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Rock containing clay minerals and anhydrite increase in volume (swell) due to water absorption. The swelling results in a build up of pressure in the bottom of the tunnel lining.
Under low overburden conditions (10-50 m) pressures at the bottom of the tunnel lining could cause the tunnel to heave, resulting in vertical displacements at the ground surface above the tunnel. Additionally, damages to the tunnel lining could occur because of varying degrees of heaving along the tunnel axis (primarily in the lower part of the cross section).
Significant heave in the 60 and 370 m sections of the Chienberg road tunnel near Basel (Switzerland) occurred before the tunnel was even finished. The observed heave rates and resulting heave damage on the tunnel lining were so serious abandonment of the tunnel project was discussed.
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