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Fig. 8

image

SPH model of a cratering on a D = 150 km target. Its cross section in the (x, y) plane is shown, with colors corresponding to the logarithm of velocity |v|. The number of SPH particles used was Npart ≐7.0 × 105. The time t ≐ 100 s corresponds to the end of fragmentation phase. (The reaccumulation phase is computed later by an N-body model with self-gravity.) The original projectile had size d = 8 km, velocity vimp = 6 km s−1, and hit the target at a very oblique angle ϑimp = 75°. Green lines indicate the distances s which wouldbe travelled by particles within the ballistic time. Consequently, the diameter of the resulting (transient) crater should be at least dcrater ≃ 60 km.

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