Research Article
Unloading Creep Characteristics of Frozen Clay Subjected to Long-Term High-Pressure K0 Consolidation before Freezing
Figure 3
Variations in axial creep strain and axial creep rate with time (σ1 = 8 MPa): (a) tc = 3 d, (b) tc = 7 d, and (c) tc = 14 d.
(a) |
(b) |
(c) |