On the nature of ion-molecule collisions.
Ion-molecule collisions of Ar-Co and N-No pairs, discussing charge exchange reaction rates and spiraling nature
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Ion-molecule collisions of Ar-Co and N-No pairs, discussing charge exchange reaction rates and spiraling nature
Ion-molecule collision charge transfer and momentum transfer relaxation rates, using ion cyclotron resonance heterodyning method
Ion trajectory and capture cross sections in quadrupole field for determining ion quadrupole effects in ion-molecule collisions
Ion-quadrupole effects in ion-molecule collisions by numerical calculations of capture cross sections and computer-plotter studies of ion trajectories
Numerical analysis of spiraling in ion molecule collisions with polar targets using computer plotting techniques
Computer made movies and time history plots for ion-dipole collisions involving polar molecules /CO, HCL and acetonitrile/
Ion-quadrupole effects are investigated via numerical calculations of capture cross sections and computer-plotter studies of ion trajectories in the quadrupole field. Capture cross sections are roughly equal to Langevin values for low rotational temperatures; a large fraction of multiple reflection captures are calculated corresponding to formation of ion-molecule complexes.
The transient method considered is analogous to similar phase coherence experiments performed in NMR and plasma physics. Using a pulsed ion cyclotron resonance (ICR) spectrometer equipped with a trapped ion analyzer cell, gaseous ions are formed by a pulse of an electron beam and then trapped in the cell by the combined effects of the magnetic and electrostatic fields. The results obtained in the experiments indicate that the classical mobility treatment of Wannier (1953) is helpful in the understanding of collision frequencies under the considered conditions.
Determination of experimental momentum transfer rate constants for systems of Cl(-) and Cr(CO)5(-) ions by means of an ion cyclotron resonance (ICR) line-broadening technique. It is found that in the pure polarization limit of small ion/large neutral collisions the Langevin ion mobility theory gives good agreement with experimental results. A comparison of isotropic and anisotropic neutral systems suggests that a correction for the anisotropic systems is necessary. Beyond the pure polarization limit the Langevin theory gives poor predictions for ion mobilities. The adjustable parameter, gamma, of the Mason-Schamp (12-6-4) potential function permits unique solution of the ion mobility for Cr(CO)5(-) in a wide range of neutral gases. The large values of gamma obtained for most of these systems imply, in terms of the Mason-Schamp theory, that the r to the minus 6th power contribution to the potential function is significant.
Vibration effects on ion-molecule collision lifetimes and multiple reflections
Isotope effects on collision dynamics of molecular hydrogen-argon ion reactions, using chemical accelerator
Theoretical description of the reaction rate of an ion-molecule interchange reaction as a function of collision parameters
Vibrational effects on capture cross sections and ion-molecule complexes formation based on ion- dipole collisions, noting multiple reflection probabilities and collision lifetimes
Vibrational degrees of freedom effects on capture cross sections and ion-molecule complexes formation in ion-dipole collisions
Ion-molecule reactions of diatomic deuterium cation with diatomic deuterium and diatomic hydrogen
Presented in this paper is an ab initio chemical model for dense interstellar clouds that incorporates 598 grain surface reactions, with small grains providing the reaction area. Gas-phase molecules are depleted through collisions with grains. The abundances of 372 chemical species are calculated as a function of time and are found to be of sufficient magnitude to explain most observations. Peak abundances are achieved on time scales of the order of 100,000 to 1 million years, depending on cloud density and kinetic temperature. The reaction rates for ion-molecule chemistry are approximately the same, indicating that surface and gas-phase chemistry may be coupled in certain regions. The composition of grain mantles is shown to be a function of grain radius. In certain grain-size ranges, large molecules containing two or more heavy atoms are more predominant than lighter 'ices' - H2O, NH3, and CH4. It is possible that absorption due to these large molecules in the mantle may contribute to the observed 3-micron band in astronomical spectra.
Ion-molecule reaction rate constants measurement by ion cyclotron resonance, assuming no ion and neutral gas molecules collisions
A drift tube mass spectrometer apparatus has been used to determine the rate coefficient, energy dependence and product ions of the reaction He(+) +H2. The total rate coefficient at 300 K is 1.1 plus or minus 0.1) 10 to minus 13th power cu cm/sec. The reaction proceeds principally by dissociative charge transfer to produce H(+), with the small remainder going by charge transfer to produce H2(+) and by atom rearrangement to produce HeH(+). The rate coefficient increases slowly with increasing ion mean energy, reaching a value of 2.8 x ten to the minus 13th power cu cm sec at 0.18 eV. The corresponding reaction with deuterium, He(+) + D2, exhibits a value (5 plus or minus 1) x 10 to the minus 14th cu cm/sec at 300K. The reaction rates for conversion of H(+) and HeH(+) to H3(+) on collisions with H2 molecules are found to agree well with results of previous investigations.