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Molecular-dynamics analysis of the diffusion of molecular hydrogen in all-silica sodalite
Author(s) -
Annemieke W. C. van den Berg,
Stefan T. Bromley,
Edwin Flikkema,
Jacek C. Wojdeł,
Thomas Maschmeyer,
J.C. Jansen
Publication year - 2004
Publication title -
the journal of chemical physics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.071
H-Index - 357
eISSN - 1089-7690
pISSN - 0021-9606
DOI - 10.1063/1.1737368
Subject(s) - sodalite , molecular dynamics , transition state theory , arrhenius equation , hydrogen , thermodynamics , diffusion , activation energy , atmospheric temperature range , chemistry , chemical physics , effective diffusion coefficient , extrapolation , molecular diffusion , materials science , computational chemistry , kinetics , reaction rate constant , physics , organic chemistry , zeolite , operations management , mathematics , mathematical analysis , metric (unit) , magnetic resonance imaging , quantum mechanics , radiology , catalysis , medicine , economics
In order to investigate the technical feasibility of crystalline porous silicates as hydrogen storage materials, the self-diffusion of molecular hydrogen in all-silica sodalite is modeled using large-scale classical molecular-dynamics simulations employing full lattice flexibility. In the temperature range of 700-1200 K, the diffusion coefficient is found to range from 1.610(-10) to 1.810(-9) m(2)/s. The energy barrier for hydrogen diffusion is determined from the simulations allowing the application of transition state theory, which, together with the finding that the pre-exponential factor in the Arrhenius-type equation for the hopping rate is temperature-independent, enables extrapolation of our results to lower temperatures. Estimates based on mass penetration theory calculations indicate a promising hydrogen uptake rate at 573 K.

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