RATE CONSTANTS AND BRANCHING RATIOS FOR THE REACTIONS OF SELECTED ATMOSPHERIC PRIMARY CATIONS WITH N-OCTANE AND ISOOCTANE (2,2,4-TRIMETHYLPENTANE)

Citation
St. Arnold et al., RATE CONSTANTS AND BRANCHING RATIOS FOR THE REACTIONS OF SELECTED ATMOSPHERIC PRIMARY CATIONS WITH N-OCTANE AND ISOOCTANE (2,2,4-TRIMETHYLPENTANE), The journal of physical chemistry. A, Molecules, spectroscopy, kinetics, environment, & general theory, 101(49), 1997, pp. 9351-9358
Citations number
16
ISSN journal
10895639
Volume
101
Issue
49
Year of publication
1997
Pages
9351 - 9358
Database
ISI
SICI code
1089-5639(1997)101:49<9351:RCABRF>2.0.ZU;2-6
Abstract
Gas-phase ion molecule reactions of the primary atmospheric cations (N O+, O-2(+), O+, N+, and N-2(+)) With two isomers of octane, n-C8H18 an d iso-C8H18 (2,2,4-trimethylpentane) have been studied using a variabl e temperature selected ion flow tube instrument. Reaction rate constan ts and product branching fractions were measured from 300 to 500 K. Th e reactions of O-2(+), O+, N+, and N-2(+) with n-C8H18 and iso-C8H18 p roceed at the collision rate via dissociative and/or nondissociative c harge transfer. The NO+ reactions occur primarily by hydride transfer; the reaction rate for the straight-chain isomer is only one-fourth th e collision rate, while the reaction rate for the branched isomer is s ignificantly enhanced. The reaction of n-octane with each atmospheric cation generates two to four major product ions and numerous minor spe cies. The major ionic products are alkyl cations, CnH2n+1+, where the degree of fragmentation of the hydrocarbon chain is governed largely b y the reactant ion recombination energy. The largest ionic products ob served, n-C8H17+ and n-C8H18+ thermally decompose at temperatures abov e 300 K. The reaction of isooctane with each atmospheric cation genera tes fewer minor species than was observed in the n-octane reactions, a nd only one to three major product ions are observed. The main ionic p roduct of the O-2(+), O+, N+, and N-2(+) reactions is the alkyl cation C4H9+, although several reactions also produce significant amounts of the related radical cation C4H8+. The main ionic product of the NO+ r eaction, C8H17+, thermally decomposes into C4H9+ at temperatures above 300 K. Presumably, the specificity of the product ion formation in th e iso-C8H18 reactions is a consequence of the neutral reactant structu re. Except for thermal fragmentation of C8Hm+ product ions at temperat ures above 300 K, there is little temperature dependence on the produc t ion branching fractions for the reported reactions.