Experimental Study on the Effect of Initial Water Content and Temperature Gradient on Soil Column Segregation Frost Heave

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2022/4679547/figures/4679547.fig.0016a.svgz" name="4679547.fig.0016a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Morphology of segregated ice in segregation cracks in the T4 soil column</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2022/4679547/figures/4679547.fig.0016b.svgz" name="4679547.fig.0016b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>The segregated ice layer in the segregation cracks of the T4 soil column</td></tr></table>

<div>The T4 soil column segregated ice phenomenon.</div>

Geofluids

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Figure 16

Figure 16: Experimental Study on the Effect of Initial Water Content and Temperature Gradient on Soil Column Segregation Frost Heave 