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Quantification of Hydrogen Concentrations in Surface and Interface Layers and Bulk Materials through Depth Profiling with Nuclear Reaction Analysis
Published on: March 29, 2016
Hydrogen diffusion in potassium intercalated graphite studied by quasielastic neutron scattering
Justin Purewal1, J Brandon Keith, Channing C Ahn
1California Institute of Technology, W. M. Keck Laboratory 138-78, Pasadena, California 91125, USA. jjpurewal@hrl.com
This study quantifies hydrogen diffusion in potassium graphite (KC24), finding coefficients between 3.6-8.5 x 10^-9 m^2/s. These values are lower than carbon adsorbents but comparable to zeolites.
Area of Science:
- Materials Science
- Physical Chemistry
- Condensed Matter Physics
Background:
- Graphite intercalation compounds like KC24 can adsorb hydrogen.
- Hydrogen adsorption in KC24 forms a 2D condensed phase.
- Strong adsorption potentials and steric barriers are predicted to limit hydrogen diffusion in KC24.
Purpose of the Study:
- To experimentally measure and simulate hydrogen self-diffusion in KC24.
- To compare experimental diffusion data with molecular dynamics simulations.
- To understand hydrogen mobility within the KC24 host structure.
Main Methods:
- Quasielastic neutron scattering (QENS) was used to measure H2 self-diffusion.
- Molecular dynamics (MD) simulations were performed for comparison.
- Experimental spectra were fitted to a honeycomb net diffusion model.
Main Results:
- Experimental H2 diffusion coefficients in KC24 were determined.
- Values ranged from 3.6 x 10^-9 m^2/s at 80 K to 8.5 x 10^-9 m^2/s at 110 K.
- Experimental and simulated diffusion coefficients showed good agreement.
Conclusions:
- Hydrogen diffusion in KC24 is significantly slower than in carbon adsorbents.
- The measured diffusion rates are comparable to those in molecular sieve zeolites.
- The honeycomb net diffusion model accurately describes H2 mobility in KC24.
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