Specimens of Georgia kaolinite were compacted on 4-in. molds at three compaction efforts having 7,425, 42,750, and 78,750 ft-lb/cu ft of energy, respectively. Samples representing each effort were compacted at water contents which were 5 and 1 percent dry and 1 and 5 percent wet of optimum water content. After compaction, these samples were studied in the scanning electron microscope, which revealed that the compaction had produced some degree of dispersed or face-to-face orientation of the clay platelets. The dispersed orientation was not particularly enhanced at the higher compaction efforts. Also, there was no evidence of any enhancement of this orientation on the wet side of optimum for those samples compacted at 42,750 and 78,750 ft-lb/cu ft. The sample compacted at 7,425 ft-lb/cu ft did exhibit excellent dispersed orientation at 5 percent wet of optimum. The development of dispersed fabric is believed to be due more to the actual water content than to whether the samples are wet or dry of optimum moisture content, and the dispersed fabric is probably related to the plastic limit.

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  • Corporate Authors:

    U.S. Army Waterways Experiment Station

    3909 Halls Ferry Road
    Vicksburg, MS  United States  39180-6199
  • Publication Date: 1975-5

Media Info

  • Features: Appendices; Figures; References;
  • Pagination: 37 p.

Subject/Index Terms

Filing Info

  • Accession Number: 00097002
  • Record Type: Publication
  • ISBN: Task 03
  • Report/Paper Numbers: S-75-11 Final Rpt.
  • Files: TRIS
  • Created Date: Jul 15 1975 12:00AM