Roth, Maul, and Gericke: Photodissociation dynamics of OClO
10583
1
9,20
gated with the REMPI technique
and the O atom is easily
column filled with NaClO and Raschig rings. While the gas
2
accessed by REMPI,2
1,22
the experimenters concentrated on
flowed through the column, OClO and NaCl were produced.
The gas was transferred into the reaction chamber without
further purification. The cell was evacuated by two oil diffu-
sion pumps ͑Leybold, 500 l/s͒ and a turbomolecular pump
͑Leybold Heraeus 360 CSV, 360 l/s͒ to a base pressure of
measuring ClO and Cl fragments, but no oxygen fragment
analysis has been performed. In this work, for the first time
REMPI spectra of the oxygen fragments are presented,
formed by dissociation of OClO (A A (18,0,0)) upon ex-
citation at 308 nm. We state selectively probed all spin-orbit
˜
2
2
Ϫ4
10 Pa. The OClO gas was expanded into the reaction
3
states of oxygen O( P ) with ͑2ϩ1͒-REMPI at wavelengths
chamber by a pulsed nozzle ͑General Valve͒ which was op-
erated at a stagnation pressure of 200–600 mbar and a pulse
duration of typically 250 s. At a repetition rate of 10 Hz,
J
around 225 nm. Analyzing state specific velocity distribu-
tions by time of flight measurements, kinetic and internal
energies of the ClO partner fragment are obtained, taking
into account the conservation of energy and linear momen-
tum. Thus, the energetics and the ͑joint partner͒ product state
distributions of the photodissociation process can completely
be characterized, especially with respect to the dissociation
pathways leading to spectroscopically dark, highly vibra-
tionally excited ClO fragments. Furthermore, new dissocia-
tion pathways were found with a rise in excitation energy but
their dissociation geometry, decay time, and spatial distribu-
tion is still unknown. In addition, we present high resolution
REMPI spectra of the spectroscopically accessible ClO
which were investigated by Vaida et al.23 at lower resolu-
tion. In order to obtain some information on the dissociation
time, polarization measurements were performed, and the in-
fluence of the polarization vector of the probe laser on the
shape of the TOF profile, reflecting the spatial fragment dis-
tribution, was analyzed.
Ϫ3
the background pressure was 10 Pa with the nozzle in op-
eration. From linewidth measurements with CO, the parent
molecule temperature could be estimated to be about 10 K.
Thus, the internal energy of OClO is negligible.
The molecular beam propagates perpendicularly to the
axis of our time of flight spectrometer, which is described in
detail elsewhere.28 At the end of the spectrometer, micro-
channel plates in chevron configuration are used to enhance
the ion signal. The TOF spectrometer can be operated in
three different ways.
First, in the drift mode the ions drift through the spec-
trometer with a total length sϭ0.57m only because of their
initial recoil velocity. The signal is monitored with a multihit
time-to-digital converter ͑FAST 7885͒ with a time resolution
of 5 ns per channel, stored in a data buffer ͑FAST MCD/PC͒
and transferred to a personal computer. The drift mode di-
rectly yields the velocity distribution F (v) from the mea-
v
D
T
The generation of highly vibrationally excited ClO in the
photodissociation of OClO is of great importance in atmo-
spheric chemistry because of possible subsequent ClO reac-
tions with constituents of the atmosphere.
Choo and Leu suggested the following reactions of vi-
brationally excited ClO with Cl and O3:
sured TOF profile F (t) via the relation
D
T
2
F ͑v͒ϭF ͑t͒•t .
͑6͒
v
Second, in the acceleration mode, the ions are acceler-
ated along a region of 0.19 m (ϭs/3) by a homogeneous
electric field of variable strength. In the present measure-
ments the electric field was fixed at 2600 V/m. The accelera-
tion region is followed by a field free drift region of twice
the length of the acceleration region. The shape of the tem-
porally broadened ion signal was monitored by a digital tran-
sient wave form recorder ͑LeCroy 9450͒. The acceleration
2
4
ClO͑vϾ2͒ϩCl→Cl ϩO,
͑3͒
͑4͒
2
ClO͑vӷ0͒ϩO →ClOϩO ϩO.
Similarly, the UV dissociation of O at 226 nm (O3
3
2
3
2
5
ϩh(226 nm͒→O ϩO) is known to produce highly vi-
2
3
Ϫ
g
mode yields the distribution F (v ) of the velocity compo-
brationally excited O (X ⌺ ,vу26) molecules, which
v
x
x
2
could be a so far neglected source in the atmospheric ozone
production via the reaction,
nent v along the spectrometer axis from the TOF profile
x
A
F (⌬t) via the linear relationship
T
3
O ͑vу26͒ϩO →O ϩO͑ P͒.
͑5͒
ϭc •⌬t,
͑7͒
2
2
3
vx
Ј
Furthermore, a vibrationally excited oxygen molecule can be
2
0
where cЈϭ8s/3t ϭ8eU /m accounts for the acceleration
A
dissociated by near UV radiation, whereas O in its ground
2
voltage U , the spectrometer length s, particle mass m, and
A
level requires VUV26 radiation. As a result of the higher flux
of near UV light in the atmosphere, this oxygen dissociation
pathway becomes important for atmospheric chemistry.
Due to the formation of extremely vibrationally excited
charge e. ⌬tϭtϪt is the deviation from the center of the
acceleration profile.
Equation ͑7͒ holds in all practically relevant cases,
where the acceleration energy is large compared to the initial
kinetic energy of the observed fragment:
0
ClO radicals, reactions with the atmospheric molecules O or
N become possible, and in this case the reaction rate may
well exceed the relaxation rate.
2
2
1
2
mv2.
e•UAӷEkinϭ
͑8͒
F (v) is easily obtained from F (v ) if the spatial fragment
v
v
x
x
EXPERIMENT
distribution is known.
The OClO molecule was generated according to the
Third, in the Doppler mode the electric field is so large
that one cannot measure any difference in arrival time. In-
stead the total intensity of the ion signal is integrated by a
27
method of Derby and Hutchinson. A bulb containing a gas
mixture of about 10% Cl and 90% N was coupled to a
2
2
J. Chem. Phys., Vol. 107, No. 24, 22 December 1997
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