TY - JOUR
T1 - Scale size effect in momentum enhancement
AU - Walker, James D.
AU - Chocron, Sidney
AU - Durda, Daniel D.
AU - Grosch, Donald J.
AU - Movshovitz, Naor
AU - Richardson, Derek C.
AU - Asphaug, Erik
N1 - Funding Information:
We thank Walter Huebner for his encouragement and support of this work. This research was partially supported by the NASA Outer Planets Research program, grant NNG06GE91G and by Southwest Research Institute.
PY - 2013
Y1 - 2013
N2 - When an impactor strikes a body at hypervelocities the momentum transferred to the impacted body is greater than the initial impactor momentum. This effect is due to the crater ejecta, and when the impacted body's mass provides some of the momentum change, the effect is referred to as momentum enhancement. The small amount of data on this question implies that there is a scale effect - that is, as the projectile size increases there is an increase in the imparted momentum beyond that anticipated due to the increase in projectile size. Recently, experimental data was gathered on the increase in momentum caused by crater ejecta when 4.45-cm diameter aluminum spheres struck granite targets. The amount of momentum enhancement (characterized by the ratio β) was greater than 2 for 2 km/s impacts. Compared with other data at much smaller scale, these tests imply an impactor scale and an impactor density effect for hypervelocity strikes into rock. The implied impactor size scale effect is surprisingly large - to a 0.4 power - and extrapolation indicates that a 1-meter aluminum sphere striking a consolidated rock surface at 10 km/s could have a β exceeding 40, supposing the scale size effect does not saturate on the order of 10 cm. Such a large momentum enhancement shows that kinetic impactors can be very efficient at deflecting asteroids.
AB - When an impactor strikes a body at hypervelocities the momentum transferred to the impacted body is greater than the initial impactor momentum. This effect is due to the crater ejecta, and when the impacted body's mass provides some of the momentum change, the effect is referred to as momentum enhancement. The small amount of data on this question implies that there is a scale effect - that is, as the projectile size increases there is an increase in the imparted momentum beyond that anticipated due to the increase in projectile size. Recently, experimental data was gathered on the increase in momentum caused by crater ejecta when 4.45-cm diameter aluminum spheres struck granite targets. The amount of momentum enhancement (characterized by the ratio β) was greater than 2 for 2 km/s impacts. Compared with other data at much smaller scale, these tests imply an impactor scale and an impactor density effect for hypervelocity strikes into rock. The implied impactor size scale effect is surprisingly large - to a 0.4 power - and extrapolation indicates that a 1-meter aluminum sphere striking a consolidated rock surface at 10 km/s could have a β exceeding 40, supposing the scale size effect does not saturate on the order of 10 cm. Such a large momentum enhancement shows that kinetic impactors can be very efficient at deflecting asteroids.
KW - Cratering
KW - Failure modeling
KW - Hypervelocity impact
KW - Impact experiments
KW - Momentum enhancement
KW - Scaling
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U2 - 10.1016/j.proeng.2013.05.028
DO - 10.1016/j.proeng.2013.05.028
M3 - Conference article
AN - SCOPUS:84891666642
SN - 1877-7058
VL - 58
SP - 240
EP - 250
JO - Procedia Engineering
JF - Procedia Engineering
T2 - 12th Hypervelocity Impact Symposium, HVIS 2012
Y2 - 16 September 2012 through 20 September 2012
ER -