“…where c′ � effective cohesion, c t ′ � unified effective cohesion, c tt � unified total cohesion, φ′ � effective internal friction angle, φ t ′ � unified effective internal friction angle, φ b � friction angle relative to matric suction, φ b t � unified friction angle with matric suction, u a � pore-air pressure, u w � pore-water pressure, u a −u w � matric suction, σ � total normal stress, σ−u a � net normal stress, b � unified strength theory parameter, and 0 ≤ b ≤ 1. e parameter b represents the effect of intermediate principal stress on the strength of unsaturated soils, and it can be calculated by the values of basic mechanical properties (e.g., uniaxial compressive strength, uniaxial tensile strength, and pure shear strength) or comparing the limit loci of equation (1) with true triaxial tests of unsaturated soils on a deviatoric plane. In addition, the friction angle φ b is simply taken as a constant not larger than the effective internal friction angle φ′, and its variation with respect to matric suction can be well addressed by a hyperbolic function similar to that of Zhang et al [29] and Yan et al [30].…”