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

Table 1

Hydraulic conductivity of conglomerate samples.

State	Pressure difference ( (MPa))	Confining pressure ( (MPa))	Temperature ( (°C))	Hydraulic conductivity ( (×10^-9cm/s))	Permeability ( (×10^-5μm^2))
Integrated	1	3	10	9.88	1.32
			20	11.13	1.14
			28	13.38	1.15
			35	15.91	1.18
			50	1.71	0.10
		5	10	1.61	0.21
			20	3.08	0.32
			28	2.42	0.21
			35	8.03	0.60
			50	1.43	0.08
		7	10	0.62	0.08
			20	0.91	0.09
			28	1.70	0.15
			35	2.49	0.18
			50	0.78	0.04
Fractured	1	3	10	300.61	40.13
			20	251.12	25.80
			28	264.74	22.67
			35	268.55	19.92
			50	352.47	20.00
		5	10	191.89	25.61
			20	217.58	22.35
			28	197.64	16.92
			35	213.07	15.80
			50	230.02	13.05
		7	10	110.66	14.77
			20	106.91	10.98
			28	117.93	10.10
			35	126.47	9.38
			50	246.84	14.00