The Coupling Effect of Rainfall and Reservoir Water Level Decline on the Baijiabao Landslide in the Three Gorges Reservoir Area, China

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2017/3724867/figures/3724867.fig.008a.svgz" name="3724867.fig.008a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Only rainfall considered</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2017/3724867/figures/3724867.fig.008b.svgz" name="3724867.fig.008b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Only reservoir water level decline considered</td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2017/3724867/figures/3724867.fig.008c.svgz" name="3724867.fig.008c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>The coupling of rainfall and reservoir water level decline</td></tr></table>

<div>The distribution of pore water pressure under different boundary conditions (unit, Pa).</div>

Geofluids

fig8

Figure 8

Figure 8: The Coupling Effect of Rainfall and Reservoir Water Level Decline on the Baijiabao Landslide in the Three Gorges Reservoir Area, China 