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)