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Flocculation Value and Gel Structure of Sodium/Calcium Montmorillonite and Illite Suspensions
Author(s) -
Oster J. D.,
Shainberg I.,
Wood J. D.
Publication year - 1980
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/sssaj1980.03615995004400050016x
Subject(s) - montmorillonite , flocculation , illite , chemistry , sodium , kaolinite , nuclear chemistry , clay minerals , inorganic chemistry , mineralogy , organic chemistry
The flocculation value, the minimum salt concentration which causes flocculation within 24 hours, was determined for mixtures of Na‐ and Ca‐montmorillonite (API‐25) and Fithian illite (API‐35). The equivalent fraction of exchangeable Na + , E Na , varied from 0 to 1. We prepared Na/Ca clay suspensions by adding the appropriate amounts of homoionic dry clays to a series of Na/Ca chloride solutions (0.2 to 80 mol c m −8 ; 0.2 to 80 meq liter −1 ) with appropriate sodium adsorption ratio and shaking the mixture for 1 hour. The flocculation value of Ca‐montmorillonite (0.25 mol o m −3 ) increased rapidly with small amounts of exchangeable Na + : the flocculation value for an E Na of 0, 0.2, 0.4, and 1 was 0.25, 6, 9, and 12 mol c m −3 , respectively. The flocculation values for Ca‐ and Na‐illite were 0.25 and 55 mol o m −3 , respectively, and increased linearly with E Na . Van der Waals attraction forces are mainly responsible for flocculation of Ca‐montmorillonite and illite systems. Edge‐to‐face attraction is dominant in flocculating Na‐montmorillonite. The large effect of small amounts of exchangeable Na + in montmorillonite suspensions results from demixing of exchangeable ions whereby Na + is the predominant cation on the external surfaces when E Na < 0.20.