The
infrared (IR) spectra of the O–H stretching vibrations
of pyridine–water clusters (Pyd)
m
(H2O)
n
, with m, n = 1–4, have been investigated with infrared–vacuum
ultraviolet (VUV) spectroscopy under a jet-cooled condition. The time-of-flight
mass spectrum of (Pyd)
m
(H2O)
n
+ by VUV ionization at ∼9 eV showed an unusual intensity pattern
with very weak ion signals for m = 1 and 2 and stronger
signals for m ≥ 3. This unusual mass pattern
was explained by a drastic structural change of (Pyd)
m
(H2O)
n
upon
the VUV ionization, which was followed by the elimination of water
molecules. Among the recorded IR spectra, only one spectrum monitored,
(Pyd)2
+ cation,
showed a well-resolved structure. The spectrum was analyzed by comparing
with the simulated ones of possible stable isomers of (Pyd)2(H2O)
n
, which were obtained
with quantum-chemical calculations. Most of the calculated (Pyd)2(H2O)
n
clusters had
the characteristic structure in which H2O or (H2O)2 forms a hydrogen-bonded bridge between two pyridines
to form the π-stacked (Pyd)2, and an additional H2O molecule(s) extends the H-bonded network. The π-stacked
(Pyd)2(H2O)
n
moiety
is very stable and is thought to exist as a local structure in a pyridine/water
mixed solution. The Fermi resonance between the O–H stretch
fundamentals and the overtones of the O–H bending vibrations
in (Pyd)
m
(H2O)
n
was found to be less pronounced in the case of (Pyd)
m
(NH3)
n
studied previously.