Study on the REV Size of Fractured Rock in the Non-Darcy Flow Based on the Dual-Porosity Model

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2018/7535927/figures/7535927.fig.0011a.svgz" name="7535927.fig.0011a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Porous media</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2018/7535927/figures/7535927.fig.0011b.svgz" name="7535927.fig.0011b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Fractured media</td></tr></table>

<div>Pore pressure fields obtained by ABAQUS-PPCE.</div>

Geofluids

fig11

Figure 11

Figure 11: Study on the REV Size of Fractured Rock in the Non-Darcy Flow Based on the Dual-Porosity Model 