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J. Chem. Phys., Vol. 120, No. 12, 22 March 2004
Relaxation of H2O
5593
from the zeroth vibrational state, with the intensity of the
As well as general fundamental interest, there are two
specific reasons for interest in the vibrational relaxation of
high levels of H2O. First, the work reported here is closely
connected with earlier work, both from Crim and
co-workers18 and from our own group,19,20 on the bimolecu-
lar reactivity towards radical atoms of H2O in high vibra-
tional levels of the ground electronic state. In particular, our
own work has focused on the measurement of rate coeffi-
cients for the removal,19 and especially the removal by
chemical reaction,20 of H2O molecules from specific highly
excited vibrational levels in collisions with H atoms. In that
work, rate coefficients were derived indirectly for the vibra-
tional relaxation of H2O from several excited levels in colli-
sions with unexcited H2O molecules.19 However, in arriving
at the results for removal by H atoms, it was implicitly as-
sumed that the relaxation of the excited H2O molecules by
the small amount of undissociated H2 and by the Ar carrier
gas was unimportant. The present work, to a degree, tests
that assumption.
A second reason for interest in the relaxation from high
vibrational levels of H2O is the proposal that two-stage pho-
tolysis of H2O might provide a source of OH radicals in the
atmosphere21 that has not been accounted for in atmospheric
models. The hypothesis is that visible solar radiation could
promote water molecules to high vibrational levels in the
electronic ground state and that these molecules might then
be photodissociated by light of longer wavelength than is
required to dissociate H2O from its lowest vibronic level.
Obviously, for this mechanism to be significantly operative,
it would be necessary for photolysis from high vibrational
levels to occur at a rate that is competitive with relaxation
from those levels in collisions with atmospheric gases, espe-
cially N2 and O2 .
Ϫ
absorption to
than that to
͉
04 almost two orders-of-magnitude greater
͘
13
ϩ
͉
04
.
͘
The strong local mode character of H2O(
͉
04 Ϫ), com-
͘
bined with its relative ease of preparation via absorption in
the high overtone band at around 719 nm, has led to a num-
ber of interesting dynamics experiments being performed on
this selectively excited species.14 These experiments fall into
two groups: Those which examine the OH produced by pho-
todissociation of H2O(
͉
04 Ϫ), in what is frequently referred
͘
to as vibrationally mediated photodissociation,15–17 and
those in which the results of collisions of H2O(
radical atoms are examined.14,18–20
͉
04 Ϫ) with
͘
Comparisons between the OH produced when
H2O(͉ ͉
04 Ϫ) and H2O( 13 Ϫ) are photolyzed at wavelengths
͘ ͘
р266 nm15–18 yielded two results of particular importance to
our experiments. First, the former process yields, in effect,
only OH( ϭ0), whereas the photodissociation of
v
H2O(͉
13 Ϫ) overwhelmingly produces OH( ϭ1).15 Sec-
v
͘
ond, at 266 nm, van der Waals et al.15 were only able to
detect OH product from the photodissociation from
H2O(͉ ͉
04 Ϫ), not from H2O( 13 Ϫ). These results have been
͘ ͘
rationalized by Weide et al.17 They showed that efficient
photodissociation from these vibrationally excited states
arises because of overlap between the lobe on the wave func-
Ϫ
Ϫ
tions in the
͉04 and ͉13 levels of the electronic ground
͘ ͘
˜
state at large O–H separations and those on the A dissocia-
tive potential energy surface. The fact that the ͉04 wave
͘
Ϫ
function extends to large O–H separations allows appre-
ciable overlap at lower energies, and therefore, longer wave-
Ϫ
lengths, than in the case of
͉
13
͘
.
It should be noted that the experiments of Crim’s group
on the vibrationally mediated photodissociation of H2O were
done under essentially collisionless conditions. Conse-
quently, they could be confident that the rovibrational distri-
butions of the OH that they detected result from selective
The two motivations identified in the two previous para-
graphs explain our choice of collision partners in the present
Ϫ
work. We have studied collisional relaxation of H2O(
͉
04
͘
)
by ͑a͒ H2O, Ar, and H2 , the main constituents of the mix-
tures in our previous experiments,19,20 and ͑b͒ N2 and O2 ,
the main constituents of the Earth’s atmosphere. There have
been only two previous studies of the vibrational relaxation
of H2O. Finzi et al.,22 using the laser-induced vibrational
fluorescence technique, measured rate coefficients from the
photodissociation of the initially prepared vibrational state.
ϩ
Because of the difficulty of preparing H2O in the (
͉
04
͘
)
state, there are no experimental data, or indeed theoretical
calculations, on photodissociation of this state. Nevertheless,
it seems reasonable to suppose that the cross sections for
photodissociation from this state will be similar to those for
coupled ͑100͒ and ͑001͒, or and 3 , normal mode states
04 Ϫ).
1
photodissociation of H2O(͉
͘
in collisions with the same range of collision partners that we
have employed. The temperature range of these measure-
ments was extended by Zittel and Masturzo.23 Both sets of
workers concluded that populations in the and states
The method that is used in the present work to examine
the relaxation of highly vibrationally excited H2O relies on
the fact that H2O molecules with four quanta of O–H
stretching vibration are selectively photolyzed at 266 nm;
that is, neither unexcited H2O molecules nor H2O molecules
with fewer than four quanta of excitation in a local O–H
stretching vibration are significantly photolyzed at this wave-
length. We utilize this property to follow the decay of the
1
3
rapidly equilibrated and that these excited molecules then
relaxed via the 2 level.
2
II. EXPERIMENT
excited H O population by observing the OH( ϭ0) that is
v
2
produced when H2O(
photolysed at various delays, after an initial population of
H2O(
04 Ϫ) has been produced by exciting H2O molecules
͉
04 Ϫ), and probably H2O(
͉
04 ϩ), are
The general method employed in the present experi-
ments is similar to that used previously to determine the
branching ratio between reaction and relaxation in the re-
͘
͘
͉
͘
from their ground vibrational level using a pulsed tunable
moval of H2O from its (
atoms,19,20 in that it relies on the selective photolysis of
H2O(
04 Ϯ) by laser radiation at 266 nm and the detection
of the OH( ϭ0) that is formed using LIF.20
͉
04 Ϫ) level in collisions with H
͘
dye laser. Later, we discuss further whether our technique is
Ϫ
likely to monitor only the population in the
͉
04 state, or
͉
͘
͘
Ϫ
ϩ
the sum of the populations in the ͉04 and ͉04 states.
v
͘ ͘
134.117.10.200 On: Mon, 23 Jun 2014 09:01:50