2005
DOI: 10.1016/j.jcis.2004.10.070
|View full text |Cite
|
Sign up to set email alerts
|

Interaction between cationic surfactants and montmorillonites under nonequilibrium condition

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

1
25
0
3

Year Published

2011
2011
2018
2018

Publication Types

Select...
7
1
1

Relationship

0
9

Authors

Journals

citations
Cited by 60 publications
(29 citation statements)
references
References 22 publications
1
25
0
3
Order By: Relevance
“…For all the OMt, their basal spacings can reach a relative stable value within 0.5 h, and this is in agreement with the reports about quick adsorption of CTMA on montmorillonite [40]. While in the aging process the OMt always show the decrease of basal spacing values.…”
Section: Possible Structure Of Wet Omtsupporting
confidence: 91%
“…For all the OMt, their basal spacings can reach a relative stable value within 0.5 h, and this is in agreement with the reports about quick adsorption of CTMA on montmorillonite [40]. While in the aging process the OMt always show the decrease of basal spacing values.…”
Section: Possible Structure Of Wet Omtsupporting
confidence: 91%
“…The peaks observed between 1200 and 400 cm -1 are characteristic of silicate backbone: the bands at 1204, 1050 and 806 cm -1 are assigned to Si-O bond stretching vibration of Si-O-Si group [35]. The bands at 647 and 696 cm -1 correspond to Si-O stretching and Mg-OH bond vibration respectively [36].…”
Section: Modification Of Sepiolite By Graffing Of Orgnosilanesmentioning
confidence: 99%
“…At the opposite, the implication of fibrous clay minerals for electroanalytical purposes is scarce, although many works in literature have been devoted to their chemical modification [24][25][26][27][28]. Depending on the nature of the clay mineral, the preparation of organic-inorganic clay-based composite materials, exploited as electrode material proceeds mainly by two processes: (1) the intercalation of organic molecules within layered clay minerals such as kaolinite [29][30][31][32] and montmorillonite [1,[33][34][35][36], and (2) the grafting of functionalized organic molecules onto the surface of clay minerals [6,[37][38][39][40]. This last approach is convenient for all types of clay minerals bearing hydroxyl groups (aluminol or silanol) in their structure since it leads to the irreversible binding of the organic molecule on the clay surface.…”
Section: Introductionmentioning
confidence: 99%
“…These interlayer cations can be easily replaced in aqueous solutions by more voluminous ones, and quaternary alkylammonium cations (also known as surfactants) are the mostly used to that purposes. Within the interlayer region of the hosting clay mineral, the surfactant molecules can adopt a monolayer, a bilayer, a pseudotrimolecular or a paraffin layer depending on their concentration in relation with the cation exchange capacity of the clay mineral [18,19]. It is important to mention that other kinds of organic groups can be used, the final aim being the elaboration of composite materials with both hydrophilic and hydrophobic surfaces as well as a large porosity and surface area that have been proven to be efficient sorbents for organic molecules.…”
Section: Ion Exchange (Class 1)mentioning
confidence: 99%