Abstract
Canonical ensemble molecular dynamics simulations were conducted for methane diffusion in AlPO4-5 in order to assess the role of the lattice motion on adsorbate diffusivity in straight pore zeolites. Both a static lattice model and a full dynamic lattice model were used at a loading of 1.5 methane/unit cell at 295 K. Although recent simulation work has asserted that there should be a difference, we show that there is little difference in the observed methane diffusivity (1.26 × 10-7 m2/s) and passing frequency (0.305) when a static lattice approximation is used over a full dynamic lattice (1.33 × 10-7 m2/s and 0.328). Furthermore, we introduce a methodology for handling lattice motion in molecular simulations by utilizing the normal vibrational modes in a harmonic crystal approximation.
Original language | English (US) |
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Pages (from-to) | 3345-3350 |
Number of pages | 6 |
Journal | Journal of Chemical Physics |
Volume | 112 |
Issue number | 7 |
DOIs | |
State | Published - Feb 15 2000 |