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Total OH reactivity at Cape Corsica during summer 2013
Nora ZannoniValerie Gros, Roland Sarda-Esteve,
Sebastien Dusanter, Vincent Michoud, Vinayak Sinha
OH reactivity: meaning and importance
CH4
?
Sources Sinks∙OHOzoneSOA
OH budgetUnmeasured/ Unknown species
Total OH reactivity
CO
2
Total OH reactivity: OH loss for reactive compounds in atmosphere
3
Measuring the Total OH reactivity:The Comparative Reactivity Method (CRM)
(Sinha et al., 2008)
• Glass reactor + PTR-MS • OH produced in situ• Pyrrole (m/z 68) reference compound• Competition between pyrrole and ambient reactive compounds
Pyrrole + zero air
Hg lamp N2 dry pump
To PTR-MS
14 cm
3 cm
20x103
18
16
14
12
10
8
6
pyrr
ole
conc
entr
atio
n (c
ps)
1:00 PM 2:00 PM 3:00 PM 4:00 PM 5:00 PM 6:00 PMTime
1)31(
)23(CKp
CC
CCRair
C0 Lamp on
C1Wet N2 in
C2ambient air in
C3
Pyrrole + ambient air
N2 wet
Site of study
Ersa- Cape Corsica
4
5
Cape Corsica monitoring station (42.97°N, 9.38°E, alt 533 m)
6 km 2.5 km
Courtesy of J.Sciare
24/06/13
Installationand tests
01/07/13 08/07/13 13/07/13 16/07/13 05/08/13
Intercomparison with CRM MD
Plant experimentMeasurement campaign
OH REACTIVITY
Goal: (i) Measure reactivity of air masses enriched in anthropogenic compounds and their oxidation products;
(ii) Use missing reactivity as a tool for chemical closure
Total OH reactivity
• Total OH reactivity ranges between CRM LOD up to 20 s-1
•On average 5 s-1 during the whole campaign•Diurnal profile•Peaks when temperature increases
6Zannoni et al., in preparation + poster
20
15
10
5
To
tal O
H r
ea
ctiv
ity (
s-1
)
7/17/2013 7/22/2013 7/27/2013 8/1/2013 8/6/2013
35
30
25
20
Te
mp
era
ture
(°C
) 100
80
60
40
RH
(%)
Total OH reactivity Total OH reactivity_hourly avg
RH Temperature
7
Ancillary gas phase measurementsSpecies group Species nameAVOCs(44)
methane, ethane, propane, n-butane, n-pentane, n-hexane, n-octane, n-nonane, n-undecane, n-dodecane, 2-methylpropane, 2-methylpentane, 2-methylhexane, 2,2- dimethylbutane, 2,2-dimethylpropane, 2,3- dimethylpentane, 2,4- dimethylpentane, 2,2,3-trimethylbutane, 2,2,4-trimethylpentane, 2,3,4- trimethylpentane, cyclohexane, ethylene, propylene, 1-butene, 2-methylpropene, 2-methyl-2-butene, 3-methyl-1-butene, 1,3-butadiene, trans-2-butene, cis-2-butene, 1-pentene, trans-2-pentene, cis-2-pentene, hexene, benzene, toluene, ethylbenzene, styrene, m-xylene, o-xylene, p-xylene, acetylene, 1-butyne, acetonitrile.
BVOCs (7) isoprene, a-pinene, b-pinene, d-limonene, a-terpinene, b-terpinene, camphene. OVOCs (15) acetaldehyde, formic acid, acetone, acetic acid, mglyox, methyl ethyl ketone,
propionic acid, ethyl vinyl ketone, butiric acid, nopinone, pinonaldehyde, methacrolein, methyl vinyl ketone, formaldehyde, methanol.
Others (3) NO, NO2, CO.
11% 39%
16% 34%
BVOCs
AVOCs
othersOVOCs
21% 4% 24%
52%
BVOCs
AVOCs
others
OVOCs
Daytime OH reactivity speciation Nighttime OH reactivity speciation
i
iOHi XkR
Measured vs calculated reactivity
West Marine
West Marine
East (Italy)
East (Italy)North (France)
South SouthTransported air massesorigins
8
20
15
10
5
OH
reac
tivity
(s-1
)
7/17/2013 7/22/2013 7/27/2013 8/1/2013
OH reactivity_measured OH reactivity_calculated OH reactivity_measured_uncertainty OH reactivity_calculated_uncertainty
Significant missing OH reactivity
9
8
6
4
2
0
OH
rea
ctiv
ity (
s-1)
17/07/2013 22/07/2013 27/07/2013 01/08/2013
missing reactivity
20
15
10
5
OH
re
activity (
s-1
)
7/17/2013 7/22/2013 7/27/2013 8/1/2013
OH reactivity_measured OH reactivity_calculated OH reactivity_measured_uncertainty OH reactivity_calculated_uncertainty
West Marine
South
What can explain the missing OH reactivity?
1.4
1.2
1.0
0.8
0.6
0.4
0.2
0.0
mix
ing
ratio
(pp
bv)
17/07/2013 22/07/2013 27/07/2013 01/08/2013
missing MT total MT (PTR-MS) MT speciated
Missing monoterpenes?
10
What can explain the missing OH reactivity?
…In part yes!
apinene camphene bpinene
myrcene
limonene
cineole
camphor
borneol
Rosmarinus officinalis emissions map
Bracho-Nunez et al., 2011
8
6
4
2
0
OH
rea
ctiv
ity (
s-1)
17/07/2013 22/07/2013 27/07/2013 01/08/2013
limonene linalool myrcene ocimene camphor missing reactivity
Hypothetical influence of unmeasured monoterpenes expected for the Mediterranean shrubland based on the missing monoterpenes concentration
11
What can also explain the missing OH reactivity?
Unmeasured OVOC’s? Probably also! Courtesy of Agnes Borbon
Chromatogram 24/07/13 mono and multifunctional carbonyls
0h
3h
6h
9h
12h
15h
18h
21h
12
Take home message(s):
- Total OH reactivity varied between LOD-20 s-1
- Main influences from BVOCs
- Significant missing reactivity during 23-30/07:
-unmeasured MT-OVOCs
-Research question not completely answered: few anthropogenic events and low loadings of anthropogenic pollutants
-Further investigate OVOCs
13
14
OH reactivity in biogenic environments:
High OH reactivity measured in the Mediterranean basin (even at a site not supposed to be “forested”)
Cape Corsica site very complex: budget not constrained, highest influence by BVOC’s…
...what about the OH reactivity at other remote and continental Mediterranean sites?
806040200Total OH reactivity (s-1)
Di Carlo et al., 2004
Ren et al., 2006
Sinha et al., 2008
Ingham et al., 2009
Sinha et al., 2010
Noelscher et al., 2012
Mao et al., 2012
Noelscher et al., 2013
Edwards et al., 2013
Hansen et al., 2014
Charmex 2013
CANOPEE 2014
temperate tropical boreal mediterranean
15
...and you for your attention!
ANY QUESTION?
Acknowledgments:
LSCE: Bernard Bonsang, Cerise Kalogridis, Cyril Vuillemin, Eric Hamonou, Francois Dulac
Mines Douai: Stephane Sauvage, Vincent Michoud, Sebastien Dusanter, Nadine Locoge, Thierry Leonardis,
LAMP: Aurelie Colomb
LISA: Agnes Borbon
16
Diurnal pattern
2500
2000
1500
1000
500
0
Vol
ume
Mix
ing
Rat
ios
(ppt
v)
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24
Hour of Day
Diurnal Pattern of total BVOCs (10-90 % whiskers)
Diurnal pattern of total OH reactivity well resembles the one of total BVOC’s, with a maximum at 15.00
17
12
10
8
6
4
2
0
Tota
l OH
reac
tivity
(s-1
)
1 2 3 4 5 6 7 8 9 10 1112 13 14 15 1617 18 19 20 2122 23 24Hour of Day
Diurnal pattern of total OH reactivity (10-90% whiskers)
Species contributions for each period
18
West Marine
West Marine
East (Italy)
East (Italy)North (France)
South South
15%
20%
21%
44%
BVOCs
AVOCs
others
OVOCs
10%
34%
19%
37%
BVOCs
AVOCs
others
OVOCs 13%
29%
22%
37%
BVOCs
AVOCs
others
OVOCs
10% 41%
16%
33%
BVOCs
AVOCs
others
OVOCs
10% 43%
11%
36%
BVOCs
AVOCs
others
OVOCs
12%
42%
12% 34%
BVOCs
AVOCs
othersOVOCs
BVOC’s relative and absolute reactivity100
80
60
40
20
0
Re
lativ
e c
on
trib
utio
ns
to O
H r
ea
ctiv
ity (
%)
00:0023/07/2013
00:0024/07/2013
00:0025/07/2013
00:0026/07/2013
00:0027/07/2013
a-terpinene a-pinene b-pinene camphene g-terpinene isoprene limonene
100
80
60
40
20
0
Rel
ativ
e co
ntrib
utio
ns to
OH
rea
ctiv
ity (
%)
00:0027/07/2013
12:00 00:0028/07/2013
12:00 00:0029/07/2013
12:00 00:0030/07/2013
a-terpinene a-pinene b-pinene camphene g-terpinene isoprene limonene
8
6
4
2
0
OH
rea
ctiv
ity (
s-1)
16/07/2013 21/07/2013 26/07/2013 31/07/2013 05/08/2013
limonene camphene a-terpinene g-terpinene b-pinene isoprene a-pinene monoterpenes
BVOC Day (%) Night (%)
a-pinene 7.69 20.73
b-pinene 16.49 16.05
limonene 12.03 11.36
camphene 1.48 3.05
a-terpinene 31.08 31.33
g-terpinene 1.28 5.04
isoprene 29.96 12.45
19
Atmospheric dynamics during ChArMEX
20
3228242016
[°C
]
17/07/2013 22/07/2013 27/07/2013 01/08/2013 06/08/2013
100806040
[%]
600400200
0
[W/m
^2]
300
200
100
0
[°]
100
80
60
40
[pp
bv]
1.20.80.40.0
[pp
bv]
12
8
4
[m/s]
86420
[Bq
/m3
] 0.8
0.6
0.4
0.2
[km]
Temperature
WS
RH
Radon_activity
isoprene Ozone
Solar Irradiance
Wind direction
BL height
What can explain the missing OH reactivity?
OVOC’s? Probably also!
West (>36 h of processing)
South
North east (12-18h of processing)
North west
West South North East North-West
Courtesy of Vincent Michoud21
OH reactivity from gas phase measurements
22
Instrument Measured species
GC-FID AVOC’s C2-C13
a-pinene, b-pinenePTR-TOF-MS CH3OH,CH3CN, CH3CHO, HCOOH,
CH3COOH, CH3COCH3, MVK+MACR, MGLYOX, MEK, CH3CH2COOH, EVK, CH₃CH₂CH₂-COOH, nopinone, pinonaldehyde
GC-MS Limonene, camphene, a-terpinene, g-terpinene
NOx analyser
NO, NO2
AEROLASER (Hantzsch method)
HCHO
Picarro CH4, CO
i
iOHi XkR