CHEMICAL OSMOSIS IN COMPACTED CLAYEY MATERIAL AND THE PREDICTION OF WATER TRANSPORT

In order to investigate the ability of a compacted clay to act as a semi-permeable membrane an experimental setup was constructed. A flexible wall permeameter was connected with two reservoirs and a clay sample was subjected to chemical potential gradient by filling the reservoirs with solutions of different salt concentrations. For a commercially available bentonite the semi-permeability expressed by the reflection coefficent was investigated, and compared with the model by Marine & Fritz (1983). The values found were significantly lower than predicted. The large difference between prediction and observation may originate from diffusion-osmosis, ie the convection or drag of water due to the diffusion of salt. (A) For the covering abstract see IRRD 898792.

  • Availability:
  • Corporate Authors:

    Thomas Telford Limited

    London,   United Kingdom 
  • Authors:
    • KEIJZER, TJS
    • KLEINGELD, P J
    • LOCH, JPG
  • Publication Date: 1997

Language

  • English

Media Info

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Filing Info

  • Accession Number: 00752960
  • Record Type: Publication
  • Source Agency: Transport Research Laboratory
  • ISBN: 0-7277-2606-4
  • Files: ITRD
  • Created Date: Sep 28 1998 12:00AM