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Published in Soil Sci Soc Am J 33:37-41 (1969)
© 1969 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Standard Free Energies of Exchange for Alkali Metal Cations on Wyoming Bentonite1

R. G. Gast2

ABSTRACT

Standard free energies of exchange, {Delta} Go, were determined for the exchange of Na with Li, K, Rb, and Cs and Li with K between 0.001N chloride solutions and 5% Wyoming bentonite gels at 25C. Values were also determined for Na -> Rb, Na -> Cs, and Rb -> Cs exchanges between 0.0075N chloride solutions and 0.75% Wyoming bentonite suspensions. Application of the additivity rule indicates that the values are accurate to within ±50 to 100 cal mole-1. Values for the 5% gels range from +48 cal mole-1 for Na -> Li exchange to –1,081 cal mole-1 for Na -> Cs exchange. There is a small but consistent increase in the {Delta}Go values for the 0.75% suspensions compared to those for the 5% gels. With the possible exception of Li, a linear relationship was found between {Delta}Go values and Debye-Huckle parameters for the respective cations indicating that the adsorption of monovalent cations from strong electrolyte solutions is governed by their hydrated radii.


NOTES

1 This manuscript is published with the permission of the Director of the University of Tennessee Agr. Exp. Sta., Knoxville.

2 Agricultural Research Laboratory of the University of Tennessee, Oak Ridge; operated by the Tennessee Agr. Exp. Sta. for the US Atomic Energy Commission under Contract no. AT-40-1-GEN-242.

Received for publication March 8, 1968. Accepted for publication August 12, 1968.




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B. J. Teppen and D. M. Miller
Hydration Energy Determines Isovalent Cation Exchange Selectivity by Clay Minerals
Soil Sci. Soc. Am. J., December 2, 2005; 70(1): 31 - 40.
[Abstract] [Full Text] [PDF]




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