6
ꢂ3 25
yields an estimated
photolytic lifetime of CHF
2
CHO at EUPHORE and reported
ꢂ5 ꢂ1
concentration of 10 radicals cm
lifetime for C 2x+1CHO of around 20 d. The photolysis
a value of the photolytic rate coefficient of 2.82 ꢁ 10
s
x
F
with an estimated quantum yield for photodissociation of 0.30.
lifetime under atmospheric degradation of these aldehydes was
found to be close to one day and hence the dominant loss
process for the fluoroaldehydes in the gas phase will be by
photolysis. When a soluble species is formed fairly uniformly
in the atmosphere, which will be the case for short chain length
The photolysis lifetime for CHF CHO obtained from this work
2
of about 10 h is more in line with the lifetimes determined in the
6
present investigation on fluoroaldehydes. Chiappero et al. have
recently determined the quantum yields for photodissociation
of CF
lysis at 308 nm in 700 Torr of N
CF CHO), 0.08 (C CHO) and 0.04 (CF
used to estimate the rates of photolysis of CF CHO, C
CHO, C CHO, CF CH CHO and CF (CF CH
within the troposphere. The calculated photolytic lifetimes
for C F
3
CHO, C
4
F
9
CHO and CF
3
CH
2
CHO following photo-
. The values of 0.17
CH CHO) were
CHO,
CHO
x
C F2x+1CHO, the average lifetime for uptake into cloud
2
droplets is of the order of 15–20 d and hence this loss process
will only be a minor degradation pathway. It is concluded
from the available data that the major atmospheric removal
pathway for fluoroaldehydes will be by photolysis and that
(
3
F
4 9
3
2
3
2 5
F
C
3
F
7
F
4 9
3
2
3
2
)
5
2
x
under low NO conditions this pathway may be a source of
CHO were o2 d in reasonable agreement with
2x+1
fluorinated carboxylic acids in the troposphere.
x
the experimental photolysis lifetimes found in this study under
atmospheric conditions. The lifetimes estimated for
C F CH CHO of 10–15 d are in line with the value of
x 2x+1 2
Acknowledgements
approximately 10 d found experimentally at EUPHORE for
4
CF CH CHO by Sellevag et al.
3 2
We acknowledge The Telomer Research Program, the French
National Programme for Atmospheric Chemistry (LEFE-
´
n CEAM
CHAT) and EUROCHAMP for support. Fundacio
Conclusions and atmospheric implications
is supported by the Generalitat Valenciana and Fundacion
´
BANCAIXA.
x
Reaction of OH with C F2x+1CHO leads to the formation of
the C F2x+1C(O)O2 radical, which in the presence of NOx
x
produces the corresponding fluoroalkyl radical. Subsequent
stepwise degradation of these radicals eventually leads to the
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1
24
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1
1
1
x 2
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suggested for the short chain fluorinated hydrates.
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F2x+1C(O)OH in a similar manner to that
x
F
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estimated from the data obtained in this investigation. Using
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the averaged rate coefficients k(OH + C F2x+1CHO) =
x
3
ꢂ1 ꢂ1
6
ꢁ 10ꢂ13 cm molecule
s and a global averaged OH
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