A guided-ion beam mass spectrometer is used to study the reactions FeC
H2+ + D-2 and Fe+(D-6,F-4) + CD4, thereby experimentally probing the [
FeCH4](+) potential energy surface(PES). The results obtained are comp
ared to recent theoretical results. Experiment and theory agree that d
ehydrogenation of methane by Fe+ is hindered by a tight, four-center t
ransition state complex. The major discrepancy observed between experi
ment and theory is in the height of this barrier, which theory predict
s to be 75 kJ/mol (92 kT/mol after correction for zero-point energies)
versus our experimental result of 41 +/- 6 kJ/mol. Our results can be
interpreted by using phase space theory to help understand how variou
s features on the PES control branching ratios among the various chann
els observed, including extensive hydrogen scrambling in the FeCH2+ D-2 reaction. Lastly, results for the [FeCH4](+) PES are compared to t
hose for the [CoCH4](+) PES obtained in a previous study in order to h
elp assess the effect of potential energy surfaces of different spin i
n the former case.