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Study of interactions between rhodamine B and a beidellite-rich clay fraction

Published online by Cambridge University Press:  06 August 2020

Hamida Belhanafi
Affiliation:
Laboratory of Biodiversity and Conservation of Soil and Water, Mostaganem University, B.P. 992 RP, Algeria
Abdellah Bakhti*
Affiliation:
Laboratory of Biodiversity and Conservation of Soil and Water, Mostaganem University, B.P. 992 RP, Algeria
Noureddine Benderdouche
Affiliation:
Laboratory of Structure, Elaboration and Application of Molecular Materials, Mostaganem University, B.P. 188, Algeria
*

Abstract

The interaction between a basic dye, rhodamine B, and a separated fine fraction from natural clay was studied. Chemical analysis, X-ray diffraction and Fourier-transform infrared spectroscopy confirmed the predominance of beidellite in the fine clay fraction. The interaction of rhodamine B with the fine clay fraction showed that sorption was fast and followed a pseudo-second-order kinetic model. The comparison between sorbed rhodamine B amounts as a function of the various experimental parameters such as pH, sorbent mass, dye concentration and the presence of competing ions suggests that: (1) the sorption process is largely pH-dependent; (2) significant competition is observed between the dye and the Ca2+ and Mg2+ ions; (3) the sorption proceeds, principally, by a cation-exchange mechanism; and (4) the sorption capacity of the fine fraction in the presence of competing cations such as Ca2+ is ~0.28 mmol g–1.

Type
Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland, 2020

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Footnotes

Associate Editor: Huaming Yang

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