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Journal ArticleDOI

Pore size distribution and adsorption selectivity of sepiolite

Shinji Inagaki, +3 more
- 01 Mar 1990 - 
- Vol. 25, Iss: 1, pp 99-105
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TLDR
In this paper, the authors measured the micropore distribution and effective size of the channels of natural sepiolite from Turkey by the BET method, and the results showed that molecules larger than benzene could not migrate into the channels.
Abstract
Micropore distribution and effective size of the channels of natural sepiolite from Turkey were measured by the BET method. Before the BET measurement, the samples were treated under a water vapour atmosphere at various pressures to fill progressively the sepiolite micropores with water. The surface areas measured by means of N 2 adsorption decreased with increased vapour pressures of water. The outer surface area was estimated by comparison of the surface area of the vacuum-dried sepiolite with that filled with adsorbed water. The total surface area was ~290 m2/g, and the outer surface area was 170 m2/g, the difference being attributed to the structural micropores of the sepiolite. The ratio of the surface areas possessed by the channels and that of the outer surface suggest that the mean thickness of the sepiolite fibre was ~ 12 nm. The effective size of the channels was estimated from the number of various-sized molecules sorbed by the sepiolite, the results showing that molecules larger than benzene could not migrate into the channels.

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Citations
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Adsorption kinetics and mechanism of cationic methyl violet and methylene blue dyes onto sepiolite

TL;DR: In this article, the use of low-cost and ecofriendly adsorbents was investigated as an ideal alternative to the current expensive methods of removing dyes from wastewater, and it was shown that the adsorption of dyes on sepiolite was a gradual process.
Journal ArticleDOI

Molecular access to intracrystalline tunnelsof sepiolite

TL;DR: The availability of the structural micropores in sepiolite for the access of molecular or ionic entities is an old and controversial subject as discussed by the authors, which is revised in this work in the light of the most recent experimental data obtained in our research group.
Journal ArticleDOI

Adsorptive removal of methylene blue from colored effluents on fuller's earth

TL;DR: The adsorption behavior of methylene blue on four fuller's earth samples of varying compositions was investigated using a spectrophotometric technique to obtain information on the color removal and the distribution coefficient increased with an increase in the initial concentration, attained a maximum value, and decreased again at higher initial concentrations.
Journal ArticleDOI

Variability of the surface properties of sepiolite

TL;DR: In this article, a comparative study of a wide collection of sepiolites (22 samples from different locations) was made with the aim of understanding the real============variability of the surface properties in sepiolite.
Journal ArticleDOI

Effect of heating and acid pre-treatment on pore size distribution of sepiolite

TL;DR: In this article, the effects of thermal treatment on the pore structure of sepiolite and acid-treated samples were investigated, and the acid pre-activation caused restrictions in possible crystal deformation during thermal treatment.
References
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Journal ArticleDOI

Struktur und Entstehung des Sepioliths

TL;DR: The Sepiolith is a selbstandiges mineral, dem folgende strukturformel zukommt as mentioned in this paper, and it enthalt zeolithisches, Kristall, and Konstitutionswasser.
Journal ArticleDOI

Evolution of surface area in a sepiolite as a function of acid and heat treatments

TL;DR: In this article, the variations in surface area of a sepiolite (Toledo, Spain) after acid and heat treatments (1 n to 5 n, HNO3, 110, 200, 300, 400 and 500°C for 100 h) have been studied.
Journal ArticleDOI

Structural analysis of sepiolite by selected area electron diffraction; relations with physico-chemical properties

TL;DR: In this paper, the electron structural analysis of a Madagascar sepiolite (Ampandrandava) was carried out by selected area electron diffraction obtained from monocristals, and Fourier projections, derived from the experimental intensity of Okl, hOl and hkO reflections, showed that the Mg2+ cations on the edges of the sheets are distributed between two sites.