The Necessity of Feedback Physics in Setting the Peak of the Initial Mass Function

TL;DR

This paper argues that feedback physics, such as radiative heating from stars, is essential to establish a characteristic mass scale in the initial mass function of stars, which pure isothermal turbulence models fail to produce.

Contribution

It demonstrates that including feedback physics like radiative heating in star formation models creates a stable characteristic mass scale consistent with observations.

Findings

Pure isothermal turbulence models produce scale-free IMFs.

Feedback mechanisms like radiative heating set a nearly invariant characteristic mass.

Models without feedback do not reproduce the observed IMF peak.

Abstract

A popular theory of star formation is gravito-turbulent fragmentation, in which self-gravitating structures are created by turbulence-driven density fluctuations. Simple theories of isothermal fragmentation successfully reproduce the core mass function (CMF) which has a very similar shape to the initial mass function (IMF) of stars. However, numerical simulations of isothermal turbulent fragmentation thus far have not succeeded in identifying a fragment mass scale that is independent of the simulation resolution. Moreover, the fluid equations for magnetized, self-gravitating, isothermal turbulence are scale-free, and do not predict any characteristic mass. In this paper we show that, although an isothermal self-gravitating flow does produce a CMF with a mass scale imposed by the initial conditions, this scale changes as the parent cloud evolves. In addition, the cores that form undergo further fragmentation and after sufficient time forget about their initial conditions, yielding a scale-free pure power-law distribution $\mathrm{d} N/\mathrm{d} M\propto M^{-2}$ for the stellar IMF. We show that this problem can be alleviated by introducing additional physics that provides a termination scale for the cascade. Our candidate for such physics is a simple model for stellar radiation feedback. Radiative heating, powered by accretion onto forming stars, arrests the fragmentation cascade and imposes a characteristic mass scale that is nearly independent of the time-evolution or initial conditions in the star-forming cloud, and that agrees well with the peak of the observed IMF. In contrast, models that introduce a stiff equation of state for denser clouds but that do not explicitly include the effects of feedback do not yield an invariant IMF.