Investigation on the Influence of Temperature and Confining Pressure on the Hydraulic Conductivity of the Integrated and Fractured Jurassic Conglomerates

Figure 10

Seepage flow rate changes in the shear failure samples with various temperatures when the confining pressures are (a) 3 MPa, (b) 5 MPa, and (c) 7 MPa.

(a)

(b)

(c)