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

<div>(a) Experimental design of the gas breakthrough method using the intravessel deformation fluid flow apparatus. Simplified illustrations of the (b) permeability measurement phase and (c) gas breakthrough experiment.</div>

Geofluids

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Figure 2: Experimental Measurement of the Transport Flow Path Aperture in Thermally Cracked Granite and the Relationship between Pore Structure and Permeability 

Figure 2 | Experimental Measurement of the Transport Flow Path Aperture in Thermally Cracked Granite and the Relationship between Pore Structure and Permeability 