UNSATURATED TRANSIENT AND STEADY-STATE FLOW OF MOISTURE IN SUBGRADE SOIL

A general procedure for determining the soil-water properties necessary for predicting moisture movement in subgrade soils is described. A gamma-ray transmission method was used for the nondestructive measurement of the water content and a tensiometer-pressure transducer arrangement to measure the soil-water pressure (suction); the unsaturated hydraulic conductivity, diffusivity, and soil-water characteristic functions were evaluated for AASHO A-4 subgrade soil. The soil was compacted in a column at uniform density and moisture content and tested under isothermal conditions. A water table was established at the bottom of the soil column and the transport of water through the subgrade soil studied. The mathematical procedures for determining the soil-water properties from the laboratory data are described, and the use of the experimentally determined hydraulic conductivity, soil-water diffusivity, and soil-water characteristic functions in the prediction of moisture changes in an AASHO A-4 soil is demonstrated. /Author/

Media Info

  • Media Type: Print
  • Features: Figures; References;
  • Pagination: pp 56-61
  • Monograph Title: Subsidence over mines and caverns, moisture and frost actions, and classification
  • Serial:

Subject/Index Terms

Filing Info

  • Accession Number: 00158158
  • Record Type: Publication
  • ISBN: 0309025885
  • Files: TRIS, TRB
  • Created Date: Sep 28 1977 12:00AM