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Swelling Pressure of Montmorillonite Layers Versus H-O-H Bending Frequency of the Interlayer Water

Published online by Cambridge University Press:  28 February 2024

Laibin Yan
Affiliation:
Department of Agronomy, Purdue University, West Lafayette, Indiana 47907-1150
Philip F. Low
Affiliation:
Department of Agronomy, Purdue University, West Lafayette, Indiana 47907-1150
Charles B. Roth
Affiliation:
Department of Agronomy, Purdue University, West Lafayette, Indiana 47907-1150
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Abstract

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The in-depth perturbation of vicinal water by the surfaces of montmorillonite layers was investigated by relating the swelling pressure, Π, of the montmorillonite layers to the H-O-H bending frequency, ν2, of the interlayer water. For this purpose, an oriented montmorillonite gel was deposited on a porous filter in an environmental chamber. On its underside the filter was in contact with a solution maintained at atmospheric pressure. By admitting nitrogen gas at a known pressure to the environmental chamber, water was squeezed from the gel into the solution until equilibrium was reached and Π equalled the applied pressure. Then the gel was divided into 2 parts. One part was used for the gravimetric determination of the water content, mw/mc. It was possible, therefore, to determine mw/mc as a function of Π. The other part of the sample was transferred to an FTIR spectrometer where the ν2 of the water within it was measured by attenuated total reflectance. Thus, the same samples were used to determine the dependence of both Π and ν2 on mw/mc. It was found that Π and ν2 were both exponential functions of mc/mw and so a linear relation was found between ln(Π + 1) and ln(ν22°), where ν2° is the H-O-H bending frequency of bulk water. These results strongly support the conclusion that the in-depth perturbation of the water by the surfaces of the montmorillonite layers is primarily responsible for both the development of Π and the departure of ν2 from ν2°.

Type
Research Article
Copyright
Copyright © 1996, The Clay Minerals Society

References

Achanta, S., Cushman, J.H. and Okos, M.R.. 1994. On multicomponent, multiphase thermomechanics with interfaces. Int J Eng Sci 32: 17171738.CrossRefGoogle Scholar
Achanta, S. and Cushman, J.H.. 1994. Nonequilibrium swelling-and capillary-pressure relations for colloidal systems. J Colloid Interface Sci 168: 266268.CrossRefGoogle Scholar
Anderson, D.M. and Low, P.F.. 1958. The density of water adsorbed by lithium-, sodium-, and potassium-bentonite. Soil Sci Soc Am Proc 22: 99103.CrossRefGoogle Scholar
Barclay, L.M. and Ottewill, R.H.. 1970. Measurement of forces between colloidal particles. Special Discuss Faraday Soc 1: 138147.CrossRefGoogle Scholar
Callaghan, I.C. and Ottewill, R.H.. 1975. Interparticle forces in montmorillonite gels. Faraday Discuss Chem Soc 57: 110118.CrossRefGoogle Scholar
Clementz, D.M. and Low, P.F.. 1976. Thermal expansion of inter-layer water in clay systems. In: Kerker, M., editor. Colloid interface science, vol 3. New York: Academic Pr. p 485502.CrossRefGoogle Scholar
Derjaguin, B.V. and Churaev, N.V.. 1974. Structural component of disjoining pressure. J Colloid Interface Sci 49: 249255.CrossRefGoogle Scholar
Falk, M.. 1984. The frequency of the H-O-H bending fundamental in solids and liquids. Spectrochim Acta 40A: 4348.CrossRefGoogle Scholar
Falk, M., Flakus, H.T. and Boyd, R.J.. 1986. An ab initio SCF calculation of the effect of water-anion and water-cation interactions on the vibrational frequencies of water. Spectrochim Acta 42A: 175180.CrossRefGoogle Scholar
Fripiat, J.J., Chaussidon, J. and Touillaux, R.. 1960. Study of dehydration of montmorillonite and vermiculite by infrared spectroscopy. J Phys Chem 64: 12341241.CrossRefGoogle Scholar
Fu, M.H., Zhang, Z.Z. and Low, P.F.. 1990. Changes in the properties of a montmorillonite-water system during the adsorption and desorption of water. Hysteresis. Clays Clay Miner 38: 485492.CrossRefGoogle Scholar
Gan, H.. 1990. Factors affecting the interparticle bond energies of Na-montmorillonite [dissertation]. West Lafayette, IN: Purdue Univ. 155 p.Google Scholar
Greinacher, E., Lüttke, W. and Mecke, R.. 1955. Infrareotspektros-kopische untersuchungen an Wasser, gelöst in organischen Lösungsmitteln. Z Electrochem 59: 2331.Google Scholar
Grodzicki, A. and Piszczek, P.. 1994. Influence of structural factors on water molecule bending vibration frequencies in crystalline hydrates. Polish J Chem 68: 26872697.Google Scholar
Israelachvili, J.N. and Adams, G.E.. 1978. Measurement of forces between two mica surfaces in aqueous electrolyte solutions in the range 0-100 nm. J Chem Soc Faraday Trans I 74: 9751001.CrossRefGoogle Scholar
Jorgensen, P.. 1968. I. R. study of water adsorbed on Wyoming bentonite. Geologiska Føren Stochholm Førh 90: 213220.Google Scholar
Johnston, C.T., Sposito, G. and Erickson, C.. 1992. Vibrational probe studies of water interactions with montmorillonite. Clays Clay Miner 40: 722730.CrossRefGoogle Scholar
Kay, B.D. and Low, P.F.. 1975. Heats of compression of clay-water mixtures. Clays Clay Miner 23: 266271.CrossRefGoogle Scholar
Kjellander, R. and Marcelja, S.. 1985. Perturbation of hydrogen bonding in water near polar surfaces. Chem Phys Lett 120: 393396.CrossRefGoogle Scholar
Low, P.F.. 1976. Viscosity of interlayer water in montmorillonite. Soil Sci Soc Am J 40: 500505.CrossRefGoogle Scholar
Low, P.F.. 1979. Nature and properties of water in montmo-rillonite-water systems. Soil Sci Soc Am J 43: 651658.CrossRefGoogle Scholar
Low, P.F.. 1980. The swelling of clay. II. Montmorillonites. Soil Sci Soc Am J 44: 667676.CrossRefGoogle Scholar
Low, P.F.. 1987a. Structural component of the swelling pressure of clays. Langmuir 3: 1825.CrossRefGoogle Scholar
Low, P.F.. 1987b. The clay-water interface. In: Schultz, L.G., van Olphen, H., Mumpton, F.A., editors. Proceedings of the International Clay Conference; Denver, CO; 1985. Bloomington, IN: Clay Miner Soc. p 247256.Google Scholar
Low, P.F.. 1992. Interparticle forces in clay suspensions, flocculation, viscous flow and swelling. In: Güven, N., Pollastro, R.M., editors. Clay-water interface and its rheological implications. Boulder, CO: Clay Miner Soc. p 157190.Google Scholar
Lubetkin, S.D., Middleton, S.R. and Ottewill, R.H.. 1984. Some properties of clay-water dispersions. Philos Trans R Soc London A 311: 353368.Google Scholar
Mulla, D.J., Cushman, J.H. and Low, P.F.. 1984. Molecular dynamics and statistical mechanics of water near an uncharged silicate surface. Water Resour Res 20: 619628.CrossRefGoogle Scholar
Mulla, D.J. and Low, P.F.. 1983. The molar adsorptivity of interparticle water in clay-water system. J Colloid Interface Sci 95: 5160.CrossRefGoogle Scholar
Mulla, D.J., Low, P.F., Cushman, J.H. and Diestler, D.J.. 1984. A molecular dynamics study of water near silicate surfaces. J Colloid Interface Sci 100: 576580.CrossRefGoogle Scholar
Mulla, D.J., Low, P.F. and Roth, C.B.. 1985. Measurement of the specific surface area of clays by internal reflectance spectroscopy. Clays Clay Miner 33: 391396.CrossRefGoogle Scholar
Norrish, K.. 1954. The swelling of montmorillonites. Discuss Faraday Soc 18: 120134.CrossRefGoogle Scholar
Oster, J.D. and Low, P.F.. 1964. Heat capacities of clay and clay-water mixtures. Soil Sci Soc Am Proc 28: 605609.CrossRefGoogle Scholar
Pimentel, G.C. and McClellan, A.L.. 1960. The hydrogen bond. San Francisco: Freeman. 475 p.Google Scholar
Poinsignon, C., Cases, J.M. and Fripiat, J.J.. 1978. Electrical-polarization of water molecules adsorbed by smectites: an infrared study. J Phys Chem 82: 18551860.CrossRefGoogle Scholar
Russell, J.D. and Farmer, V.C.. 1964. Infra-red spectroscopic study of the dehydration of montmorillonite and saponite. Clay Min Bull 5: 443464.CrossRefGoogle Scholar
Sadlej, J. and Sadlej, A.J.. 1977. Theoretical infrared and Raman spectroscopic parameters for H2O and the H2O⃛Li+ system. Faraday Discuss Chem Soc 64: 112119.CrossRefGoogle Scholar
Sallé de Chou, J., Low, P.F. and Roth, C.B.. 1980. Absorption of infrared radiation by D2O and HDO mixed with montmorillonite. Clays Clay Miner 28: 111118.CrossRefGoogle Scholar
Sartori, G., Furlani, C. and Damiani, A.. 1958. On the problem of the vibrational frequencies of water in complexes. J Inorg Nucl Chem 8: 119124.CrossRefGoogle Scholar
Serratosa, J.M.. 1960. Dehydration studies by IR spectroscopy. Am Mineral 45: 11011104.Google Scholar
Sun, Y., Lin, H. and Low, P.F.. 1986. The nonspecific interaction of water with the surfaces of clay minerals. J Colloid Interface Sci 112: 556564.CrossRefGoogle Scholar
Van der Marel, H.W. and Beutelspacher, H.. 1976. Atlas of Infrared Spectroscopy of Clay Minerals and Their Admixtures. Amsterdam: Elsevier Science. p 3363.Google Scholar
Viani, B.E., Low, P.F. and Roth, C.B.. 1983. Direct measurement of the relation between interlayer force and interlayer distance in the swelling of montmorillonite. J Colloid Interface Sci 96: 229244.CrossRefGoogle Scholar
Viani, B.E., Roth, C.B. and Low, P.F.. 1985. Direct measurement of the relation between swelling pressure and interlayer distance in Li-vermiculite. Clays Clay Miner 33: 244250.CrossRefGoogle Scholar
Wu, J., Low, P.F. and Roth, C.B.. 1989. Effects of octahedral-iron reduction and swelling pressure on interlayer distances in Na-nontronite. Clays Clay Miner 37: 211218.Google Scholar
Yan, L.B., Low, P.F. and Roth, C.B.. 1996. Enthalpy changes accompanying the collapse of montmorillonite layers and the penetration of electrolyte into interlayer space. J Colloid Interface Sci 182: 417424.CrossRefGoogle Scholar
Yan, L.B., Roth, C.B. and Low, P.F.. 1996. Changes in the Si-O vibrations of smectite layers accompanying the sorption of interlayer water. Langmuir 12: 44214429.CrossRefGoogle Scholar
Zhang, Z.Z. and Low, P.F.. 1989. Relation between the heat of immersion and the initial water content of Li-, Na- and K-montmorillonite. J Colloid Interface Sci 133: 461472.CrossRefGoogle Scholar
Zhang, F., Low, P.F. and Roth, C.B.. 1995. Effects of monovalent, exchangeable cations and electrolytes on the relation between swelling pressure and interlayer distance in montmorillonite. J Colloid Interface Sci 173: 3441.CrossRefGoogle Scholar