Research Article

Experimental Measurement of the Transport Flow Path Aperture in Thermally Cracked Granite and the Relationship between Pore Structure and Permeability

Table 2

Summary of experimental results.

Treated temperaturePcPpPorosity
°CMPaMPaμmMPam2%

40050.850-0.8850.103-0.1070.5-1.38
7.51.21-1.590.0573-0.07540.75-1.32
1011.24
151.51.13
2021.07
252.51.02
3030.990

60050.039-0.0481.87-2.300.5-1.83
7.50.056-0.0621.45-1.600.75-1.66
100.074-0.0781.15-1.211-1.50
150.113-0.1240.723-0.7941.5-1.33
200.154-0.1880.476-0.5812-1.22
250.238-0.2750.326-0.3762.5-1.17
300.351-0.3620.247-0.2553-1.11

80050.5-2.66
7.50.027-0.0283.18-3.300.75-2.44
100.0412.181-2.21
150.063-0.0651.38-1.421.5-1.91
200.081-0.0960.936-1.082-1.72
250.126-0.1400.642-0.7132.5-1.58
300.181-0.1920.468-0.4963-1.50

Pc = confining pressure; Pp = pore pressure from the permeability measurement;  = permeability;  = gas breakthrough pressure;  = flow path aperture.