2002
DOI: 10.1006/jcis.2001.8074
|View full text |Cite
|
Sign up to set email alerts
|

Aggregation of Rhodamine 3B Adsorbed in Wyoming Montmorillonite Aqueous Suspensions

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

2
26
0
1

Year Published

2002
2002
2024
2024

Publication Types

Select...
8

Relationship

0
8

Authors

Journals

citations
Cited by 40 publications
(29 citation statements)
references
References 33 publications
2
26
0
1
Order By: Relevance
“…This can be interpreted in terms of light scattering from the clay mineral particles, or of other causes related to the interactions of the dyes at the clay mineral surface. Similar trends have frequently been observed for dye/clay mineral dispersions [29]. The lowering of the luminescence has mostly been assigned to the dye aggregation, changes in the optical properties in a more polar environment at the interfaces, self-quenching, or quenching by the clay mineral substrate itself [17,30].…”
Section: Absorption and Fluorescence Spectroscopymentioning
confidence: 78%
“…This can be interpreted in terms of light scattering from the clay mineral particles, or of other causes related to the interactions of the dyes at the clay mineral surface. Similar trends have frequently been observed for dye/clay mineral dispersions [29]. The lowering of the luminescence has mostly been assigned to the dye aggregation, changes in the optical properties in a more polar environment at the interfaces, self-quenching, or quenching by the clay mineral substrate itself [17,30].…”
Section: Absorption and Fluorescence Spectroscopymentioning
confidence: 78%
“…Intercalation of organic dyes into layered silicates is one method of producing ordered organic-inorganic hybrid materials with interesting photofunctions [1][2][3][4][5][6][7][8][9][10][11]. Especially, the smectite group is used as a very convenient host structure for the intercalation of organic dyes for two reasons.…”
Section: Introductionmentioning
confidence: 99%
“…It is interesting to mention in this context that absorption and intercalation of rhodamine 3B in various clays were studied by Lo´pez Arbeloa and co-workers [32][33]35] and found red shifts of the monomer absorption maximum by 7, 12, and 12.5 nm on montmorillonite, 10, 17, and 23 nm on Hectorite, and 10 nm on Laponite. The smaller shifts in montmorillonite and Hectorite were attributed to monomer absorption on the external clay surface and the intermediate shifts were attributed to monomer adsorption in the interlamellar regions, and the larger shifts were attributed to dimers or higher order aggregates.…”
Section: Spectroscopic Investigationmentioning
confidence: 92%
“…The adsorption of the dye in clay systems has generally been attributed to ion exchange [32][33][34][35][36], although Yariv et. al.…”
Section: Spectroscopic Investigationmentioning
confidence: 99%