Experimental Study of Joint Roughness Influence on Fractured Rock Mass Seepage

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2021/8813743/figures/8813743.fig.005a.svgz" name="8813743.fig.005a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Pressure chamber</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2021/8813743/figures/8813743.fig.005b.svgz" name="8813743.fig.005b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Pressurization system</td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2021/8813743/figures/8813743.fig.005c.svgz" name="8813743.fig.005c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Computer control system</td></tr></table>

<div>TAW-2000M rock triaxial servo instrument.</div>

Geofluids

fig5

Figure 5

Figure 5: Experimental Study of Joint Roughness Influence on Fractured Rock Mass Seepage 