Research Article

Unloading Creep Characteristics of Frozen Clay Subjected to Long-Term High-Pressure K0 Consolidation before Freezing

Table 3

The steady creep rate of the frozen clay specimens (−15°C).

SpecimenPrimary deviator stressSecondary deviator stressTertiary deviator stress
σ1 − σ3 (MPa) (%·h−1)σ1 − σ3 (MPa) (%·h−1)σ1 − σ3 (MPa) (%·h−1)

8 MPa-3 d3.50.1594.00.3134.50.681
8 MPa-7 d3.50.1114.00.1845.00.718
8 MPa-14 d4.00.1814.50.3255.00.582
10 MPa-3 d3.50.1434.00.2664.50.591
10 MPa-7 d4.30.2154.70.3645.10.618
10 MPa-14 d4.50.2215.00.4015.50.729
10 MPa-28 d4.20.1204.70.2075.20.355