M. Hahn et al. / Journal of Molecular Spectroscopy 223 (2004) 138–147
139
however, the authors point out that the compound does
not survive 80 K in condensed phase. Another important
aspect: because this molecule is only composed of the
atoms C, H, N, and O there is some evidence that it may
be detected in interstellar space by radio astronomy just
like the unsubstituted ketene [21], and laboratory sim-
ulations have already been carried out [22] how it could
be formed in outer space. Looked at from this point of
view the microwave transitions published herein could
be useful.
with a yield of 95%. The resulting cyanoacetic acid was
then processed as above.
2.1.4. N13CCHCO
The same procedure was used as described under
Section 2.1.3 but with 13C-labeled KCN.
2.1.5. NCCHC18O
To obtain this isotopomer, the simplified procedure
of not isolating the cyanoacetyl chloride could not be
used. Instead, the reaction mixture from the chlorina-
tion of the cyanoacetic acid was, again after removal of
ether and POCl3, carefully distilled under a pressure of
20 Pa, yielding the pure chloride at 33 °C. This was
hydrolyzed with H218O according to
2. Experimental procedures
2.1. Chemical preparation of cyanoketene
NBC–CH2–COCl þ H218O ! NBC–CH2–CO18OH
þ HCl
producing a cyanoacetic acid containing one 18O-atom.
Chlorinating this acid as described under Section 2.1.1
resulted in a 1:1-mixture of ‘‘normal’’ and 18O-cyano-
acetyl cloride. The final pyrolysis therefore also produced
a 1:1-mixture of cyanoketene and 18O-cyanoketene.
2.1.1. Parent molecule NCCHCO
We intended to prepare cyanoketene by dehydro-
chlorination of cyanoacetic acid chloride, NC–CH–
COCl, under pyrolytic conditions in the gas phase.
Since, however, this precursor is known to be unstable
[23], we at first did not attempt to isolate this compound.
It was prepared, instead, in the usual way by chlori-
nating the free acid in dry diethyl ether with PCl5 at
room temperature. Then the reaction mixture was
cooled down to )40 °C, and the ether was distilled off.
After removal of the ether the remaining mixture was
further cooled to )60 °C and connected to the flow
system. This consisted of an oven of 10 cm in length
surrounding a quartz tube of 1 cm i.d. and loosely
packed with rock-wool for better heat transfer, spec-
trometer cell, LN2-traps, and vacuum line. The oven still
kept cool, the by-product POCl3 was withdrawn
through the absorption cell, its final disappearance being
monitored by some microwave transitions. Then the
oven was heated to 750 °C; this temperature giving
the strongest signals for almost all isotopomers. Finally
the sample was allowed to warm up until the pressure
was sufficient for optimum spectroscopic conditions; ice
water was convenient. After use the sample had always
to be kept below )20 °C.
2.2. Spectrometer Set-up
The microwave spectrograph was of conventional
Stark-type operating at 30 kHz and equipped with a
self-configurated and -programmed ELTEC computer—
based on a MOTOROLA 68K processor—for time
averaging because the pyrolytic reaction is not really
stationary. 1000 points for spectrum and also for fre-
quency markers could be taken and shown on the screen
with a repetition rate of 9 Hz. For survey spectra 50MHz
ranges were used with real-time frequency markers, the
MARCONI-sweeper swept via its FM-input. The fre-
quency accuracy of 300–500 kHz was sufficient for as-
signments. By means of the frequency markers these
spectra could be concatenated with arbitrary frequency
scaling for viewing larger spectral ranges. For precise
frequency measurements the sweeper was phase-stabi-
lized against the frequency standard and swept via the
reference frequency of 30 MHz by means of a voltage-
frequency converter. Ranges of 1–3 MHz were used, also
with real-time frequency markers and resulting in an
accuracy better than 10 kHz. Finally each line was fitted
to Lorentzian shape to obtain the center frequency. The
frequency standard was monitored against the standard
signals of DCF77-station, Mainflingen, Germany, the
relative deviations kept <10ꢀ8. The cell temperature
was )15 °C and the pressure 4 Pa for the survey spectra
and down to 0.2 Pa for frequency measurements, de-
pending upon the intensity of the transition. Figs. 1 and
2 show examples of a survey spectrum and of a fre-
quency determination. The small structures in Fig. 1 are
2.1.2. NCCDCO
The acidity of the hydrogen atoms in cyanoacetic acid
is sufficiently high to exchange them against deuterium
by shaking the acid with D2O. The degree of exchange
was monitored by means of a quadrupole mass spec-
trometer. After drying, the acid was processed as de-
scribed above. A remarkable isotope effect was observed
for the pyrolysis of just this isotopomer: cyanoketene
formation had its optimum already at 600 °C, and above
660 °C no more signals were found.
2.1.3. 15NCCHCO
The sodium salt of chloroacetic acid was reacted with
15N-labeled KCN according to a Kolbe-synthesis and