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Effect of Hydrocarbon Chain Length on Adsorption of Cationic Surfactants onto Clinoptilolite

Published online by Cambridge University Press:  01 January 2024

Bahri Ersoy  and
Mehmet S. Çelik
Bahri Ersoy*
Affiliation:
Afyon Kocatepe University, Engineering Faculty, Mining Engineering Department, 03100 Afyon, Turkey
Mehmet S. Çelik
Affiliation:
İstanbul Technical University, Mining Faculty, Minerals and Coal Processing Section, Ayazaga, 80626, Istanbul, Turkey
*
*E-mail address of corresponding author: [email protected]
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Abstract

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The adsorption behavior of quaternary ammonium cationic surfactants with different hydrocarbon chain lengths, i.e. HDTMA (hexadecyltrimethylammonium), TDTMA (tetradecyltrimethylammonium) and DDTMA (dodecyltrimethylammonium), onto clinoptilolite has been investigated. The adsorption isotherms of these surfactants are correlated with the ζ potential curves of clinoptilolite. Accordingly, the applicability of the hemimicelle hypothesis to the adsorption of cationic surfactants at the clinoptilolite/water interface considering in the electrical double layer (EDL) of clinoptilolite is discussed. Even though the adsorption occurs in the EDL of clinoptilolite, the adsorption of HDTMA, TDTMA and DDTMA onto clinoptilolite is not conveniently described by the hemimicelle hypothesis. The absence of all expected marked increase in the ζ potential curves at the hemimicelle concentration is ascribed to the large external cation exchange capacity of clinoptilolite. The hydrocarbon chain length of surfactant molecules is found to have a significant effect on the ion exchange as well as hydrophobic interaction mechanisms. The effectiveness of both ion exchange and hydrophobic interactions increases with increasing chain length, and so the greatest surfactant adsorption onto clinoptilolite was obtained by HDTMA.

Keywords

AdsorptionCationic SurfactantClinoptiloliteDouble LayerHydrophobic InteractionIon Exchangeζ Potential
Type
Research Article
Information
Clays and Clay Minerals , Volume 51 , Issue 2 , April 2003 , pp. 172 - 180
Copyright
Copyright © 2003, The Clay Minerals Society

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