Research Article
Unloading Creep Characteristics of Frozen Clay Subjected to Long-Term High-Pressure K0 Consolidation before Freezing
Figure 4
Variations in the axial creep strain and axial creep rate with time (σ1 = 10 MPa): (a) tc = 3 d, (b) tc = 7 d, (c) tc = 14 d, and (d) tc = 28 d.
| (a) |
| (b) |
| (c) |
| (d) |