Hostname: page-component-586b7cd67f-t7fkt Total loading time: 0 Render date: 2024-11-23T01:51:05.680Z Has data issue: false hasContentIssue false

Orientation of Hexanediamine in Synthetic Fluorhectorite

Published online by Cambridge University Press:  02 April 2024

William Hertl
Affiliation:
Corning Inc., Research & Development Division (SP-FR-6), Corning, New York 14831
Roger F. Bartholomew
Affiliation:
Corning Inc., Research & Development Division (SP-FR-6), Corning, New York 14831
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Fourier-transform infrared (FTIR) spectroscopic studies were carried out on 1,6-hexanediamine hydrochloride (HDA)-treated synthetic fluorhectorite to determine the orientation of functional groups within the structure. Oriented crystal layers were prepared by flocculating the smectite slurry with glass fibers to obtain a 100-µm-thick paper. Orientations were determined by measuring integrated IR band intensities at various incident beam angles (≤60°), inasmuch as absorption occurred only if the oscillating dipole of the functional group interacted with the electric vector of the incident radiation. The H-N-H plane in amine groups was aligned parallel to the lamellar plane. The H-O-H plane of the small amount of sorbed water was inclined 45° or more to the interlamellar layer, and the OH groups were inclined 45° to this layer.

Even with the incorporation of HDA in the interlamellar structure, at high humidity, additional water sorbed. The sorbed water competed with and displaced amine groups from the surface, resulting in randomly oriented amine groups. Many of the amine groups were ionized, whereas the additional sorbed water showed little orientation.

This study demonstrated that the orientation of intercalated amines in fluorhectorite can be determined by following the intensity changes in infrared-active bands as a function of the incident beam angle. With intercalated HDA, the orientations were influenced by the presence of interlayer water.

Type
Research Article
Copyright
Copyright © 1990, The Clay Minerals Society

References

Adams, J. M., Martin, K. and McCabe, R. W., 1987 Clays as selective catalysts in organic synthesis J. Inclusion Phenom. 5 663674.CrossRefGoogle Scholar
Beali, G. H., Grossman, D. G., Hoda, S. N. and Kubinski, K. B., 1980 Inorganic gels and ceramic papers, films, fibers, boards, and coatings made therefrom U. S. Patent .Google Scholar
Bellamy, L. J., 1975 The Infrared Spectra of Complex Molecules, Vol. 1 3rd London Chapman and Hall 279284.CrossRefGoogle Scholar
Farmer, V.C. and Russell, J. D., 1971 Interlayer complexes in layer silicates Trans. Faraday Soc. 67 27372749.CrossRefGoogle Scholar
Fripiat, J. J., Letellier, M. and Levitz, P., 1984 Interaction of water with clay surfaces Philos. Trans. R. Soc. London Ser. A 311 287299.Google Scholar
Hoda, S. N., 1986 Ceramic mica-reinforced dimensionally stable laminates PC Fab. 9 109112.Google Scholar
Hougardy, J., Serratosa, J. M., Stone, W. and van Olphen, H., 1970 Interlayer water in vermiculite: Thermodynamic properties, packing density, nuclear pulse resonance, and infrared absorption Spec. Discuss. Faraday Soc. 1 187193.CrossRefGoogle Scholar
Jasse, B. and Koenig, J. L., 1979 Orientational measurements in polymers using vibrational spectroscopy J. Mac-romol. Sci.-Rev. Macromol. Chem. C17 61135.CrossRefGoogle Scholar
Johnston, C. F., Sposito, G., Bocian, D. F. and Birge, R. R., 1984 Vibrational spectroscopic study of the interlamellar kaolinite-dimethyl sulfoxide complex J. Phys. Chem. 88 59595964.CrossRefGoogle Scholar
Juo, A. S. R. and White, J. L., 1969 Orientation of the dipole moments of hydroxyl groups in oxidized and unox-idized biotite Science 165 804805.CrossRefGoogle ScholarPubMed
Labotka, T. C. and Rossman, G. R., 1974 The infrared pleochroism of lawsonite: The orientation of the water and hydroxide groups Amer. Mineral. 59 799806.Google Scholar
Mingelgrin, U. and Tsvetkov, F., 1985 Adsorption of di-methylanilines on montmorillonite in high-pressure chromatography Clays & Clay Minerals 33 285294.CrossRefGoogle Scholar
Odom, I. E., 1984 Smectite clay minerals; Properties and uses Philos. Trans. R. Soc. London. Ser. A 311 391409.Google Scholar
Raupach, M. and Janik, L. J., 1976 The orientation of ornithine and 6-aminohexanoic acid adsorbed on vermiculite from polarized I.R. ATR spectra Clays & Clay Minerals 24 127133.CrossRefGoogle Scholar
Rouxhet, P., Herbillon, A. and Fripiat, J. J., 1966 The relation between mica vermiculitization and OH dipole orientation Bull. Groupe Fr. Argiles 18 39.CrossRefGoogle Scholar
Serratosa, J. M. and Bailey, S. W., 1964 Infrared analysis of the orientation of pyridine molecules in clay complexes Clays and Clay Minerals, Proc. 14th Natl. Conf, Berkeley, California, 1966 New York Pergamon Press 385391.Google Scholar
Serratosa, J. M. and Bradley, W. F., 1958 Determination of the orientation of OH bond axes in layer silicates by infrared absorption J. Phys. Chem. 62 11641167.CrossRefGoogle Scholar
Serratosa, J. M., Hidalgo, A. and Vinas, J. M., 1962 Orientation of OH bonds in kaolinite Nature 195 486487.CrossRefGoogle Scholar
Serratosa, J. M., Johns, W. D. and Shimoyama, A., 1970 I.R. study of alkyl-ammonium vermiculite complexes Clays & Clay Minerals 18 107113.CrossRefGoogle Scholar
Slade, P. G., Telleria, M. I. and Radoslovich, E. W., 1976 The structures of ornithine-vermiculite and 6-aminohexanoic acid-vermiculite Clays & Clay Minerals 24 134141.CrossRefGoogle Scholar
Taylor, D. R. and Ludlum, K. H., 1972 Structure and orientation of phenols chemisorbed on 7-alumina J. Phys. Chem. 76 28822886.CrossRefGoogle Scholar