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Fractality of Porous Silicas: A Comparison of Adsorption and Porosimetry Data

โœ Scribed by Alexander Yu. Fadeev; Olga R. Borisova; George V. Lisichkin


Publisher
Elsevier Science
Year
1996
Tongue
English
Weight
94 KB
Volume
183
Category
Article
ISSN
0021-9797

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โœฆ Synopsis


sions given in (10,11). The authors (16, 17) suggest that The fractal dimensions of seven porous silicas were determined solids that are synthesized via a sol-gel procedure can have by means of gas adsorption, chemisorption of chlorosilanes, and a fractal surface only as an exception but not as a rule. mercury porosimetry. The silicas under investigation are shown The fractality of silicas and other porous solids was studto be surface fractals in the range of cross-sectional areas from ied by means of several physicochemical techniques: adsorp-0.162 (N 2 ) to 1.450 sq. nm ((C 6 H 13 ) 3 SiCl). The surface fractal tion from gases and liquids (4, 18-22), mercury porosimedimensions obtained range from 2.05 to 2.90. On the other hand, try (4, 6, 23), small angle X-ray scattering (24-26), elecmercury porosimetry data show that the silicas studied can be tron microscopy (27), energy transfer between adsorbed hardly considered as pore fractals within the range of a pore radius molecules (28-34), and others. A central technique in the from 3.5 to 1000 nm. The apparent contradiction is discussed in the text.


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