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Accretion-disk self-gravity is the contribution of the disk's own matter to its gravitational field. A low total disk mass can still matter for local vertical confinement or the growth of density disturbances. The Toomre parameter compares gravity with pressure and rotation, but instability does not guarantee fragmentation: heating by gravitationally driven motions can balance cooling. Local numerical experiments distinguish that regulated state from breakup when cooling is sufficiently rapid.^[ref]

Charles F. Gammie studies accretion disks, black holes and computational approaches to their dynamics. His 2001 study used local, razor-thin models to investigate gravitational instability in a cooling astrophysical disk.

The models distinguish two outcomes. Sufficiently slow radiative cooling permits a fluctuating state in which dissipation of turbulence replaces the lost heat; faster cooling permits gravitational fragmentation. The reported transition depends on the local model and its assumptions. Its broader importance is the explicit link between an energy balance and whether a disk transports angular momentum or breaks into bound structures.^[ref]

A gas disk near $Q_T\sim 1$ need not form bound fragments: gravitational compression and shocks can heat it into a self-regulated spiral state. Fast enough cooling, often parameterized by $\beta =\Omega t_{\mathrm{cool}}$, permits collapse to continue. A numerical critical beta depends on thermodynamics, dimensionality and the cooling model; it is not universal.^[ref]

Gravitational instability of an astrophysical disk occurs when a density enhancement attracts enough additional matter for self-gravity to overcome the disk's restoring motions. It can generate spiral density waves or, under suitable thermal conditions, lead to cooling-limited disk fragmentation. Gas pressure and orbital motion oppose collapse on different scales.

For local axisymmetric disturbances of an inviscid razor-thin disk with surface density of a disk $\Sigma$, barotropic sound speed $c_s$ and radial epicyclic frequency $\kappa$, the compressive dispersion relation isThe razor-thin disk Poisson kernel supplies the attractive $|k|$ term. Pressure dominates at large wavenumber, while epicyclic motion stabilizes sufficiently small wavenumbers. Minimizing over $|k|$ gives $|k{|}_{\ast }=\pi G\Sigma /c_s^2$ and ${\omega }_{\min }^2={\kappa }^2[1-Q^{-2}]$, where the gas Toomre parameter is $Q=c_s\kappa /(\pi G\Sigma )$. Thus $Q<1$ admits exponential local axisymmetric growth; $Q=1$ is marginal. Collisionless stellar disks require a different random-motion treatment and numerical normalization.^[ref]

Linear growth does not guarantee bound fragments. Compression and shocks heat the gas; continued collapse depends on radiative cooling, transport and the tidal environment. Cooling-limited disk fragmentation therefore asks a further nonlinear question beyond whether an infinitesimal disturbance grows.^[ref]

A sufficiently self-gravitating disk can fragment directly, bypassing the slow assembly of a massive solid core. In the simplest thin gas-disk model the competition is between self-gravity, pressure and rotational shear. Axisymmetric perturbations havewhere $\kappa$ is the radial epicyclic frequency, not the opacity. In a nearly Keplerian disk, $\kappa \simeq \Omega$. This is Toomre's stability criterion; finite thickness and global/nonaxisymmetric modes modify the precise boundary. The fastest local wavelength is $\lambda =2c_s^2/(G\Sigma )$, of order the disk scale height times $2\pi$ when $Q_T\simeq 1$.

Instability alone does not ensure bound planets. Compression and shocks heat the gas, raising $Q_T$; a slowly cooling disk can maintain self-regulated spiral turbulence. Cooling-limited disk fragmentation requires energy loss on a sufficiently short dynamical timescale, conventionally expressed as $\beta =\Omega t_{\mathrm{cool}}$ below a model-dependent threshold. The often quoted $\beta \sim 3$ belongs to a particular local razor-thin calculation, not every real disk.^[ref] Cold massive outer disks are promising sites, but fragment contraction, tidal survival, further accretion and migration determine whether the result remains a planetary-mass body or grows into a brown dwarf.

For gravitational collapse of a settled particle layer, if “core collapse” instead denotes a solid-particle layer, its random-velocity dispersion replaces gas sound speed in an appropriate particle-disk stability condition. Settling and concentration can enable collapse into planetesimals; gas turbulence and particle stirring oppose it. This route makes solid seeds for later core accretion and is physically distinct from direct gas fragmentation. In both cases one must establish self-gravity against velocity support and tides, rather than infer collapse from high surface density alone.