were involved in the nucleation
JT JT ([H2SO4 ] 0
) (RH0
) ([NH 3]0
)
McGraw, R., and Zhang, R. Y., J. Chem. Phys., 128, 2008.
a 2.17 in Beijing, indicating 2 H2SO4 molecules were involved in the nucleation
Zheng, J. et al., Atmos. Chem. Phys., 11, 2011.
4. High Resolution Time of Flight‐CIMS4. High Resolution Time of Flight CIMS
HRToF‐ID‐CIMS
Aerodyne HRToF‐CIMS
O2+
CH5NH+
Amonia and Amines in Nanjing 2012
CH5N H
AcknowledgementsAcknowledgements
• Prof Renyi ZhangProf. Renyi Zhang
• Prof. Mindong Chen
f i i Ch• Prof. Jianmin Chen
• Prof. Min Hu
• Prof. Yan Ma
• Prof Lin WangProf. Lin Wang
Thank you for your attention!