Gas-phase ion chemistry and ab initio theoretical study of phosphine. II. Reactions of PH+ with PH3

Citation
P. Antoniotti et al., Gas-phase ion chemistry and ab initio theoretical study of phosphine. II. Reactions of PH+ with PH3, J CHEM PHYS, 109(24), 1998, pp. 10853-10863
Citations number
70
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
JOURNAL OF CHEMICAL PHYSICS
ISSN journal
00219606 → ACNP
Volume
109
Issue
24
Year of publication
1998
Pages
10853 - 10863
Database
ISI
SICI code
0021-9606(199812)109:24<10853:GICAAI>2.0.ZU;2-4
Abstract
The gas-phase ion chemistry of phosphine has been investigated by ab initio theoretical calculations and experimental techniques. Following a previous study of H and H-2 loss pathways from the P-3-PH3+ adduct (generated by P- 3(+) reacting with PH3), the quantum chemical study of these processes has been extended to the ion-molecule reactions starting from (PH+)-P-2 reactin g with PH3, as observed by ion trapping. In these experiments, PH+ reacts t o give P2Hn+ (n = 2,3) product ions, with loss of H-2 or H in different pat hways, and also reacts in charge-exchange processes to form PH and PH3+. Mo reover, elimination of two hydrogen molecules has been observed leading to the formation of the P-2(+) ion species. All these processes take place at similar rates, their constants ranging from 1.2 to 5.5 x 10(-10) cm(3) mole cule(-1) s(-1). The geometrical structures and energies of transition struc tures, reaction intermediates, and final products have been determined by a b initio theoretical methods. The initial step is formation of the (HP)-H-2 -PH3+ adduct. Then, a hydrogen atom can be directly lost either from dicoor dinated or tetracoordinated phosphorus, to give P-3-PH3+ or (HP)-H-1=PH2+, respectively. Alternatively, one hydrogen can first undergo a displacement from the latter to the former P atom to give (H2P)-H-2-PH2+. This migration can then be followed by P-H bond dissociation, yielding again (HP)-H-1=PH2 +. Dissociation of H-2 can also occur, from either the initial HPPH3+ or re arranged H2P-PH2+ isomeric ions, yielding the (HP)-H-2=PH+ or (H2P)-H-2=Ptons, respectively. These last species are related by a H-migration process . A last H-2 loss from H2P = P+ produces P-2(2)+. Other pathways were explo red, but proved not to be viable. The heats of formation of the P2Hn+ (n = 0-4) ionic species have also been computed and reported with the experiment al data in the literature. (C) 1998 American Institute of Physics. [S0021-9 606(98)30548-6].