Hostname: page-component-586b7cd67f-dsjbd Total loading time: 0 Render date: 2024-11-22T23:21:40.070Z Has data issue: false hasContentIssue false

Effect of Hydrostatic Pressure on the Swelling of n-Butylammonium Vermiculite

Published online by Cambridge University Press:  02 April 2024

M. V. Smalley
Affiliation:
Physical Chemistry Laboratory, South Parks Road, Oxford, OX1 3QZ, United Kingdom
R. K. Thomas
Affiliation:
Physical Chemistry Laboratory, South Parks Road, Oxford, OX1 3QZ, United Kingdom
L. F. Braganza
Affiliation:
Institut Laue-Langevin, Grenoble 38042 Cedex, France
T. Matsuo
Affiliation:
Chemical Thermodynamics Laboratory, University of Osaka, Toyonaka, Osaka 560, Japan
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.

The osmotic swelling of an n-butylammonium vermiculite in a 0.1 M solution of n-butylammonium chloride has been studied as a function of temperature and hydrostatic pressure by neutron diffraction. On application of a pressure of 1050 bar the vermiculite swelled macroscopically at 20°C, the c-axis spacing changing from 19.4 to 126 Å. The phase transition was completely reversible with respect to both pressure and temperature, and a complete study of the temperature-pressure phase diagram was made at pressures as high as 2000 bar. The heat capacity change with temperature across the swelling transition was measured at atmospheric pressure, and the enthalpy and entropy of the change from crystalline to osmotic phases were found to be, respectively, 5.2 J/g and 0.0183 J/K·g of dry clay. The combination of the entropy change with the gradient of the pressure-temperature phase boundary gave the volume change accompanying the transition. The total volume of the swollen phase was less than that of the crystalline phase plus the appropriate amount of solution, corresponding to a fractional decrease of about 0.1% in the water volume from bulk solution to between the plates.

Type
Research Article
Copyright
Copyright © 1989, The Clay Minerals Society

References

Braganza, L. F., Crawford, R. J., Smalley, M. V. and Thomas, R. K. (1989) Swelling of n-butyl ammonium vermiculite in water: Clays & Clay Minerals 37 (in press).Google Scholar
Braganza, L. F. and Worcester, D. L., 1986 Hydrostatic pressure induces hydrocarbon chain interdigitation in single component phospholipid bilayers Biochemistry 25 25912596.CrossRefGoogle ScholarPubMed
Derjaguin, B. V., Churaev, N. V. and Muller, V. M., 1987 Surface Forces New York Plenum 293295.CrossRefGoogle Scholar
Garrett, W. G., Walker, G. F. and Swineford, A., 1962 Swelling of some vermiculite-organic complexes in water Clays and Clay Minerals New York Pergamon Press 557567.CrossRefGoogle Scholar
Humes, R. P., 1985 Interparticle forces in clay minerals United Kingdom Oxford University, Oxford.Google Scholar
Hunter, R. J., 1987 Foundations of Colloid Science Oxford Clarendon Press 428431.Google Scholar
Institut Laue-Langevin, 1986 Neutron Research Facilities at the High High Flux Reactor Grenoble, France Institut Laue-Langevin.Google Scholar
Low, P. F., 1987 Structural component of the swelling pressure of clays Langmuir 3 1825.CrossRefGoogle Scholar
Matsuo, T. and Suga, H., 1985 Adiabatic calorimeters for heat capacity measurement at low temperature Thermochimica Acta 88 149158.CrossRefGoogle Scholar
Norrish, K., Rausel-Colom, J. A., Swineford, A. and Franks, P. C., 1963 Low angle X-ray diffraction studies of the swelling of montmorillonite and vermicuite Clays and Clay Minerals New York Pergamon Press 123149.Google Scholar
Rausel-Colom, J. A., 1964 Small angle X-ray diffraction study of the swelling of butylammonium vermiculite Trans. Far. Soc 60 190201.CrossRefGoogle Scholar
van Olphen, H., 1977 An Introduction to Clay Colloid Chemistry 2nd ed. New York Wiley 150161.Google Scholar
Walker, G. F., 1960 Macroscopic swelling of vermiculite crystals in water Nature 187 312313.CrossRefGoogle Scholar