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Euradwaste '08 - EU Bookshop - Europa

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Distance from heater surface (mm)<br />

100<br />

90<br />

80<br />

70<br />

60<br />

50<br />

40<br />

30<br />

20<br />

10<br />

0<br />

0.00E+00 1.00E-03 2.00E-03 3.00E-03 4.00E-03 5.00E-03 6.00E-03 7.00E-03 8.00E-03<br />

Concentration (mol/kg)<br />

197<br />

Initial<br />

1 Day<br />

3 Day<br />

7 Day<br />

15 day<br />

30 Day<br />

Figure 2: Chloride distribution of T-test (initial degree of saturation 65 %)<br />

Tests were also done to investigate the effect of temperature on HM-properties. In one set of tests<br />

FEBEX bentonite was compacted at dry densities 1.50 and 1.60 g/cm3 and saturated with deionised<br />

water under vertical stresses from 0.1 to 3.0 MPa at temperatures from 30 to 80°C while the vertical<br />

strains were measured. In another FEBEX bentonite compacted at dry density 1.50, 1.60 and 1.70<br />

g/cm3 was saturated with deionised water under constant volume conditions and temperatures from<br />

20 to 80°C while the swelling stresses developed were measured. Afterwards permeability was determined<br />

in the same specimens by imposing hydraulic gradients to the saturated samples. The<br />

swelling under load tests have shown that the effect of temperature on the swelling capacity is<br />

smaller than the effect of the vertical load applied during hydration or the effect of initial dry density.<br />

The Febex Mock-up is an experiment at almost full scale and under controlled boundary conditions.<br />

The aim is to know and understand the long-term behaviour of a clay barrier submitted to thermal<br />

and hydraulic gradients, and to validate and verify the near field THM models under controlled<br />

boundary conditions. The mock-up test surpasses the space-scale limitation of the laboratory tests,<br />

by adoption of the actual dimensions of the repository, but it does not prevent the time-scale limitation.<br />

The duration of the test, related to the operative life of the repository, makes it possible to extrapolate<br />

the future behaviour of the clay barrier from the experimental transient state [3] (ENRESA<br />

1997). The final evaluation will be made after the dismantling. However, the test is stilla a valuable<br />

instrument to understand and evaluate the behaviour in the near field, and the generated data-base<br />

has value in itself. In particular, it has verified most of the hypothesis on the THM processes in the<br />

transient phase of the clay barrier, especially in the presence of water vapour.<br />

The Febex “in situ” test consisted of a full-scale simulation of a HLW disposal facility, in accordance<br />

with the ENRESA AGP Granito (Deep Geological Disposal, Granite) reference concept. The<br />

test comprises two electrical heaters, of dimensions and weight equivalent to those of the canisters<br />

in the concept, in a 2.28 m diameter drift specifically selected and excavated in granite. The entire<br />

space surrounding the heaters is filled with blocks of compacted bentonite to complete the 17.4 m<br />

of barrier for the test section. This test zone was closed with a concrete plug. The test was installed

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