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

Figure 9

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

(a)

(b)

(c)