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GMT - Field Testing - Saturation of the EBS |
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Gas Migration in EBS and Geosphere (GMT)
Field Testing - Saturation of the EBS |
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Artificial saturation of the sand/bentonite layers had to be carried
out due to the low natural inflow rate.

- Initial saturation stages used low pressure injections into
layer 1 and the upper cavern backfill
- Once the upper cavern was filled, the pressure was raised to
about 580 kPa (this is similar to the ambient pressure prior to
excavation)
- Once the target pressure was reached, the pressure was maintained
by balancing injection with inflows to GMT drift and the VE shear
zone
- The saturation stage ended on 15th October '02 when the water
tests began
- High water saturation was achieved quickly in layers 8, 9 and
10. These high permeability layers may be due to the presence
of the gas visualisation tracer

- Much slower saturation of layers 2 to 6 and layer 11 was observed.
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Gas Migration in EBS and Geosphere (GMT) Experiment
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2005 Grimsel Test Site - Switzerland
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