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 GMT - Field Testing - Saturation of the EBS
 
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 Saturation of the EBS
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Home > GMT Project > Field Testing
Gas Migration in EBS and Geosphere (GMT)
Field Testing - 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.

 

 
Gas Migration in EBS and Geosphere (GMT) Experiment  
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