To determine the void ratio (e) and degree of saturation (S) for the given soil, we first need to find the dry density (ρ_d) and the specific gravity (G_s). The dry density can be calculated using the formula ( \rho_d = \frac{m}{V} ), where ( m ) is the mass of the dry soil and ( V ) is the volume. The mass of the dry soil can be calculated as ( m = \frac{mass}{1 + moisture\ content} = \frac{41.54}{1 + 0.232} \approx 33.69 ) kg, giving a dry density of ( \rho_d = \frac{33.69}{0.02135} \approx 1575.68 ) kg/m³.
Next, the void ratio ( e ) can be found using ( e = \frac{G_s \cdot \rho_w}{\rho_d} - 1 ), where ( \rho_w ) (density of water) is approximately 1000 kg/m³. Substituting ( G_s = 2.722 ) and ( \rho_d \approx 1575.68 ) kg/m³, we find ( e \approx 0.662 ).
To find the degree of saturation ( S ), we can use the formula ( S = \frac{w \cdot \rho_d}{e \cdot \rho_w} ), where ( w ) is the moisture content as a decimal (0.232). Plugging in the values, we get ( S \approx \frac{0.232 \cdot 1575.68}{0.662 \cdot 1000} \approx 0.223 ) or 22.3%.
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