transfer is suggested to be the prevailing mechanism with the
para-substituted phenols considered in the regression line.
both anions as well as aromatic compounds including the
substituted phenols become essentially independent of the
Gibbs free energy of the reaction. This indicates electron
transfer as the dominant mechanism. On the other hand for
ꢂ1
4
. Environmental aspects
reactions with DG
R
4 ꢂ50 kJ mol
the observed rate
The NO radical is recognised as playing an important role in
3
night-time atmospheric chemistry. It has also been established
that, since the industrial revolution, the tropospheric abun-
dances of the precursors of NO
increasing as a result of anthropogenic activities. Thus, the
coefficients are not due to concerted electron transfer only.
Finally, it was observed that in ortho-substituted phenol
steric effects plays a decisive role whereas electronic effects
are responsible for the reactivity of para-substituted phenols.
3 2 3
, i.e. NO and O , have been
abundance of NO
have increased.
Following the suggestion that NO
carbons, the reactivity of NO towards naturally occurring and
3
anthropogenic atmospheric trace gases has been investigated.
Although aromatic compounds such as benzene or toluene
3
and its impact on the troposphere must also
might react with hydro-
References
3
1
2
3
4
5
H. B. Singh, Composition, Chemistry, and Climate of the Atmo-
sphere, VNR, New York, 1995.
B. J. Finlayson-Pitts and J. N. Pitts, Jr., Chemistry of the Upper
and Lower Atmosphere, Academic Press, San Diego, 2000.
J. H. Seinfeld and S. N. Pandis, Atmospheric chemistry and physics,
J. Wiley & Sons, Toronto, 1998.
J. E. Stern, R. C. Flagan, D. Grosjean and J. H. Seinfeld, Environ.
Sci. Technol., 1987, 21, 1224.
Eurotrac II CMD (Chemical Mechanism Development) – Final
Report 2003, eds. U. Schurath and K.-H. Naumann, Springer,
Munich, 2003.
react slowly with NO
with a variety of compounds and the results obtained in this
work confirm the high reactivity of NO towards organic polar
compounds such as substituted phenols.
3 3
, NO has been shown to react rapidly
3
Furthermore, it was observed under the experimental
conditions applied in this work that phenols bearing an
electron-donating group, such as hydroxyphenols, cresols and
6
7
J. U. White, J. Opt. Soc. Am., 1946, 42, 285.
H. Herrmann and R. Zellner, Reactions of NO -Radicals in
3
methoxyphenols, react with NO exclusively via H-abstraction
3
Aqueous Solution in N-Centered Radicals, ed. Z. B. Alfassi, Wiley,
New York, 1998, p. 291.
with the formation of the corresponding substituted phenoxy
radical and a molecule of HNO . Hence, the gas phase con-
3
8
9
0
1
Th. Umschlag, R. Zellner and H. Herrmann, Phys. Chem. Chem.
Phys., 2002, 4, 2975.
P. Barzaghi and H. Herrmann, Phys. Chem. Chem. Phys., 2002,
version of aromatic compounds, such as benzene, toluene and
anisole, which produces the corresponding phenols, might lead
to an acidification of the tropospheric aqueous phase in the
continental area as a consequence of the fast reaction of
4, 3669.
1
1
H. Herrmann, M. Exner, H.-W. Jacobi, G. Raabe, A. Reese and
R. Zellner, Faraday Discuss., 1995, 100, 129.
R. Bosque and J. Sales, J. Chem. Inf. Comput. Sci., 2003, 43, 637.
phenols with NO
ents like –CN, –NO
3
in aqueous solution. Deactivating substitu-
cause a decrease in the rate constants in
2
12 O. Ito, S. Akiho and M. Iino, J. Phys. Chem., 1989, 93, 4079.
13 T. Del Giacco, E. Baiocchi and S. Steenken, J. Phys. Chem., 1993,
aqueous solution in both mechanisms, in H-atom abstraction
reactions as well as in electron-transfer reactions. Therefore
these reactions might be of minor importance for tropospheric
cloud and aerosol chemistry.
9
7, 5451.
1
1
4
5
G. F. Pedulli, M. Lucarini and P. Pedrielli, in Free Radicals in
Biology and Environment, ed. F. Minisci, Nato ASI Series, Kluwer
Academic Publishers, Dordrecht, 1997, p. 169.
K. A. Connors, Chemical Kinetics – The Study of the Reaction
Rates in Solution, VCH Publishers Inc., New York, 1990.
H. Herrmann, Chem. Rev., 2003, 103, 4691.
G. V. Buxton, C. L. Greenstock, W. P. Helman and A. B. Ross,
J. Phys. Chem. Ref. Data, 1988, 17, 513.
M. Roder, L. Wojnarovits and G. Foldiak, Radiat. Phys. Chem.,
5. Summary and conclusions
1
1
6
7
In this work, a number of rate constants for the reaction of
NO with substituted phenols in aqueous solution were deter-
3
1
8
9
mined. The predominant number of kinetic parameters was
determined for the first time and hence increases the kinetic
database now available and can be used to implement existing
1990, 36, 175.
E. J. Land and M. Ebert, Trans. Faraday Soc., 1967, 63, 1181.
1
20 N. Getoff and S. Solar, Radiat. Phys. Chem., 1986, 28, 443.
21 R. S. Shetiya, K. N. Rao and J. Shankar, Indian J. Chem., Sect. A,
57,58
models
for a better understanding of tropospheric multi-
1
976, 14, 575.
phase chemistry. However, the potential user of the kinetic
data and the correlations has to be aware of the uncertainties
derived from rate constants obtained under conditions which
may not be typical for the tropospheric aqueous phase
throughout.
2
2
2
3
M. Ye and R. H. Schuler, J. Liq. Chromatogr., 1990, 13, 3369.
O. S. Savel’eva, L. G. Shevchuk and N. A. Vysotskaya, Zh. Org.
Khim., 1972, 8, 283.
2
4
J. Feitelson and E. Hayon, J. Phys. Chem., 1973, 77, 10.
25 P. O’Neill and S. Steenken, Ber. Bunsenges. Phys. Chem., 1977,
81, 550.
The reactivity of NO turned out to be complex and hence
3
2
2
6
7
B. Cercek and M. Ebert, Adv. Chem. Ser., 1968, 81, 210.
G. E. Adams, J. W. Boag, J. Currant and B. D. Michael, in Pulse
Radiolysis, eds. M. Ebert, J. P. Keene, A. J. Swallow and J. H.
Boxendale, Academic Press, New York, 1965, p. 131.
complicated to model, as both thermochemical, molecular and
structural effects appear to be important in determining the
rate at which NO reacts. Therefore, it is also important to
3
study reactions which might not be directly relevant for tropo-
spheric chemistry but lead to mechanistic insights.
The results presented here improved the knowledge on these
reactions. For some compounds considered in this study it was
possible to describe the observed rate constants in view of a
single mechanism (H-ABS) acting during the oxidation pro-
cess. For these compounds a correlation (eqn. (2)) was pro-
vided for the prediction of second-order rate constants for the
2
8
P. Neta and L. M. Dorfman, Adv. Chem. Ser., 1968, 81, 222.
29 G. W. Burton and K. U. Ingold, Acc. Chem. Res., 1986, 19, 194.
30 J. A. Howard and K. U. Ingold, Can. J. Chem., 1963, 41, 2800.
31 G. W. Burton and K. U. Ingold, J. Am. Chem. Soc., 1981, 103,
6
472.
3
2
3
G. W. Burton, T. Doba, E. L. Gabe, L. Hughes, F. L. Lee,
L. Prasad and K. U. Ingold, J. Am. Chem. Soc., 1985, 107, 7053.
H. A. Zahalka, B. Robillard, L. Hughes, J. Lusztyk, G. W.
Button, E. G. Janzen, Y. Kotake and K. U. Ingold, J. Org.
Chem., 1988, 53, 3739.
3
3
reaction of NO with substituted phenols reacting by H-
abstraction mechanism. The correlation obtained here covers
a lack in the literature and is in general agreement with
34 J. A. Howard and J. C. Scaiano, in Radical Reaction Rates in
Liquids, ed. S. Fischer, Springer-Verlag, Berlin, 1984, vol. 13, Part d.
35 D. V. Avila, K. U. Ingold and J. Lusztyk, J. Am. Chem. Soc.,
7
previous studies. The contribution of the electron transfer
1993, 115, 466.
D. V. Avila, K. U. Ingold, J. Lusztyk, W. H. Green and D. R.
on the rate coefficients for the reactions of NO
tuted phenols in aqueous solution was investigated and
3
with substi-
3
6
Procopio, J. Am. Chem. Soc., 1995, 117, 2929.
37 L. Valmigli, J. T. Banks, K. U. Ingold and J. Lusztyk, J. Am.
Chem. Soc., 1995, 117, 9966.
4
compared to former studies. The model shows that for
7
ꢂ1
DGR o ꢂ50 kJ mol the rate constants for the reaction with
T h i s j o u r n a l i s & T h e O w n e r S o c i e t i e s 2 0 0 4
P h y s . C h e m . C h e m . P h y s . , 2 0 0 4 , 6 , 5 3 7 9 – 5 3 8 8
5387