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Y. Xu, W. Jager / Journal of Molecular Structure 599 /2001) 211±217
213
17671 MHz. An extensive search was carried out in
the region and two transitions were located. Both of
these have fairly small transition dipole moments,
about a quarter of that of the Ne±CO2 complex
;0.0244;13) Debye) [14], estimated by comparing
the p=2 microwave excitation pulse lengths. The rela-
tive intensities of these two transitions and their rela-
tive frequencies suggested that one might be a
candidate for the normal isotopomer and the other
one for the 13C isotopomer in its natural abundance.
However, the frequency of the candidate for the
normal isotopomer was about 70 MHz higher than
predicted from the infrared constants. Unfortunately,
the next higher J transitions are located in the 35 GHz
frequency region, outside the operating range of our
Fourier Transform microwave spectrometer. It was
therefore critical to con®rm the assignment with addi-
tional information, such as isotopic data and nuclear
quadrupole hyper®ne structures.
lower than expected, by comparing the intensity of
He±O13CO in natural abundance ;,1.1%) and that
of He±O13C18O ;,5% in the enriched sample).
At this point, the samples of OC18O, OC17O,
O13C18O, and O13C17O were prepared using enriched
H218O ;99%) and H217O ;35%) with normal CO2 and
13CO2 ;99%), respectively, to ensure high observable
intensity for all the isotopomers under consideration.
The intensity of the candidate transition for He±
O13C18O increased dramatically upon using the
enriched sample prepared with H218O and 13CO2. An
intensity increase was also observed when using the
sample prepared with H217O and 13CO2. This ®nding
was a surprise initially and caused some concern
about the assignment to He±O13C18O. The assignment
could only be correct if the H217O sample contained
substantial amounts of H218O. This was veri®ed by
carrying out parallel experiments on the known tran-
sitions of the various isotopomers of Ne±CO2 [15].
The tests veri®ed a signi®cant percentage of H218O in
the H217O sample and support therefore the original
assignment. A similar search and con®rmation proce-
dure was carried out for the rotational transition of
He±OC18O. It was located 18.5 MHz above the He±
O13C18O line, consistent with the measured frequency
difference of 22.6 MHz in the He±OCO/He±O13CO
pair.
The searches for transitions of the He±OC17O and
the He±O13C17O isotopomers were carried with the
hopes to resolve their 17O nuclear quadrupole hyper-
®ne structures. This would not only further secure the
assignment but would also provide valuable new
information about the angular isotropy of the He±
CO2 interaction potential energy surface. In the
studies of various isotopomers of Ar±CO2
[16,17,18] and Ne±CO2, [14,19] it was found that
the transition frequencies of the 17O containing isoto-
pomers could be interpolated from the 16O and 18O
data with an accuracy of better than 100 kHz. This
interpolation procedure, however, appeared not to
work well for the He±CO2 system. An initial scan
of the region where the J 1±0 transitions of the
He±OC17O and He±O13C17O isotopomers were
expected, was unsuccessful. A wider frequency scan
of about 400 MHz with the He±OC17O sample,
produced one set of lines, resembling nuclear hyper-
®ne pattern of a J 1±0 transition for a nucleus with
spin 5/2. The corresponding hyper®ne pattern was
We anticipated large uncertainties in the frequency
predictions for other minor isotopomers of He±CO2
when using the usual rigid structure model. The
Ê 2
unusually large inertial defect of 8.54 amu A , deter-
mined in the infrared study [7], emphasizes this
concern. However, since there was no other informa-
tion available for the further isotopic studies, we used
the ground state geometric parameters obtained in the
infrared investigation as the initial starting point. The
rotational constants for the various isotopomers were
then empirically adjusted to reproduce the same iner-
tial defect as in the normal isotopomer. This proce-
dure worked reasonably well with He±O13CO
isotopomer mainly because the 13C substitution
produces very little change in the rotational frequen-
cies since the carbon atom is quite close to the center
of mass of the complex. The assignment of the weaker
observed transition to He±O13CO was thus con®rmed
by the frequency position and, additionally, by a
drastic increase in intensity when enriched 13CO2
was used.
The search for the He±O13C18O isotopomer was
originally done using the enriched 13CO2 sample
;99% 13C, 5% 18O). A frequency region of about
400 MHz was scanned and a transition with the
right magnitude of transition dipole moment was
located at 17619.0744 MHz. This was much higher
in frequency than anticipated. Furthermore, the
observed intensity was found to be considerably