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Fig. 2

image

Sketch of the procedure we used to obtain the collisional cross section. In the comoving frame, the planetesimal resides at the origin (y = 0) and pebbles start at a distance yS far enough to be unperturbed by the gravity of the planetesimal. Integrations are first carried out in the x-direction, and the impact parameter bcoll,x is determined from the first and last trajectory that hits the planetesimal (xmin and xmax). Starting at the average of these two coordinates x0, the integrations are extended to the z-direction to obtain the vertical impact parameter bcoll,z.

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