Published October 2001 | Version v1
Report Open

Can the water content of highly compacted bentonite be increased by applying a high water pressure?

  • 1. Geodevelopment AB, Lund (Sweden)
  • 2. Greifswald Univ. (Germany). Dept. of Geology

Description

A great many laboratory investigations have shown that the water uptake in highly compacted MX-80 clay takes place by diffusion at low external pressure. It means that wetting of the clay buffer in the deposition holes of a KBS-3 repository is very slow if the water pressure is low and that complete water saturation can take several tens of years if the initial degree of water saturation of the buffer clay and the ability of the rock to give off water are low. It has therefore been asked whether injection of water can raise the degree of water saturation and if a high water pressure in the nearfield can have the same effect. The present report describes attempts to moisten highly compacted blocks of MX-80 clay with a dry density of 1510 kg/m3 by injecting water under a pressure of 650 kPa through a perforated injection pipe for 3 and 20 minutes, respectively. The interpretation was made by determining the water content of a number of samples located at different distances from the pipe. An attempt to interpret the pattern of distribution of injected uranium acetate solution showed that the channels into which the solution went became closed in a few minutes and that dispersion in the homogenized clay gave low U-concentrations. The result was that the water content increased from about 9 to about 11-12 % within a distance of about 1 centimeter from the injection pipe and to slightly more than 9 % at a distance of about 4-5 cm almost independently of the injection time. Complete water saturation corresponds to a water content of about 30 % and the wetting effect was hence small from a practical point of view. By use of microstructural models it can be shown that injected water enters only the widest channels that remain after the compaction and that these channels are quickly closed by expansion of the hydrating surrounding clay. Part of the particles that are thereby released become transported by the flowing water and cause clogging of the channels, which is another reason why the inflow ceases after a few minutes. It is estimated that a higher injection pressure, i.e. 2-3 MPa, should yield more effective wetting but that an injection time exceeding a few minutes will not improve it. Injection of a very salt solution is expected to be particularly effective.

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Additional details

Publishing Information

Imprint Pagination
21 p.
ISSN
1404-0344
Report number
SKB-TR--01-33

Optional Information

Notes
5 refs, 9 figs, 5 tabs