A New Bayesian Network Model for the Risk Assessment of Water Inrush in Karst Tunnels

<table class="table-group" id="tab8"><tr><td><table class="table"><tr><td class="thead-hr" colspan="2"><hr/></td></tr><tr class="thead"><td class="align_left">Risk classification</td><td class="align_center">Definition</td></tr><tr><td class="thead-hr" colspan="2"><hr/></td></tr><tr><td class="align_left">I</td><td class="align_center">Strongly conducive to the development of large karst structures</td></tr><tr><td class="align_left">II</td><td class="align_center">Generally conducive to the development of large karst structures</td></tr><tr><td class="align_left">III</td><td class="align_center">Poorly conducive to the development of large karst structures</td></tr><tr><td class="align_left">IV</td><td class="align_center">Almost not conducive to the development of large karst structures</td></tr><tr class="table-tr"><td colspan="2"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

<div>Risk classification of contact zones of dissolvable and insoluble rock.</div>

Geofluids

tab8

Table 8

Table 8: A New Bayesian Network Model for the Risk Assessment of Water Inrush in Karst Tunnels 