Impact on porous targets: Penetration, crater formation, target compaction, and ejection

C. RINGL; E.M. BRINGA; H.M. URBASSEK

PHYSICAL REVIEW E

AMER PHYSICAL SOC

Año: 2012 vol. 86 p. 61313 - 61321

1539-3755

Using a granular-mechanics code, we study the impact of a sphere into a porous adhesive granular target, consisting of monodisperse silica grains. The model includes elastic repulsive, adhesive, and dissipative forces, as well as sliding, rolling, and twisting friction. Impact velocities of up to 30 m/s and target filling factors (densities) between 19% and 35% have been systematically studied. We find that the projectile is stopped by an effective drag force which is proportional to the square of its velocity. Target adhesion influences projectile stopping only below a critical velocity, which increases with adhesion. The penetration depth depends approximately logarithmically on the impact velocity and is inversely proportional to the target density. The excavated crater is of conical form and is surrounded by a compaction zone whose width increases but whose maximum value decreases with increasing target density. Grain ejection increases in proportion with impactor velocity. Grains are ejected which have originally been buried to a depth of 8Rgrain below the surface; the angular distribution favors oblique ejection with a maximum around 45∘. The velocity distribution of ejected grains features a broad low-velocity maximum around 0.5–1 m/s but exhibits a high-velocity tail up to ∼15% of the projectile impact velocity.