I know that planets can form through accretion, bulging up from $0$ to their final mass $\mathrm{M_{planet}}$ at $\mathrm{M}(t_f)$. I know that when studying Planetary formation and migration theories, sometimes this $\mathrm{M}$ function gets modelled, e.g., as a $\propto \tanh{(k\cdot t)}$ function. What I do not know and I'd like to ask you is:
- What kind of assumptions are we throwing in (proto-) planet formation models, e.g., to describe $\mathrm{M = M}(t)$? Is this well studied? Is planetary formation being studied through N-body simulations or similars?
Context: I'm not sure if we could constrain enough with experimental data. I don't know it at all though. But at the same time, it just comes to my mind that N-body simulations starting from "simple enough" statements could help model $d\mathrm{M}/dt$ for instance. I wondered if planet caracterization through N-body "accretion simulations" is (was) a subject or not? Closed? In development? What are the problems that are being solved on this? Related