Micellization and synergistic effect in an aqueous solution of an AOS-TX100 mixture: before and after equilibrium in the presence of clay

In this research, a novel surfactant mixture consisting of anionic (alpha olefin sulfonate [AOS]) and nonionic (TX100) type was developed. Possible synergistic effect in micelle formation in different mass ratios of the mixture (1:2, 1:1, and 2:1) was studied by surface tension measurement method. R...

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Main Authors: Parak, M., Mohammadian, E., Gholamzadeh, M. A., Junin, R.
Format: Article
Published: Taylor and Francis Inc. 2015
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Online Access:http://eprints.utm.my/id/eprint/58544/
http://dx.doi.org/10.1080/10916466.2011.639320
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spelling my.utm.585442021-12-15T01:06:49Z http://eprints.utm.my/id/eprint/58544/ Micellization and synergistic effect in an aqueous solution of an AOS-TX100 mixture: before and after equilibrium in the presence of clay Parak, M. Mohammadian, E. Gholamzadeh, M. A. Junin, R. TP Chemical technology In this research, a novel surfactant mixture consisting of anionic (alpha olefin sulfonate [AOS]) and nonionic (TX100) type was developed. Possible synergistic effect in micelle formation in different mass ratios of the mixture (1:2, 1:1, and 2:1) was studied by surface tension measurement method. Rubingh's Regular Solution theory was used to evaluate the interaction parameters (β) and activity coefficient (f) for both binary mixture and single surfactants, before and after equilibrium in the presence of clay minerals (kaolinite and illite). The differences between experimentally obtained CMC values and ideally calculated values, showed nonideality of the mixtures. In addition, the lower CMC values of mixtures in comparison with individual surfactants were an indication of synergism. The synergistic effect was maintained before and after equilibrium with clay minerals. The β values of the mixture before equilibrium were in the range -1.5 to -2.6. However, after equilibrium with kaolinite, the values were in the range of -1.9 to -3.9 while after equilibrium with illite they were in the range -1 to -3. For the mixture, before and after equilibrium, the synergism became more severe as mole fractions of AOS increased in the mixture. Taylor and Francis Inc. 2015 Article PeerReviewed Parak, M. and Mohammadian, E. and Gholamzadeh, M. A. and Junin, R. (2015) Micellization and synergistic effect in an aqueous solution of an AOS-TX100 mixture: before and after equilibrium in the presence of clay. Petroleum Science And Technology, 33 (9). pp. 961-967. ISSN 1091-6466 http://dx.doi.org/10.1080/10916466.2011.639320 DOI: 10.1080/10916466.2011.639320
institution Universiti Teknologi Malaysia
building UTM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Malaysia
content_source UTM Institutional Repository
url_provider http://eprints.utm.my/
topic TP Chemical technology
spellingShingle TP Chemical technology
Parak, M.
Mohammadian, E.
Gholamzadeh, M. A.
Junin, R.
Micellization and synergistic effect in an aqueous solution of an AOS-TX100 mixture: before and after equilibrium in the presence of clay
description In this research, a novel surfactant mixture consisting of anionic (alpha olefin sulfonate [AOS]) and nonionic (TX100) type was developed. Possible synergistic effect in micelle formation in different mass ratios of the mixture (1:2, 1:1, and 2:1) was studied by surface tension measurement method. Rubingh's Regular Solution theory was used to evaluate the interaction parameters (β) and activity coefficient (f) for both binary mixture and single surfactants, before and after equilibrium in the presence of clay minerals (kaolinite and illite). The differences between experimentally obtained CMC values and ideally calculated values, showed nonideality of the mixtures. In addition, the lower CMC values of mixtures in comparison with individual surfactants were an indication of synergism. The synergistic effect was maintained before and after equilibrium with clay minerals. The β values of the mixture before equilibrium were in the range -1.5 to -2.6. However, after equilibrium with kaolinite, the values were in the range of -1.9 to -3.9 while after equilibrium with illite they were in the range -1 to -3. For the mixture, before and after equilibrium, the synergism became more severe as mole fractions of AOS increased in the mixture.
format Article
author Parak, M.
Mohammadian, E.
Gholamzadeh, M. A.
Junin, R.
author_facet Parak, M.
Mohammadian, E.
Gholamzadeh, M. A.
Junin, R.
author_sort Parak, M.
title Micellization and synergistic effect in an aqueous solution of an AOS-TX100 mixture: before and after equilibrium in the presence of clay
title_short Micellization and synergistic effect in an aqueous solution of an AOS-TX100 mixture: before and after equilibrium in the presence of clay
title_full Micellization and synergistic effect in an aqueous solution of an AOS-TX100 mixture: before and after equilibrium in the presence of clay
title_fullStr Micellization and synergistic effect in an aqueous solution of an AOS-TX100 mixture: before and after equilibrium in the presence of clay
title_full_unstemmed Micellization and synergistic effect in an aqueous solution of an AOS-TX100 mixture: before and after equilibrium in the presence of clay
title_sort micellization and synergistic effect in an aqueous solution of an aos-tx100 mixture: before and after equilibrium in the presence of clay
publisher Taylor and Francis Inc.
publishDate 2015
url http://eprints.utm.my/id/eprint/58544/
http://dx.doi.org/10.1080/10916466.2011.639320
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