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Cation exchange capacity measurements on illite using the sodium and cesium isotope dilution technique: Effects of the index cation, electrolyte concentration and competition: Modeling

Published online by Cambridge University Press:  01 January 2024

Bart Baeyens*
Affiliation:
Laboratory for Waste Management, Paul Scherrer Institut, CH-5232 Villigen PSI, Switzerland
Michael H. Bradbury
Affiliation:
Laboratory for Waste Management, Paul Scherrer Institut, CH-5232 Villigen PSI, Switzerland
*
*E-mail address of corresponding author: bart.baeyens@psi.ch

Abstract

The isotope dilution technique using Na and Cs as index cations was used to determine the cation exchange capacity (CEC) of illite du Puy as a function of background electrolyte composition. The work showed, in accord with previous studies, that the CEC values were in the order Cs-CEC > Na-CEC. Sodium is commonly chosen as the index cation in CEC determinations using the isotope dilution method. The experimentally measured Na-CEC values for Na-illite increased from ∼75 to ∼200 meq kg−1 for NaClO4 concentrations in the range 5.6 × 10−4 to 1.25 × 10−2 M. Cesium CEC determinations showed a much less pronounced trend over a CsNO3 concentration range from 10−3 to 10−2 M. A reference Cs-CEC value of 225 meq kg−1 was chosen. Careful chemical analyses of the supernatant solutions revealed that Ca and Mg at the (sub)μmolar level were present in all the determinations, despite the extensive conditioning procedures used. Competition between (Ca + Mg) and Na for the exchange sites was put forward as an explanation for the variation of Na-CEC values. This hypothesis was confirmed in a series of single (45Ca) and double (45Ca plus 22Na) labeling experiments. Calcium-sodium selectivity coefficients ((NaCaKc)) were calculated from the experimental data for NaClO4 concentrations from 5.6 × 10−4 to 0.1 M and exhibited a variation from 1.6 to 14.3. A two-site cation exchange model was developed with site capacities and NaCaKc values for each site: planar site capacity =180 meq kg−1, NaCaKcPS=2; type II site capacity = 45 meq kg−1, NaCaKcII=80. The model was able to predict the Na and Ca occupancies in the Na-CEC experiments over the whole range of NaClO4 concentrations. It is recommended that Cs should be used instead of Na as the index cation for determining the CEC of illite.

Type
Research Article
Copyright
Copyright © The Clay Minerals Society 2004

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References

Baeyens, B. and Bradbury, M.H., (1997) A mechanistic description of Ni and Zn sorption on Na-montmorillonite. Part I: Titration and sorption measurements Journal of Contaminant Hydrology 27 199222.CrossRefGoogle Scholar
Bolt, G.H. Sumner, M.E. and Kamphorst, A., (1963) A study of the equilibrium between three categories of potassium in an illitic soil Soil Science Society of America Proceedings 27 294299.CrossRefGoogle Scholar
Bradbury, M.H. and Baeyens, B., (1994) Sorption by cation exchage. Incorporation of a cation exchange model into geochemical computer codes Villigen PSI and NTB 94-11, Nagra, Wettingen, Switzerland Paul Scherrer Institut.Google Scholar
Bradbury, M.H. and Baeyens, B., (1997) A mechanistic description of Ni and Zn sorption on Na-montmorillonite. Part II: Modelling Journal of Contaminant Hydrology 27 223248.CrossRefGoogle Scholar
Bradbury, M.H. and Baeyens, B., (1998) A physico-chemical characterisation and geochemical modelling approach for determining porewater chemistries in argillaceous rocks Geochimica et Cosmochimica Acta 62 783795.CrossRefGoogle Scholar
Bradbury, M.H. and Baeyens, B., (2000) A generalised sorption model for the concentration dependent uptake of Cs by argillaceous rock Journal of Contaminant Hydrology 42 141163.CrossRefGoogle Scholar
Bradbury, M.H. and Baeyens, B., (2003) Porewater chemistry in compacted re-saturated MX-80 bentonite Journal of Contaminant Hydrology 61 329338.CrossRefGoogle ScholarPubMed
Brouwer, E. Baeyens, B. Maes, A. and Cremers, A., (1983) Caesium and rubidium ion equilibria in illite clay Journal of Physical Chemistry 87 12131219.CrossRefGoogle Scholar
Bruggenwert, M.G.M. Kamphorst, A. and Bolt, G.H., (1982) Survey of experimental information on cation exchange in soil systems Soil Chemistry B. Physico-Chemical Models Amsterdam Elsevier 141203.Google Scholar
Cremers, A., (1968) Ionic movement in a colloidal environment Leuven, Belgium University of Leuven Postdoctoral thesis.Google Scholar
Cremers, A. and Thomas, H.C., (1966) Self-diffusion in suspensions. Sodium in montmorillonite at equilibrium Journal of Physical Chemistry 70 32293234.CrossRefGoogle Scholar
Cremers, A. Elsen, A. De Preter, P. and Maes, A., (1988) Quantitative analysis of radiocesium retention in soils Nature 335 247249.CrossRefGoogle Scholar
Davies, C.W., (1962) Ion Association London Butterworths.Google Scholar
De Preter, P., (1990) Radiocesium retention in the aquatic, terrestrial and urban environment: a quantitative and unifying analysis Leuven, Belgium University of Leuven PhD thesis.Google Scholar
Eberl, D.D., (1980) Alkali cation selectivity and fixation by clay minerals Clays and Clay Minerals 28 161172.CrossRefGoogle Scholar
Gaines, G.I. and Thomas, H.C., (1953) Adsorption studies on clay minerals. II. A formulation of the thermodynamics of exchange adsorption Journal of Physical Chemistry 21 714718.CrossRefGoogle Scholar
Gorgeon, L., (1994) Contribution à la modélisation physicochimique de la retention de radioeléments à vie longue par des materiaux argileux France Université Paris 6 PhD thesis.Google Scholar
Goulding, K.W.T. and Talibudeen, O., (1980) Heterogeneity of cation-exchange sites for K-Ca exchange in aluminosilicates Journal of Colloid and Interface Science 78 1524.CrossRefGoogle Scholar
Horseman, S.T. Higgo, J.J. Alexander, J. and Harrington, J.F., (1996) Water, gas and solute movement through argillaceous media Paris, France Nuclear Energy Agency, OECD.Google Scholar
Jackson, M.L., (1968) Weathering of primary and secondary minerals in soils Transactions of the International Society of Soil Science 4 281292.Google Scholar
Jenne, E.A., Chappel, W. and Peterson, K., (1977) Trace element sorption by sediments and soils: Sites and processes Molybdenum in the Environment, Vol. 2 New York Dekker 425553.Google Scholar
Kim, Y. and Kirkpatrick, R.J., (1997) 23Na and 133Cs NMR study of cation adsorption on mineral surfaces: Local environments, dynamics, and effects of mixed cations Geochimica et Cosmochimica Acta 61 51995208.CrossRefGoogle Scholar
Kim, Y. Kirkpatrick, R.J. and Cygan, R.T., (1996) 133Cs NMR study of cesium on the surfaces of kaolinite and illite Geochimica et Cosmochimica Acta 60 40594074.CrossRefGoogle Scholar
Maes, A. and Cremers, A., (1975) Cation-exchange hysteresis in montmorillonite: A pH-dependent effect Soil Science 119 198202.CrossRefGoogle Scholar
Maes, A. and Cremers, A., (1977) Charge density effects in ion exchange. Part 1. Heterovalent exchange equilibria Journal of the Chemical Society, Faraday Transactions I 73 18071814.CrossRefGoogle Scholar
Maes, A. Cremers, A., Sibley, T.H. and Myttenaere, C., (1986) Europium sorption on a clay sediment: sulphate and ionic strength effects Application of Distribution Coefficients to Radiological Assessment Models Amsterdam Elsevier 103110.Google Scholar
Maes, A., Peigneur, P. and Cremers, A. (1976) Thermodynamics of transition metal ion exchange in montmorillonite. Proceedings of the International Clay Conference, Mexico City, pp. 319329.Google Scholar
Nagra, Project Opalinus Clay. Safety Report. Demonstration of disposal feasibility for spent fuel, vitrified high-level waste and long-lived intermediate-level waste (Entsorgungsnachweis) (2002) Wettingen, Switzerland Nagra.Google Scholar
Poinssot, C. Baeyens, B. and Bradbury, M.H., (1999) Experimental studies of Cs, Sr, Ni, and Eu sorption on Naillite and the modelling of Cs sorption Villigen PSI and NTB 99-04, Nagra, Wettingen, Switzerland Paul Scherrer Institut.Google Scholar
Poinssot, C. Baeyens, B. and Bradbury, M.H., (1999) Experimental and modelling studies of caesium sorption on illite Geochimica et Cosmochimica Acta 63 32173227.CrossRefGoogle Scholar
Sawhney, B.L., (1970) Potassium and cesium ion selectivity in relation to clay mineral structure Clays and Clay Minerals 18 4752.CrossRefGoogle Scholar
Sawhney, B.L., (1972) Selective adsorption and fixation of cations by clay minerals: A review Clays and Clay Minerals 20 93100.CrossRefGoogle Scholar
Sposito, G. Holtzclaw, K.M. Charlet, L. Jouany, C. and Page, A.L., (1983) Sodium-calcium and sodium-magnesium exchange on Wyoming Bentonite in perchlorate and chloride background ionic media Journal of the Soil Science Society of America 47 5156.CrossRefGoogle Scholar
Tamura, T. and Jacobs, D.G., (1960) Structural implications in cesium sorption Health Physics 2 391398.CrossRefGoogle ScholarPubMed
Van Bladel, R. and Menzel, R., (1969) () A thermodynamic study of sodium-strontium exchange on Wyoming bentonite. Proceedings of the International Clay Conference, Tokyo, pp. 619634.Google Scholar