The Parabolic Variational Inequalities for Variably Saturated Water Flow in Heterogeneous Fracture Networks

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2018/9062569/figures/9062569.fig.006a.svgz" name="9062569.fig.006a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Homogenous dam</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2018/9062569/figures/9062569.fig.006b.svgz" name="9062569.fig.006b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Nonhomogenous dam</td></tr></table>

<div>Verification on saturated steady seepage problems.</div>

Geofluids

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Figure 6

Figure 6: The Parabolic Variational Inequalities for Variably Saturated Water Flow in Heterogeneous Fracture Networks 