(
)
N.I. ButkoÕskaya, D.W. SetserrChemical Physics Letters 312 1999 37–44
39
through three molecular sieve traps cooled by ace-
tonerdry ice mixture and liquid N2 before being
added to the reactor. These traps reduce the H2O and
CO2 impurities. The isotopic and chemical purity of
were selected for comparison that had similar reagent
Ž
.
concentrations see the figure caption , and the rela-
tive intensities in Fig. 1 reflect the relative concentra-
tions of the isotopic water molecules generated by
Ž
.
Ž
.
CH3SD CDN Isotopes were )94% and )99.6%,
the CH3SH CH3SD and DMDS chemical reaction
systems. One should note the comparable yields of
water molecules in both systems. The observation of
D2O emission spectra from ODqDMDS is convinc-
Ž
respectively. The CH3SSCH3 purchased as a liquid
from Aldrich Chemical, 99% was degassed in
.
freeze–thaw–pump cycles. The central fraction from
a room temperature liquid sample was expanded into
a 10 l Pyrex glass bulb and a 7% mixture in Ar was
prepared. This mixture was used during the same
working day. The DMDS mixture was metered to the
reactor through a 10 mm ID glass line approximately
50 cm in length. Experiments were done with two
independently prepared DMDSrAr mixtures.
Ž
.
ing evidence for the importance of reaction 1b . The
observation of D2O emission from the ODqDMDS
reaction also eliminates the possibility that the de-
composition of DMDS in the gas handling procedure
could be the source of the water emission, e.g., the
source cannot be ODqCH3SH.
The spectra from the DMDS and CH3SH
CH3SD systems are very similar. Analysis of the
Ž
.
The computer simulation procedure used to assign
stretching and bending mode distributions from the
H2O, HOD and D2O spectra has been described
spectra by computer simulation showed only very
small differences, which can be explained from con-
tamination in the ODqCH3SD system by the
CH3SH isotopic impurity 10 . The H2O stretching
distributions obtained by simulation of the spectra
w
x
8,10–13 . In the present work, our interpretations
w
x
are mainly based on the overall appearance of the
emission spectra and on the total emission intensi-
ties, and we will not describe the simulation proce-
dures. The limited degree of vibrational relaxation of
the product water molecules for the short reaction
time and low Ar pressure has been discussed in Refs.
Ž
.
.
are P1,3 1:2:3 s 66:30:5 from DMDS and
Ž
P1,3 1:2:3 s68:26:6 from CH3SH; the D2O stretch-
Ž
.
ing distributions are P1,3 1:2:3 s64:33:2 for DMDS
Ž
.
and P1,3 1:2:3 s65:32:3 for CH3SD. The 1,3 sub-
scripts denote the coupled n1 and n3 modes. The
HOD emission in the 3200–4000 cmy1 range is
overlapped with the Õ2 qÕ3 combination bands from
D2O, and a complete analysis of these spectra will
w
x
8,10–13 . For the conditions of the experiments to
be described, the populations in the n1 and n3
modes of H2O and D2O and the populations in the
n1 and n2 modes of HOD are coupled by collisions
with Ar. The vibrational relaxation of H2O, D2O,
and HOD molecules beyond this coupling is negligi-
ble. The only assumption in the spectral simulation is
that the rotational distributions are represented by
300 K Boltzmann distributions.
w
x
be made later 10 . It is sufficient here to note that
the two spectra in Fig. 1c,d in the 3200–4000 cmy1
range are identical. The spectral pattern from the
ODqDMDS system, including the intensity ratio
between the D2O and HOD parts of the spectra, did
not change with variation of DMDS or OD concen-
tration, when the former was varied between 1 and
7=1012 molecule cmy3 and the latter was varied
between 1.5 and 2.8=1013 molecule cmy3. The
D2O and HOD emission arise from the same source
in the ODqDMDS reaction and, in fact, this source
is the reaction of OD with CH3SD.
3. Results and discussion
3.1. Chemiluminescent spectra
The raw chemiluminescent spectra from the OH
qDMDS and ODqDMDS reaction systems are
shown in Fig. 1b,d, respectively. They can be com-
pared to the H2O spectra in the 3200–4000 cmy1
3.2. Kinetic behaÕior and reaction mechanism
Ž
.
range from the OHqCH3SH reaction Fig. 1a and
Comparative kinetic measurements were carried
out for the ODqDMDS and ODqH2 S systems in
order to quantify the water yield in the DMDS
system. The H2 S system was chosen as one nearly
y1
Ž
.
Ž
D2O 2400–3000 cm
and HOD 3200–4000
cmy1 spectra from the ODqCH3SD reaction Fig.
.
Ž
.
w
x
1c measured in our previous studies 8,10 . Spectra