Abstract:9 pH-neutralisation curves of some natural clay samples containing inters/ratified illite-montmorillonite minerals have been studied. It has been observed that their titration curves are d(fferent from those of kaolinite, montmorillonite, illite and their natural mixtures. Unlike these, the titration curves of samples containing interstratified minerals show four inflections at pH ranges 5-6, 7-7.5, 8-9.5 and 10-10.5. The role of associated clay and non-clayey materials on the nature of their titration curves … Show more
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