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Surface Mobilities of Cations in Clays
Author(s) -
Cremers A. E.,
Laudelout H.
Publication year - 1966
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1966.03615995003000050014x
Subject(s) - montmorillonite , ionic bonding , kaolinite , chemistry , activation energy , diffusion , ionic conductivity , ion , conductivity , clay minerals , alkali metal , electrical resistivity and conductivity , surface conductivity , tortuosity , inorganic chemistry , analytical chemistry (journal) , mineralogy , thermodynamics , porosity , electrolyte , organic chemistry , electrode , physics , electrical engineering , engineering
The effect of clay content and temperature on the electrica conductivity of two Na‐kao inite clays is investigated. The effect of the type of cation is examined in the Camp‐Berteau montmorillonite. The ionic surface mobilities (i.e. corrected for tortuosity effects) are calculated from the conductivity results. In Na‐kaolinite clays, surface mobility steadily increases with increasing cay content and attains about 40% of its solution value when clay content becomes about 70% by weight. In montmorillonite clays, surface mobility increases until clay content reaches about 35% by weight. Higher clay contents result in nearly constant values for the surface mobilities. In the series of alkali metal cations, surface mobilities increase from Cs + (attains about 7% of its solution value at 55% clay) to Na + (attains about 60% of its solution value at 55% clay); activation energies increase from Na + (4.6 kcal/eq. at 55% clay) to Cs + (5.6 kcal/eq at 55% clay). The ionic mobilities and activation energies can be correlated with the polarizabilities of the ions. It is suggested that the mobility of an ion along a clay surface is influenced more by crystallographic than by hydrated ionic volume. The large negative entropies of activation, calculated on the basis of the transition theory of rate processes, are interpreted in terms of hydration effects when an ion moves from one site to another. The agreement between self‐diffusion coefficients calculated from the electrical conductivity data and the values which may be found in the literature is very good. The applicability of the electrical conductivity method for investigating purely geometrical effects is discussed.