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Table 1

Results of the two sets of simulations, with and without planetesimal fragmentation (PF).

# km km km km

Without PF With PF Without PF With PF Without PF With PF Without PF With PF
M C t M C t M C t M C t M C t M C t M C t M C t
(M) (Myr) (M) (Myr) (M) (Myr) (M) (Myr) (M) (Myr) (M) (Myr) (M) (Myr) (M) (Myr)

2 23.10 4.41 0.04 6.00 5.84 6.00 0.04 6.00 0.35 6.00 0.06 6.00 0.11 6.00 0.11 6.00
4 32.23 0.39 0.09 6.00 21.37 2.99 0.08 6.00 9.17 6.00 0.18 6.00 0.56 6.00 0.52 6.00
6 35.25 0.17 0.20 6.00 27.55 0.92 0.12 6.00 21.55 3.27 0.39 6.00 2.13 6.00 1.34 6.00
8 (...) (...) 0.45 6.00 35.73 0.33 0.15 6.00 27.77 1.64 0.67 6.00 14.99 6.00 3.58 6.00
10 (...) (...) 0.77 6.00 45.78 0.15 0.18 6.00 32.64 0.99 1.00 6.00 25.06 4.07 7.13 6.00

Notes. The first column corresponds to the disk mass. A value of # means that we consider a disk # times more massive than the minimum mass solar nebula (MMSN) of Hayashi (1981). MC represents the core mass when the planet achieves the critical mass and t represents the time at which this occurs. Simulations stopped at t = 6 Myr, so that in this case MC represents the core mass at this time. For km and for disks 8 and 10 times more massive than the MMSN, planetesimal accretion rates become so high that models do not converge when planetesimal fragmentation is not considered.

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