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Infrared Study of Water Sorption on Na-, Li-, Ca-, and Mg-Exchanged (SWy-1 and SAz-1) Montmorillonite

Published online by Cambridge University Press:  28 February 2024

Weizong Xu ,
Cliff T. Johnston ,
Paul Parker  and
Stephen F. Agnew
Weizong Xu
Affiliation:
Crop, Soil and Environmental Sciences, Agronomy Department, Purdue University, West Lafayette, Indiana 47907-1150, USA
Cliff T. Johnston
Affiliation:
Crop, Soil and Environmental Sciences, Agronomy Department, Purdue University, West Lafayette, Indiana 47907-1150, USA
Paul Parker
Affiliation:
Crop, Soil and Environmental Sciences, Agronomy Department, Purdue University, West Lafayette, Indiana 47907-1150, USA
Stephen F. Agnew
Affiliation:
CST4, MS J586, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA
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Abstract

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An environmental infrared microbalance (EIRM) cell was used to study H2O sorption on two montmorillonite samples as a function of water content and type of exchangeable cation. The vibrational spectra showed that H2O sorbed to the clay at low-water content was strongly influenced by the exchangeable cation and by the close proximity to the clay surface. At water contents <6 H20 molecules per exchangeable cation, the H-O-H bending mode of H2O (v2 mode) shifts to a lower frequency and is characterized by an increase in molar absorptivity. In contrast, the positions of the asymmetric and symmetric OH-stretching modes of sorbed water (v1 and v3 modes) shift to higher energies. These observations indicate that H2O molecules sorbed to the clay surface at low-water content are less hydrogen bonded than in bulk H2O. In addition, the vibrational-stretching and bending bands of the structural OH groups of the 2:1 layer are also strongly influenced by H2O content and type of exchangeable cation. By using the EIRM cell, the molar absorptivities of the structural OH-bending vibrations were measured as a function of H2O content. The position and molar absorptivity of the structural OH-bending bands at 920, 883, and 840 cm-1 are strongly influenced by H2O content and type of exchangeable cation. The molar absorptivity of the 920-cm-1 band, which is assigned to the AlAlOH group, decreased strongly at low-H2O content. This reduction in intensity is assigned to a dehydration-induced change in orientation of the structural OH groups resulting from the penetration of H2O molecules into siloxane ditrigonal cavities that are not associated with a net negative charge from isomorphous substitutions.

Keywords

Exchangeable CationFTIRHydrationHysteresisSmectiteSorptionWater
Type
Research Article
Information
Clays and Clay Minerals , Volume 48 , Issue 1 , February 2000 , pp. 120 - 131
Copyright
Copyright © 2000, The Clay Minerals Society

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