Soil-Water Characteristics of the Low Liquid Limit Silt considering Compaction and Freeze-Thaw Action

<table class="table-group" id="tab3"><tr><td><table class="table"><tr><td class="thead-hr" colspan="2"><hr/></td></tr><tr class="thead"><td class="align_left">Degree of compaction (%)</td><td class="align_center">Saturated water content (%)</td></tr><tr><td class="thead-hr" colspan="2"><hr/></td></tr><tr><td class="align_left">100</td><td class="align_center">23.04</td></tr><tr><td class="align_left">95</td><td class="align_center">24.50</td></tr><tr><td class="align_left">90</td><td class="align_center">26.97</td></tr><tr><td class="align_left">85</td><td class="align_center">29.46</td></tr><tr><td class="align_left">80</td><td class="align_center">30.92</td></tr><tr class="table-tr"><td colspan="2"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

<div>Saturated water content under different degrees of compaction.</div>

Advances in Civil Engineering

tab3

Table 3

Table 3: Soil-Water Characteristics of the Low Liquid Limit Silt considering Compaction and Freeze-Thaw Action 