Despite the importance of phosphorus-bearing molecules
for life
and their abundance outside Earth, the chemistry of those compounds
still is poorly described. The present study investigates phosphine
(PH3) decomposition and formation pathways. The reactions
studied include phosphine thermal dissociation, conversion into PO(2Π), PN(1Σ+), and reactions
in the presence of H2O+. The thermodynamic and
rate coefficients of all reactions are calculated in the range of
50–2000 K considering the CCSD(T)/6-311G(3df,3pd)//ωB97xD/6-311G(3df,3pd)
electronic structure data. The rate coefficients were calculated by
RRKM and semiclassical transition-state theory (SCTST). According
to our results, PH3 is stable to thermal decomposition
at T < 100 K and can be formed promptly by a reaction
network involving PH(3Σ–), PO(2Π), and PN(1Σ+). In the
presence of radiation or ions, PH3 is readily decomposed.
For this reason, it should be mainly associated with dust grains or
icy mantles to be observed under the physical conditions prevailing
in the interstellar medium (ISM). The intersystem crossing associated
with the dissociation of the isomers PON, NPO, and PNO is accessed
by multireference methods, and its importance for the gas-phase PH3 formation/destruction is discussed. Also, the implications
of the present outcomes on phosphorus astrochemistry are highlighted.