1961
DOI: 10.1039/tf9615700452
|View full text |Cite
|
Sign up to set email alerts
|

Thermodynamics of interlamellar complexes. Part 1.—Hydrocarbons in methylammonium montmorillonites

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

2
6
0

Year Published

1962
1962
1996
1996

Publication Types

Select...
9

Relationship

0
9

Authors

Journals

citations
Cited by 29 publications
(8 citation statements)
references
References 2 publications
2
6
0
Order By: Relevance
“…This is a severe restriction to place on the use of the equation since in such systems it is probable that there would be a high degree of orientation. Barrer and Kelsey 25 have discussed the problem of the application of thermodynamic functions to clay adsorption systems and have concluded that at least qualitatively correct interpretations of prominent physical aspects should be obtained. For their particular two-component systems, of hydrocarbon adsorption by alkyl ammonium montmorillonites, no other procedure could be used with comparable qualitative success.…”
Section: X-ray Datamentioning
confidence: 99%
“…This is a severe restriction to place on the use of the equation since in such systems it is probable that there would be a high degree of orientation. Barrer and Kelsey 25 have discussed the problem of the application of thermodynamic functions to clay adsorption systems and have concluded that at least qualitatively correct interpretations of prominent physical aspects should be obtained. For their particular two-component systems, of hydrocarbon adsorption by alkyl ammonium montmorillonites, no other procedure could be used with comparable qualitative success.…”
Section: X-ray Datamentioning
confidence: 99%
“…Depending of the number of carbon atoms, the alkyl anol immersion calorimetry. chains arrange themselves parallel to the sheets as a monolayer or a bilayer (4,5). When there are more than 18 carbon…”
Section: Introductionmentioning
confidence: 99%
“…The resulting organic cation substituted clay is called an "organoclay". In the 1950s and 1960s, it was shown that the sorption of vapors of nonionic organic liquids to organoclays was substantially greater than sorption to Naor Ca-clays (9)(10)(11)(12)(13)(14)(15)(16)(17)(18)(19), and these results have been summarized elsewhere (8,20). It was determined that the intercalated organic cations act as "props" that hold apart the silicate layers, allowing nonionic organic vapors to be intercalated and sorbed.…”
Section: Introductionmentioning
confidence: 99%