Macroscopic and Mesoscopic Mechanical Properties of Mine Tailings with Different Dry Densities under Different Confining Pressures

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2020/8832335/figures/8832335.fig.003a.svgz" name="8832335.fig.003a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Dry density is 1.53 g/cm<sup>3</sup></td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2020/8832335/figures/8832335.fig.003b.svgz" name="8832335.fig.003b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Dry density is 1.61 g/cm<sup>3</sup></td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2020/8832335/figures/8832335.fig.003c.svgz" name="8832335.fig.003c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Dry density is 1.66 g/cm<sup>3</sup></td></tr></table>

<div>Relationship between pore water pressure and axial strain.</div>

Geofluids

fig3

Figure 3

Figure 3: Macroscopic and Mesoscopic Mechanical Properties of Mine Tailings with Different Dry Densities under Different Confining Pressures 