Rotationally resolved photoelectron spectra of jet-cooled H 2 O, HDO and D 2 O have been recorded near the origin of thẽ X + ←X photoionising transition following single-photon ionization using the complementary techniques of mass-analysed threshold-ionization (MATI) and pulsed-field-ionization zero-kinetic-energy (PFI-ZEKE) photoelectron spectroscopy. A gas mixture of H 2 O, HDO and D 2 O with Ar was obtained by mixing H 2 O ( ) and D 2 O ( ) in a reservoir and bubbling Ar gas through the mixture. To unambiguously assign the photoelectron bands to H 2 O, HDO or D 2 O, the PFI-ZEKE photoelectron spectra of the mixture were compared to MATI spectra and to spectra of H 2 O. Analysis of the rotational structure of the origin bands (HDO and D 2 O and of the transitions to the (010), (020) and (100) levels of D 2 O + and the first excited level of the O-D stretching mode of HDO + provided new information on the photoionization dynamics of water and the energy level structure of HDO + and D 2 O + .
IntroductionWater (H 2 O) and its cation (H 2 O + ) are prototypical small molecules [1] and play an important role on earth and in the universe. Studies of H 2 O, HDO and D 2 O by vacuum-ultraviolet photoelectron and photoionization spectroscopy provide information on their interaction with short-wavelength radiation, on their photoionization dynamics and on the energy-level structure and dynamics of the cations [2-16]. The valence-shell photoionization of water, either in a single-photon process from theX 1 A 1 ground state or in multiphoton processes through electronically excited states, has provided access to a wide range of rovibrational levels of theX + 2 B 1 andà + 2 A 1 states of the cation, which are degenerate in linear (D ∞h ) configurations and subject to the Renner-Teller effect [17][18][19]. Whereas H 2 O + in the first excited state is quasilinear, the equilibrium geometry of the ground cationic state is bent and similar to that of the ground state of the neutral. Consequently, many more vibrational levels of theà + 2 A 1 state are accessible by photoionization from the ground state of the neutral than is the case for theX + 2 B 1 state [2,4,5,12,15,16].The vacuum-ultraviolet (VUV) photoelectron spectrum of theX + 2 B 1 ←X 1 A 1 photoionising transition of water thus consists of only a few vibrational bands, i.e., a strong origin band and weak and short progressions in the bending (0, v + 2 , 0) and symmetric stretching (v + 1 , 0, 0) modes [4,12,15,16]. The weakness of the bands associated with