“…The bulk modulus 𝐾 𝑒𝑣0 = 𝐸∕(3 ⋅ (1 − 2𝜈)) and the shear modulus 𝐺 𝑒𝑠0 = 𝐸∕(2 ⋅ (1 + 𝜈)) are calculated with the Poisson's ratio (𝜈 = 0.35 reported in Wichtmann et al 3 for Karlsruhe fine sand) and the Young's modulus 𝐸, from the initial inclination of the measured 𝑞(𝜖 1 ) curves in the drained monotonic triaxial tests. Pastor et al 1 and subsequently, other authors [24][25][26]49,50 recommended a default value of 𝛼 = 0.45 for different sands, for example, Hostun, Sacramento River, Banding, Niigata, Reid , and Fuji. Hereby, a drained monotonic triaxial test with un-and reloading cycles from 53 (named TMCD4, initial void ratio 𝑒 0 = 0.82) as well as a series of undrained triaxial tests considering pyknotropy effects, as listed in Table 1 (named TMU2, 5, 6, 8, 11, and 12), were used to inspect the influence of 𝛼 on both models.…”