Dynamic Characteristics and Mechanism of the Saturated Compacted Loess under Freeze-Thaw Cycles

<table class="table-group" id="tab1"><tr><td><table class="table"><tr><td class="thead-hr" colspan="2"><hr/></td></tr><tr class="thead"><td class="align_left">Parameters</td><td class="align_center">Value</td></tr><tr><td class="thead-hr" colspan="2"><hr/></td></tr><tr><td class="align_left">Density</td><td class="align_center">1.36 g/cm<sup>3</sup></td></tr><tr><td class="align_left">Moisture</td><td class="align_center">5.59%</td></tr><tr><td class="align_left">Specific gravity</td><td class="align_center">2.70</td></tr><tr><td class="align_left">Plastic limit</td><td class="align_center">15.9%</td></tr><tr><td class="align_left">Liquid limit</td><td class="align_center">24.1%</td></tr><tr><td class="align_left">Plastic index</td><td class="align_center">8.2</td></tr><tr class="table-tr"><td colspan="2"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

Geofluids

tab1

Table 1

Table 1: Dynamic Characteristics and Mechanism of the Saturated Compacted Loess under Freeze-Thaw Cycles 