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.004a.svgz" name="8813743.fig.004a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Spline spacer</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2021/8813743/figures/8813743.fig.004b.svgz" name="8813743.fig.004b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Geomagic partition isometric splines</td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2021/8813743/figures/8813743.fig.004c.svgz" name="8813743.fig.004c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Calculation of protrusion height and fluctuation angle</td></tr></table>

<div>Spline interval and calculation of Geomagic.</div>

Geofluids

fig4

Figure 4

Figure 4: Experimental Study of Joint Roughness Influence on Fractured Rock Mass Seepage 