Clays and Clay Minerals

, Volume 40, Issue 5, pp 586–592 | Cite as

Sedimentation Behavior of a Fine Kaolinite in the Presence of Fresh Fe Electrolyte

  • Kunsong Ma
  • Alain C. Pierre


The sedimentation behavior of a fine kaolinite, comprising a substantial proportion of colloidal particles as well as non-colloidal ones, has been studied when fresh FeCl3 or F2(SO4)3 electrolytes are added. The sedimentation behavior depends on the pH and the nature of electrolytes and can be explained qualitatively, in our study, by the theory of Derjaguin, Landau, Verwey, and Overbeek (DLVO theory). Fe helps also to aggregate the kaolinite particles in flocs. Two extreme kinds of qualitative sedimentation have been observed: flocculation-sedimentation and accumulation-sedimentation. However, the transition between the two kinds of sedimentation is quite progressive. The present results are discussed in reference to the DLVO theory and the hydrolysis behavior of Fe electrolytes.

Key Words

Colloid Flocculation Iron Kaolinite Sedimentation 


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Copyright information

© The Clay Minerals Society 1992

Authors and Affiliations

  • Kunsong Ma
    • 1
  • Alain C. Pierre
    • 1
  1. 1.Department of Mining, Metallurgical and Petroleum EngineeringUniversity of AlbertaEdmontonCanada

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