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Fractal characteristics of microporous adsorbents

 
: Kutarov, Volodymyr V.; Schieferstein, Eva; Zub, Yuri Leonidovych; Robens, Erich

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Fulltext urn:nbn:de:0011-n-4736197 (1.6 MByte PDF)
MD5 Fingerprint: f4debda0525b8af02cdc92e6021554ad
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Created on: 18.11.2017


Materials sciences and applications : MSA 8 (2017), No.8, pp.603-613
ISSN: 2153-117X (Print)
ISSN: 2153-1188 (Online)
English
Journal Article, Electronic Publication
Fraunhofer UMSICHT Oberhausen ()
pore structure; micropore; fractal dimension; Dubinin's equation; mathematical analysis

Abstract
The traditional version of the theory of volume filling of micropores was used for the estimation of the fractal dimension of microporous solids. For this purpose, the Dubinin’s integral equation was solved for infinite and limited integration limits. The results were applied to the adsorption of nitrogen (T = 78 K) on coal samples and Davisil F silica and to the adsorption of water (Т = 293 К) on lunar soil sample and on rice starch. The traditional version of the theory of volume filling of micropores was used for the estimation of the fractal dimension of microporous solids. For this purpose, the Dubinin’s integral equation was solved for infinite and limited integration limits. The results were applied to the adsorption of nitrogen (T = 78 K) on coal samples and Davisil F silica and to the adsorption of water (Т = 293 К) on lunar soil sample and on rice starch. The traditional version of the theory of volume filling of micropores was used for the estimation of the fractal dimension of microporous solids. For this purpose, the Dubinin’s integral equation was solved for infinite and limited integration limits. The results were applied to the adsorption of nitrogen (T = 78 K) on coal samples and Davisil F silica and to the adsorption of water (Т = 293 К) on lunar soil sample and on rice starch.

: http://publica.fraunhofer.de/documents/N-473619.html