DIFFERENTIAL EVAPO-TRANSPIRATION FROM A CLAY SURFACE AND ITS INFLUENCE ON EQUILIBRIUM POREWATER PRESSURE

The derivation is presented of expressions resulting from a steady state groundwater flow approach to determining the porewater pressure changes caused by modification of the rate of evapo-transpiration over limited areas of the ground surface. Solutions to the expressions have been computed for positions throughout the soil layer for a variety of shapes and sizes of affected area. The tabulated results may be used to estimate the effects for a wide range of conditions by making use of the principle of superposition. Case histories are presented in which observations of porewater pressure changes and of ground movement are compared with values derived from the tabulated results. (Author/TRRL)

Media Info

  • Features: Figures; References; Tables;
  • Pagination: p. 181-191
  • Serial:
    • GEOTECHNIQUE
    • Volume: 35
    • Issue Number: 2
    • Publisher: Thomas Telford Limited
    • ISSN: 0016-8505

Subject/Index Terms

Filing Info

  • Accession Number: 00451050
  • Record Type: Publication
  • Source Agency: Transport Research Laboratory
  • Files: ITRD, TRIS
  • Created Date: Aug 27 2004 9:57PM