Hostname: page-component-848d4c4894-4rdrl Total loading time: 0 Render date: 2024-06-15T12:46:55.369Z Has data issue: false hasContentIssue false

Characterization of Montmorillonite Saturated with Short-Chain Amine Cations: 2. Interlayer Surface Coverage by the Amine Cations

Published online by Cambridge University Press:  01 January 2024

Earl B. Kinter
Affiliation:
Physical Research Division, Bureau of Public Roads, Washington, D.C., USA
Sidney Diamond
Affiliation:
Physical Research Division, Bureau of Public Roads, Washington, D.C., USA

Abstract

Portions of Wyoming bentonite were saturated with a series of short-chain aliphatic amine and quaternary ammonium cations, and the amine content remaining after washing was determined by combustion analysis. For those amine cations containing one or two carbon atoms, the amount of amine found was greatly in excess of the cation-exchange capacity. It is thought that this excess consists of amine cations or uncharged amine molecules which have become partly embedded in the holes associated with the oxygen rings of the silica sheet surfaces. For the larger tertiary amine cations, slightly less than the exchange capacity was found, presumably owing to blocking of some exchange sites by steric interference.

Upon treatment of the amine-saturated clays with glycerol and quantitative determination of the glycerol retained as a monolayer, it was found that these clays retain considerably less glycerol than the original bentonite. The glycerol retention values were employed to provide quantitative estimates of the interlayer clay surface left unoccupied between cation pillars. The percentage of original interlayer surface left unoccupied ranged from about 75 percent for methylamine to essentially zero for the larger tertiary amine cations.

The validity of the areas calculated from the glycerol retention results was indirectly confirmed by deriving estimates of the cross-sectional areas of the several cations from the observed reductions in amount of glycerol retained. These experimentally derived cross-sectional areas were found to be in satisfactory agreement with areas of the cations projected from atom models.

Type
Symposium on Clay-Organic Complexes
Copyright
Copyright © Clay Minerals Society 1961

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Barrer, R. M. and MacLeod, D. M. (1955) Activation of montmorillonite by ion-exchange and sorption complexes of tetra-alkyl ammonium montmorillonite: Trans. Faraday Soc., v. 51, pp. 12901300.CrossRefGoogle Scholar
Barrer, R. M. and Reay, J. S. S. (1957) Sorption and intercalation by methyl ammonium montmorillonites: Trans. Faraday Soc., v. 53, pp. 12531261.CrossRefGoogle Scholar
Barrer, R. M. and Reay, J. S. S. (1958) Sorption by NH4+"-Cs+-montmorillonites, and ion fixation: J. Chem. Soc., pp. 38243830.CrossRefGoogle Scholar
Brindley, G. W. and Hoffman, R. W. (1962) Orientation and packing of aliphatic chain molecules on montmorillonite: in Clays and Clay Minerals, v. 9, Pergamon Press, New York, pp. 546556.CrossRefGoogle Scholar
Cowan, C. T. and White, D. (1958) The mechanism of exchange reactions occurring between sodium montmorillonite and various η-primary aliphatic amine salts: Trans. Faraday Soc., v. 54, pp. 691697.CrossRefGoogle Scholar
Diamond, Sidney and Kinter, E. B. (1958) Surface areas of clay minerals as derived from measurements of glycerol retention: in Clays and Clay Minerals, Nat. Acad. Sci. -Nat. Res. Council, pub. 566, pp. 334347.Google Scholar
Diamond, Sidney and Kinter, E. B. (1962) Characterization of montmorillonite saturated with short-chain amine cations, 1. Interpretation of basal spacing measurements: This volume.CrossRefGoogle Scholar
Dyal, R. S. and Hendricks, S. B. (1950) Total surface of clays in polar liquids as characteristic index: Soil Science, v. 69, pp. 421432.CrossRefGoogle Scholar
Greene-Kelly, R. (1956) The swelling of organophilic montmorillonites in liquids: J. Colloid Science, v. 11, pp. 7779.CrossRefGoogle Scholar
Grim, R. E. (1953) Clay Mineralogy: McGraw-Hill, New York, 384 pp.Google Scholar
Grim, R. E., Allaway, W. H. and Cuthbert, F. L. (1947) Reaction of different clay minerals with some organic cations: J. Amer. Ceramic Soc., v. 30, pp. 137142.CrossRefGoogle Scholar
Hendricks, S. B. (1941) Base-exchange of the clay mineral montmorillonite for organic cations and its dependence upon adsorption due to van dor Waals' Forces: J. Phys. Chem., v. 45, pp. 6581.CrossRefGoogle Scholar
Hendricks, S. B., Nelson, R. A. and Alexander, L. T. (1940) Hydration mechanism of the clay mineral montmorillonite saturated with various cations: J. Amer. Chem. Soc., v. 62, pp. 14571464.CrossRefGoogle Scholar
Jackson, M. L. (1956) Soil Chemical Analysis—Advanced Course: published by the author, University of Wisconsin, Madison 6, Wise.Google Scholar
Jackson, M. L. (1958) Soil Chemical Analysis: Prentice-Hall, Inc., Englewood Cliffs, N.J.Google Scholar
Kinter, E. B. and Diamond, S. (1958) Gravimetric determination of mono-layer glycerol complexes of clay minerals: in Clays and Clay Minerals, Nat. Acad. Sci.-Nat. Res. Council, pub. 566, pp. 318333.Google Scholar
Kinter, E. B. and Diamond, S. (1960) Pretreatment of soils and clays for measuring external surface area by glycerol retention: in Clays and Clay Minerals, 7th Conf., Pergamon Press, New York, pp. 125134.Google Scholar
McAtee, J. L. Jr. (1959) Inorganic-organic cation exchange on montmorillonite: Amer. Min., v. 44, pp. 12301236.Google Scholar
Mooney, R. W., Keenan, A. G. and Wood, L. A. (1952) Adsorption of water vapor by montmorillonite. I. Heat of desorption and application of B.E.T. theory: J. Amer. Chem. Soc., v. 74, pp. 13671371.CrossRefGoogle Scholar
Morel, R. (1958) Observations surla capacité d'échange et les phénomènes d'échange dans les argiles: Bul. du groupe français des argiles, v. 10, pp. 37.CrossRefGoogle Scholar
Rowland, R. A. and Weiss, E. J. (1962) Betonite-methyl amine complexes: This volume.Google Scholar
Slabaugh, W. H. and Kupka, F. (1958) Organic cation exchange properties of calcium montmorillonite: J. Phys. Chem., v. 62, pp. 599601.CrossRefGoogle Scholar
Weiss, A. (1958) Uber des Kationenaustauch vermögen der Tonminerale—II. Der Kationenaustauch bei den Mineralen der Glimmer-, Vermikulit- und Montmorillonitgruppe: Z. Anorg. Allg. Chemie, v. 297, pp. 257286.CrossRefGoogle Scholar