Self-Similar Collapse of a Self-Gravitating Viscous Disk
arXiv:astro-ph/9701189 · doi:10.1086/303964
Abstract
A self-similar solution for time evolution of isothermal, self-gravitating viscous disks is found under the condition that is constant in space (where is the viscosity parameter and is the ratio of a half-thickness to radius of the disk). This solution describes a homologous collapse of a disk via self-gravity and viscosity. The disk structure and evolution is distinct in the inner and outer parts. There is a constant mass inflow in the outer portions so that the disk has flat rotation velocity, constant accretion velocity, and surface density decreasing outward as . In the inner portions, in contrast, mass is accumulated near the center owing to the boundary condition of no radial velocity at the origin, thereby a strong central concentration being produced; surface density varies as . Moreover, the transition radius separating the inner and outer portions increases linearly with time. The consequence of such a high condensation is briefly discussed in the context of formation of a quasar black hole.
6 pages without figures. The paper has 3 figures (if you need figures, please send email to [email protected]). To appear in ApJ, 1997 May 1 issue
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