310
B. Ouyang et al. / Chemical Physics Letters 402 (2005) 306–311
The decay rate of the HNO2–NO2 adduct showed no
sign of concentration-dependence. Fitting the decay
curve at 260 nm by the first-order kinetics yielded a de-
(1) 2NO + O2: Deaeration of the sample solution would
not cause any difference in the transient absorption
curve, showing that reaction 2NO + O2 ! 2NO2
could be neglected over the entire monitoring time
range (20 ls ꢄ 1 ms). It could be explained by the
dmꢀ6 molꢀ2 sꢀ1[4], of this termolecular reaction.
(2) NO + HNO2: No reaction was observed when
injecting NO into nitrogen-saturated HNO2 solu-
tion, showing that the reaction NO + HNO2 is
immeasurably slow or does not happen at all.
(3) NO + NO2: Possibility of a significant occurrence
of this second-order reaction has been excluded,
as stated in Section 3.3. Formation of N2O3 was
suppressed by HNO2 as the efficient scavenger of
NO2. The concentration of HNO2 was by nearly
three orders of magnitude higher than that of NO.
(4) NO + NO2–HNO2: If this reaction occurred signif-
icantly, the decay rate of the NO2–HNO2 adduct
would have been influenced by the laser pulse
energy which determined the concentrations of
NO and NO2–HNO2. However, we hardly wit-
nessed such energy-dependence in the experiment.
cay rate constant of 3.0 · 103 sꢀ1
.
The decay products were unlikely to be ONOOH,
NO3 or HNO because no transient absorption signals
were observed during the decay process of HNO2–NO2
in the wavelength range of 240–800 nm, where strong
absorptions are expected for these species [6,19,20].
The formation of HNO3 and NO was therefore most
likely, as shown by reaction (R.8). The overall reaction
would then be (R.9) if this hypothesis were true, with
impressively
low
rate
constant,
4 · 106
a
standard Gibbs free energy change DrGU9 of
ꢀ24.54 kJ molꢀ1 [21]. The negative value suggests that
(R.9) is at least thermodynamically feasible and may
constitute one source of HNO3 in the photolysis of
aqueous solution of HNO2.
k8
HNO2 ꢀ NO2 ! HNO3 þ NO
ðR:8Þ
k9
NO2ðaqÞ þ HNO2ðaqÞ ! NOðaqÞ þ HNO3ðaqÞ
ðR:9Þ
Fischer and Warneck [4] noticed that the theoretically
predicted rise rate of NO3ꢀ using the reported reactions
was obviously lower than the experimentally observed
one, which to some extent validated (R.9): by adding
(R.9) to the reaction sketch summarized by Fischer, the
rise rate of NOꢀ3 was expected to increase due to a more
efficient conversion of NO2 to NOꢀ3 by (R.9) at the
expense of the reaction NO + NO2 ! N2O3 ! 2HNO2,
which essentially converted NO2 back to HNO2.
It was thus concluded that NO was not observed to be
involved into the chemical reaction process within 1 ms.
In the later time stages, it may dissolve into the solution.
4. Conclusion
According to the reactions (E.6) and (R.8), HNO2ꢀ
NO2 would either decompose to the final product
HNO3 and NO or dissociate back to the reactants once
formed. Interestingly, an opposite reaction as
The photolysis of HNO2 in the aqueous phase was
investigated using the laser flash photolysis technique.
The OH quantum yield was measured to be
0.25 0.03.
A
novel reaction NO2 + HNO2 ()
NOðgÞ þ HNO3ðgÞ ! NO2ðgÞ þ HNO2ðgÞ
ðR:10Þ
HNO2–NO2 was reported with a forward reaction rate
constant of 3.76 · 107 dmꢀ3 mol sꢀ1 and a backward
rate constant of 1.06 · 105 dmꢀ3 mol sꢀ1 at 15 1 ꢁC.
The HNO2–NO2 adduct would probably decompose
to form HNO3 and NO at a rate constant of
3.0 · 103 sꢀ1. These reactions need to be incorporated
into the solution phase chemistry of nitrogen.
has been recently reported by Mochida and Finlayson-
Pitts [22] and Saliba et al. [23]. They found HNO3 and
NO would react on the surface of porous or borosilicate
glass in the presence of water to form HNO2 and NO2,
which was the reverse of (R.9). Judging from the stan-
dard Gibbs free energy change of the reactions, one
would expect that reaction (R.10) is only thermodynam-
ically possible in the gas phase while the one (R.9) only
occurs in the aqueous phase. The direct reason for the
changing of the reaction direction is that NOꢀ3 can be
highly stabilized by its solvation process (DGU =
ꢀ37.8 kJ molꢀ1 [21]), which in turn notably lowers the
standard Gibbs formation free energy of the ion.
Acknowledgements
We thank Dr. Lei Zhu in the State University of New
York at Albany for her constructive comments on the
manuscript.
3.4. Fate of the other photolysis fragment NO
References
NO may react with O2, HNO2, NO2 and the NO2–
HNO2 adduct in the experiment system. However, pos-
sibility of a significant occurrence of the above reactions
has been excluded as following:
[1] B.J. Finlayson-Pitts, J.N. Pitts Jr., Atmospheric Chemistry
Fundamentals and Experimental Techniques, John Wiley & Sons,
1986.
[2] R.A. Cox, J. Photochem. 3 (1974) 175.