Abstract

Ab initio molecular orbital calculations at levels of theory beyond G2 have been used to study the structures, relative stabilities, ionization potentials and heats of formation of [O, P, H] neutral and cationic species, which are involved in the reactions of P + with water in the gas phase. OPH ( 3A″) and OPH + ( 2A′) are open-shell systems for which UMP theory is not reliable. Hence, their structures, as well as those of the other open-shell species were obtained at the QCISD (T)/6-311G (d, p) level. Possible shortcomings of the G2 theory were investigated by comparing G2 energies with those obtained at the QCISD (T)/6-311 + G (3df, 2p) level. The energies obtained indicate that the formation of the OPH + ( 2A′) molecular cation in the reaction of P + in its first excited state ( 1D) is exothermic and may play a significant role in the production of PO in interstellar media.

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