1999
DOI: 10.1039/a907860f
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Preparation, thermal stability and decomposition routes of clay/Triton-X100 composites

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Cited by 23 publications
(21 citation statements)
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“…This could be due to the fact that the molecule of TX100 is too big to intercalate between the interlayer space; therefore, expansion of the interlayer space was not significant, and the modification of bentonite with TX100 was seen mostly on the surface. This result is consistent with the results reported by Breen et al [49], who did not observe a significant change in basal spacing of montmorillonite after absorption of TX100.…”
Section: Resultssupporting
confidence: 94%
See 1 more Smart Citation
“…This could be due to the fact that the molecule of TX100 is too big to intercalate between the interlayer space; therefore, expansion of the interlayer space was not significant, and the modification of bentonite with TX100 was seen mostly on the surface. This result is consistent with the results reported by Breen et al [49], who did not observe a significant change in basal spacing of montmorillonite after absorption of TX100.…”
Section: Resultssupporting
confidence: 94%
“…Nonionic surfactants are rarely used in the modification of clay minerals; nevertheless, the properties of such hybrid materials are highly promising [1,11,40,41,42,43,44,45,46,47]. In addition, t -octylphenoxypolyethoxyethanol (Triton X-100 (TX100)) is one of the most popular nonionic surfactants in terms of clay modification [11,48,49,50,51,52,53]; however, the interaction of bentonite with TX100 has not been studied extensively.…”
Section: Introductionmentioning
confidence: 99%
“…For the longer-chain derivatives, the amount of end-groups enriched in the interlayer space is too small to exert deviations of the basal spacing from 1.7 nm.) The formation of helical arrangements cannot be excluded (Aranda & Ruiz-Hitzky, 1992, 1999Wu & Lerner, 1993;Billingham et al, 1997;Breen et al, 1998Breen et al, , 1999Sonon & Thompson, 2005;Deng et al, 2003Deng et al, , 2006. As the basal spacing of the Ca 2+ -montmorillonite particles in water is comparable to the basal spacing required for poly(ethylene oxide) intercalation (~1.7 nm), sterical hindrance does not impede interlamellar poly(ethylene oxide) adsorption.…”
Section: Fig 3 Fields Of Sol and Flocs For Ca 2+ -Montmorillonitementioning
confidence: 99%
“…The negative charges at both ends of the PEO chain do not impede or reduce the adsorption on Na-and Ca-montmorillonite. The reason is the optimal fit between the ethylene oxide groups and the surface oxygen atoms which causes strong van der Waals interactions between the ethylene oxide segments and the silicate layers (Lagaly & Ziesmer, 2006) (Parfitt & Greenland, 1970;Zhao et al, 1989;Ruiz-Hitzky & Aranda, 1990;Aranda & Ruiz-Hitzky, 1992, 1999Ruiz-Hitzky, 1993;Breen et al, 1998Breen et al, , 1999Bujdák et al, 2000;Smalley et al, 2001;Strawhecker & Manias, 2003;Deng et al, 2003Deng et al, , 2006Sonon & Thompson, 2005). We calculated that approximately half of the total amount of ethylene oxide units of the adsorbed cationic PEOs were intercalated.…”
Section: Discussionmentioning
confidence: 98%