Gas Migration in EBS and Geosphere (GMT) - Saturation of the EBS

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.

 

The GTS underground facilities are also available to interested 3rd parties for underground testing and research. The GTS offers cost-effective access to a fully developed, well characterised underground research facility with round the year logistical support - please contact Dr. Ingo Blechschmidt, Head of the Grimsel Test Site, for further details.