Abstract
We report on the use of in-situ small angle neutron scattering (SANS) technique to study the phase behavior of hydrogen confined in narrow pores of ultramicroporous carbon (UMC) with a very large surface area (2630 m 2/g) and pore volume (1.3 cm3/g). The effect of pore size and pressure on hydrogen adsorbed on UMC at room temperature and pressures up to ∼200 bar were investigated. In a previous experiment, we have measured the density of adsorbed H2 gas in the nanopores and mesopores of polyfurfuryl alcohol-derived activated carbon (PFAC) by SANS technique. Here, a comparative SANS study between the UMC and PFAC was conducted in order to further investigate the densification of H2 as a function of pore size and pressure. Initial results suggest that the density of confined H 2 in both UMC and PFAC is considerably higher than that of the bulk hydrogen gas. The density is systematically higher in the narrow pores and decreases with increasing pore size. These results clearly demonstrate the advantage of adsorptive storage over compressed gas storage and emphasize the greater efficiency of micropores over mesopores in the adsorption process, which can be used to guide the development of new carbon adsorbents tailored for maximum H2 storage capacities at near-ambient temperatures.
| Original language | English |
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| Title of host publication | Next-Generation Energy Storage Materials and Systems |
| Pages | 37-43 |
| Number of pages | 7 |
| DOIs | |
| State | Published - 2012 |
| Event | 2012 MRS Spring Meeting - San Francisco, CA, United States Duration: Apr 9 2012 → Apr 13 2012 |
Publication series
| Name | Materials Research Society Symposium Proceedings |
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| Volume | 1440 |
| ISSN (Print) | 0272-9172 |
Conference
| Conference | 2012 MRS Spring Meeting |
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| Country/Territory | United States |
| City | San Francisco, CA |
| Period | 04/9/12 → 04/13/12 |
Funding
This research was supported by the Materials Science and Engineering Division, Office of Basic Energy Sciences, U.S. Department of Energy. SANS experiments were conducted at ORNL’s High Flux Isotope Reactor (HFIR) supported by the Scientific Users Facility Division, Office of Basic Energy Sciences, U.S. Department of Energy. H.Z. and L.H. acknowledge ORISE/ORNL postdoctoral program.