2010
DOI: 10.1016/j.clay.2010.04.017
|View full text |Cite
|
Sign up to set email alerts
|

Alkyl ammonium intercalation of Mozambican bentonite

Abstract: Organo-bentonites containing quaternary ammonium surfactants were prepared using purified bentonite from the Boane deposit in Mozambique. The intercalation was effected by intimate mixing of the surfactants into a concentrated dispersion of soda ash activated bentonite. TG indicated organic contents that exceeded CEC expectations by up to 21 mass %. XRD results were consistent with: (i) paraffin-type extended chain intercalation at tilt angles of 27 º to 33 º; and (ii) interdigitated monolayer intercalation of… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

3
18
0

Year Published

2012
2012
2021
2021

Publication Types

Select...
8

Relationship

3
5

Authors

Journals

citations
Cited by 30 publications
(25 citation statements)
references
References 48 publications
3
18
0
Order By: Relevance
“…Moreover, the total amounts of waters removed from organosmectites below 200 • C are less than that of NaS and the elimination of the adsorbed waters from organosmectites occur at lower temperatures. This situation can be explained with the reduction of the surface energy and conversion of the silicate surface from hydrophilicity to hydrophobicity, which is in agreement with the results of the previously reported FTIR-ATR studies [24,26,36,41]. The thermal decomposition of organosmectites occurs in three stages: the dehydration of adsorbed water up to 140 • C, and then the decomposition of surfactant molecules which is followed by the dehydroxylation of smectite hydroxyl groups together with decomposition of organic carbonaceous residue of the surfactants, from 50 to 720 • C. The differentiation of the mass losses originating from dehydroxylation of smectite and decomposition of the organic cations by using the TG curves is highly difficult [80].…”
Section: Thermal Analysis Data Of Samplessupporting
confidence: 91%
“…Moreover, the total amounts of waters removed from organosmectites below 200 • C are less than that of NaS and the elimination of the adsorbed waters from organosmectites occur at lower temperatures. This situation can be explained with the reduction of the surface energy and conversion of the silicate surface from hydrophilicity to hydrophobicity, which is in agreement with the results of the previously reported FTIR-ATR studies [24,26,36,41]. The thermal decomposition of organosmectites occurs in three stages: the dehydration of adsorbed water up to 140 • C, and then the decomposition of surfactant molecules which is followed by the dehydroxylation of smectite hydroxyl groups together with decomposition of organic carbonaceous residue of the surfactants, from 50 to 720 • C. The differentiation of the mass losses originating from dehydroxylation of smectite and decomposition of the organic cations by using the TG curves is highly difficult [80].…”
Section: Thermal Analysis Data Of Samplessupporting
confidence: 91%
“…35.7 wt.% crystobalite as a major impurity [22]. The ammonium-modified bentonite showed a significant reduction in the sodium (2.11%) and calcium (0.39%) levels (described in terms of Na 2 O and CaO respectively).…”
Section: Clay Characterizationmentioning
confidence: 97%
“…The peaks at 2924 and 2850 cm −1 are attributed to the asymmetric and symmetric stretching vibrations of the methylene groups (\CH 2 − ) of aliphatic chains (Shah et al, 2013). The peak positions of the methylene asymmetric bands reflect the interlayer structure of OMts and the packing density of the chain methylenes (Massinga et al, 2010). The peaks near 2924 cm − 1 were shifted from 2929 cm −1 for 1231Mt to 2919.3 cm −1 for D1821Mt.…”
Section: Ftir Analysis Of Natural and Organically Modified Mtsmentioning
confidence: 98%