INTERPARTICLE ACTION AND RHEOLOGY OF DISPERSIVE CLAYS

The determination of the various interacting parameters in the phenomenon of clay soil dispersibility needs consideration of pore fluid chemistry, mineralogy and proportions of clay minerals, and resultant particle interaction. The need to develop an appreciation of soil dispersibility in view of the preceding has resulted in the examination of clay particle interaction with respect to the effects and influence of various salts, and in particular, the potential determining anions on the dispersive performance of certain clays. Various concentrations of NaC1, NaHCO3 and 15 meq/L NaOH were used in the preparaton of soils consisting of Kaolinite, ilite, montmorillonite, and mixtures of these clay minerals, with primary attention paid to kaolinite for the development of particle-interaction models for evaluation in terms of a flocculation-deflocculation status through a study of their rheological properties, light transmission, zeta potential, and adsorption-desorption phenomena. (Authors)

  • Availability:
  • Supplemental Notes:
    • Presented at the October 16-20, 1978, ASCE Annual Convention and Exposition held at Chicago, Illinois (Preprint 3379).
  • Corporate Authors:

    American Society of Civil Engineers

    345 East 47th Street
    New York, NY  United States  10017-2398
  • Authors:
    • YONG, R N
    • Sethi, A J
    • Ludwig, H P
    • Jorgensen, M A
  • Publication Date: 1979-10

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Subject/Index Terms

Filing Info

  • Accession Number: 00302507
  • Record Type: Publication
  • Report/Paper Numbers: ASCE 14903 Proc Paper
  • Files: TRIS
  • Created Date: Oct 27 1980 12:00AM