The Equilibrium Time and Salt Expansion Characteristic of Sulfate Saline Soil upon Cooling

<table class="table-group" id="tab2"><tr><td><table class="table"><tr><td class="thead-hr" colspan="7"><hr/></td></tr><tr class="thead"><td class="align_left">The mass of water in the initial solution (g)</td><td class="align_center">The mass of salt in the initial solution (g)</td><td class="align_center">Quality of dry salt in the filter material (g)</td><td class="align_center">The quality of water in the filter material (g)</td><td class="align_center">The mass of sodium sulfate in the crystal (g)</td><td class="align_center">The quality of theoretical crystalline sodium sulfate (g)</td><td class="align_center">Actual crystallization completion rate</td></tr><tr><td class="thead-hr" colspan="7"><hr/></td></tr><tr><td class="align_left">228.26</td><td class="align_center">51.86</td><td class="align_center">37.90</td><td class="align_center">103.26</td><td class="align_center">30.34</td><td class="align_center">30.63</td><td class="align_center">0.99</td></tr><tr class="table-tr"><td colspan="7"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

<div>Calculation of crystallization completion rate when the solution temperature reaches 12°C.</div>

Advances in Materials Science and Engineering

tab2

Table 2

Table 2: The Equilibrium Time and Salt Expansion Characteristic of Sulfate Saline Soil upon Cooling 