Abstract
We present a detailed comparison between experimental adsorption measurements and the excess adsorption predicted by the Ono−Kondo equations. The study was done for high-pressure adsorption of methane above the critical point on microporous adsorbents. The experimental adsorption isotherms of CH4 on the activated carbon CNS-201 as well as others are compared with theory over the temperature range 243−333 K and for pressures up to 16 MPa. Extension of the model to zeolites is also discussed.
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