Fig. 7

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Final vs initial mass for several simulation runs (see Table 3). The vertical lines denote 10% of m* = σ3 τsm⊙, which is the scale where pebble accretion begins. The dashed line is the identity line (y = x). Bodies ≳1022 grow their mass by several tenfold by pebble accretion and become dwarf planets. The gain in mass at low mass in the lami-1p-etairr and turb-1p-best is due to the slow pace of pebble accretion, allowing Safronov interactions to become important at low planetesimal masses.
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