The Promotion Mechanism of Frozen Stagnant Water on the Sliding in the Loess Landslide Zone of Heifangtai

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2021/9749011/figures/9749011.fig.004a.svgz" name="9749011.fig.004a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Monitoring hole of the groundwater overflow zone</td></tr><tr class="fig-image" id="b"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2021/9749011/figures/9749011.fig.004b.svgz" name="9749011.fig.004b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Monitoring hole in unsaturated area</td></tr></table>

<div>Onsite installation of monitoring instruments.</div>

Geofluids

fig4

Figure 4

Figure 4: The Promotion Mechanism of Frozen Stagnant Water on the Sliding in the Loess Landslide Zone of Heifangtai 