Abstract
The results of experimental measurements have been used to obtain relations between the density and the content of bound water and the adsorption characteristics have been calculated for clay minerals substituted with Ca and Na cations. Some of the factors controlling the hydration of exchange cations at adsorbent surfaces have been established.
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References
R. E. Grim, Clay Mineralogy [Russian translation], IL, 1959.
A. V. Kiselev, ZhFKh, 38, no. 12, 1964.
F. D. Ovcharenko, Hydrophily of Clays and Clay Minerals [in Russian], Izd. AN Ukr. SSR, Kiev, 1961.
F. D. Ovcharenko and Yu. P. Tarasevich, UKhZh,30, no. 10, 1964.
P. P. Olodovskii, Building Thermophysics [in Russian], izd. Energiya, Moscow, 1966.
I. E. Neimark, M. A. Piontkovskaya, A. I. Rastrenenko, G. S. Shemeko, V. G. Il'in, A. M. Eremeneko, and S. N. Antonovskaya, collection: Zeolites: Their Synthesis, Properties and Applications [in Russian], izd. Nauka, Moscow-Leningrad, 1965.
Ts. M. Raitburd and M. V. Slonimskaya, DAN SSSR, 163, no. 1, 1965.
S. B. Hendricks, R. A. Nelson, and L. T. Alexander, J. Amer. Chem. Soc., 62, 1457, 1940.
A. C. Siefert, Ph. D dissertation: Studies on the Hydration of Clays, Pennsylvania State College, 1912.
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Olodovskii, P.P. Adsorbed water density distribution in disperse media. Journal of Engineering Physics 12, 263–266 (1967). https://doi.org/10.1007/BF00836531
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DOI: https://doi.org/10.1007/BF00836531