ANALYSIS OF THE DERIVED CURVES OF ADSORPTION-ISOTHERMS

Citation
F. Ehrburgerdolle, ANALYSIS OF THE DERIVED CURVES OF ADSORPTION-ISOTHERMS, Langmuir, 13(5), 1997, pp. 1189-1198
Citations number
33
Categorie Soggetti
Chemistry Physical
Journal title
ISSN journal
07437463
Volume
13
Issue
5
Year of publication
1997
Pages
1189 - 1198
Database
ISI
SICI code
0743-7463(1997)13:5<1189:AOTDCO>2.0.ZU;2-Z
Abstract
The paper aims to provide new insights into the mechanism of adsorptio n of nitrogen at 77 K in the submonolayer range, by means of analysis of the isotherm derivative d[N(p)]/dp. For this purpose, a series of i sotherms of adsorption on different types of carbons are analyzed. In order to investigate deterministic isotherms, a series of isotherms of adsorption in slit-shaped micropores, calculated by Lastoskie er al., are analyzed by the same method. It is shown that the derivatives can always be fitted to power laws, i.e., d[N(p)]/dp proportional to p(v) where -2 less than or equal to v less than or equal to 0. For carbons ,several regimes, characterized by different v values are evidenced. I n contrast, for silicas, a single power law (-1 less than or equal to v less than or equal to -0.5) is evidenced over a broad range of relat ive pressures (10(-6)-0.2). It yields a Freundlich equation after inte gration, whereas more than one equation is needed to describe adsorpti on on carbons. Depending on v, integration yields Henry, Freundlich, o r Temkin equations or a new one (''C-type''), involving a negative exp onent for p. Dubinin-Radushkevich plots, largely used for carbons, are also shown. The comparison with the derivatives provides explanation for the usual deviations from the DR equation. The exponent v is relat ed to a fractal dimension D by means of the following relation: v (D - 4)/2. The physical meaning of D is discussed. When the solid surface is fractal, the upper value of D-s, which is deduced from v, is compar ed to the ones obtained by other methods. This work also provides a th eoretical background for some usual empirical isotherm equations.