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As a result, boundary markers often shift from their designated positions due to the upward movement of rocks resulting from the volumetric expansion of ice beneath road beds (Taivainen, 1963). Additional F/T studies as outlined in Table 3 at different fill volumes from 20 to 500 mL in various appropriately sized containers were also evaluated and no significant increase in percent aggregates was detected. For freeze-drying microscopy, protein sample was dispensed into a glass cell and placed on a temperature-controlled freeze-drying stage. It was observed that the GWC at the PWP was still significantly higher in BB-amended CL soil compared to SM soil. Furthermore, in both test conditions, the GWC was observed to be highest at lower suctions (500 kPa), and lowest at higher suctions (180?×?103 kPa) at a fixed BB content for both soils. The GWC follows a similar decrease pattern at both lower (500 kPa) and higher suction (180?×?103 kPa) levels in confined conditions for both soils, as presented in Fig. The occurrence is attributable to the greater SSA and the existence of minerals in the CL soil with water-retentive properties. However, the subsequent inclusion of 3.5% and 5% BB in CL soil resulted in a strength reduction of 12.92% and 24.29%, respectively, compared to non-amended CL soil for day one. The results indicate that the CL soil amended with BB reached its peak strength at a 2% biochar content.
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