The correct answer is (c) \(\frac{σ_1}{σ_3} = tan^2 (45°+\frac{φ}{2})\)
To explain I would say: The stress condition during plastic equilibrium is given by,
\(σ_1=2c \,tan(45°+\frac{φ}{2})+σ_3 tan^2 (45°+\frac{φ}{2}),\) and for cohesion-less soil, c=0,
∴ \(\frac{σ_1}{{σ_3}} = tan^2 (45°+\frac{φ}{2}).\)