EROSION RATE OF COMPACTED N-MONTMORILLONITE SOILS

Erosion rates of unsaturated compacted Na-montmorillonite clays are measured under a range of tractive stresses from surface flows in a rectangular flume. The degree of saturation of compacted samples ranges from 0.52-0.97. The Na-montmorillonite (Volclay bentonite)is mixed with ground silica to obtain samples with various percentages of clay. Samples of 100, 70, 40 and 10% clay content by dry weight are tested. Samples are compacted under 700 Pa into sample containers with 160-cm2 surface area and are subjected to flowing water in the flume. The results of the study show that the erosion rate of Na-montmorillonite soil samples increases when clay content decreases and is independent of compaction water content. The relationship between erosion rate and tractive stress is linear for all Na-montmorillonite samples. For the range of water content tested, an empirical relationship is developed to estimate the erosion rate of compacted Na-montmorillonite clays as a function of percent clay content and tractive stress.

Media Info

  • Features: Appendices; Figures; References; Tables;
  • Pagination: p. 296-305
  • Serial:

Subject/Index Terms

Filing Info

  • Accession Number: 00465506
  • Record Type: Publication
  • Report/Paper Numbers: ASCE Paper 22247
  • Files: TRIS
  • Created Date: Feb 29 1988 12:00AM