An improved method of dual-energy gamma-ray attenuation was used to measure water content and bulk density rapidly and accurately, during one-dimensional, unsaturated water movement into a column of an equal-part mixture of initially air-dry, highly swelling bentonite and silt. The bulk density near the inlet end of the column decreased rapidly as water entered. Since the ends of the column were confined, the expansion of the wetted bentonite-silt produced a compensating compression in the remaining air-dry portion of the column. Several water-content variables were plotted against the so-called reduced material coordinate M/t to the 1/2 power (Boltmann variable expressed in terms of the material coordinate m and time t). Neither the volumetric water content nor the volumetric water ratio would coalesce the data when plotted against m/t to the 1/2 power. In contrast, a plot of water saturation vs. m/t to 1/2 power did coalesce the data into a single curve, except for very early times at positions nearer than 1 cm to the water inlet.

  • Corporate Authors:

    Soil Science Society of America

    677 South Segoe Road
    Madison, WI  United States  53711
  • Authors:
    • Nofziger, D L
    • Swartzendruber, D
  • Publication Date: 1976-5

Media Info

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Filing Info

  • Accession Number: 00139299
  • Record Type: Publication
  • Files: TRIS
  • Created Date: Oct 6 1976 12:00AM