The reactions of the low energy oxonium ions CH 3CHCHC +(H)OCH 3, b 1 + , CH 2CHC +(CH 3)OCH 3, b 2 + , and CH 2C(CH 3)C +(H)OCH 3, b 3 + , are reported and compared with those of their 1,3-H shift isomers CH 3CHCHCH 2OCH 2 +, b 4 + , CH 2CHCH(CH 3)OCH 2 +, b 5 + , and CH 2C(CH 3)CH 2OCH 2 +, b 6 + . The metastable ion (MI) spectrum of the C 4H 6OCH 3 + ions b 1 + – b 3 + is dominated by loss of CH 2O. Elimination of C 3H 6, which is associated with a composite metastable peak, is also significant from b 2 + and b 3 + . From (multiple) collision experiments and analysis of D- and 13C-labeled isotopologues, it follows that b 1 + – b 3 + do not readily interconvert. Loss of CH 2O is proposed to involve a 1,5-H shift followed by a (dipole-assisted) 1,3-H shift into an energy-rich ion-neutral complex (INC) [C 4H 7 +/CH 2O]. Loss of CH 2O from b 4 + – b 6 + may also occur via an INC. This reaction is associated with a very small kinetic energy release, indicating that it generates the most stable C 4H 7 + ion, CH 2CHC +(H)CH 3, at the thermochemical threshold. However, this process is only prominent for ions b 5 + , which also undergo a facile loss of H 2O, via rearrangement in the INC [C 4H 7 +/CH 2O], to yield C 5H 7 + (most probably the cyclopentenyl cation). Loss of C 3H 6 and CO dominates the MI spectra of b 4 + and b 6 + and these reactions, which also occur from b 5 + , are proposed to take place from 1,2-H shift isomers of the cyclic counterparts of b 4 + – b 6 + . The behavior of b 1 + – b 3 + and b 4 + – b 6 + differs considerably from their C 4H 7O + homologues, CH 2CHC +(H)OCH 3, a 1 + , and CH 2CHCH 2OCH 2 +, a 2 + . Differences in the dissociation characteristics of the C nH 2n−2OCH 3 + species (n = 3–5) are discussed in terms of the energetics of the products that may be formed. ΔH f (298 K) values for the key ions in this study were obtained from CBS-QB3 calculations and thermochemical estimates.
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