Two integrations of the steady Keplerian viscous diffusion equation give this general transported quantity. fixes the mass accretion rate, while fixes the additive angular-momentum flux or inner torque. A zero-torque inner boundary condition gives ; a nonaccreting constant-torque disk has .
Freezing coefficients locally in the Keplerian viscous diffusion equation gives . A radial Fourier mode grows at rate . Negative response reverses ordinary smoothing and gives a backward heat equation, within the wavelength range where the thin disc transport closure applies.
Past exam of the mathematics course of the University of Cambridge 2012 iii Paper 61 1 iv Solution Created 2026-10-03 Updated 2026-10-07
The required pressure integral uses . With and ,The vertically averaged alpha closure for a mixed-pressure layer therefore givesThe height-integrated dynamic viscosity is . Equate it to to obtainThese are integrated equalities, not an imposed pointwise relation .
Now keep , the opacity and molecular constants independent of radius, and use Keplerian rotation . In the gas-dominated limit, but positive, the last equality gives . The column-density relation gives . Eliminating yields , whenceThis is the gas-pressure branch of a mixed-pressure alpha disk. In the radiation-dominated limit, , so andFor viscous stability of an accretion disk, linearize the Keplerian viscous diffusion equation at fixed radius: a local mass density perturbation has diffusion coefficient . The gas branch has and a positive derivative, so it smooths perturbations. The radiation branch has and a negative derivative, giving radiation-pressure viscous instability. The gas-pressure branch is viscously stable; the radiation-pressure branch is viscously unstable in this closure. This concerns radial mass-transport stability on wavelengths where the vertically averaged thin-disc model applies.
Past exam of the mathematics course of the University of Cambridge 2013 iii Paper 54 1 a Solution Created 2026-10-03 Updated 2026-10-07
Assume an axisymmetric thin disc rotating in the fixed potential of a dominant central mass, with independent of time and height. Neglect vertical mass loss and vertical angular-momentum flux at the two faces, as well as self-gravity and radial pressure corrections to the rotation law. Define the surface density and density-weighted kinematic viscosity byand let . These assumptions give the vertically averaged viscous disk equationswhere is specific angular momentum. Subtract times conservation of mass from conservation of angular momentum. Since is fixed in time,Substitution into conservation of mass proves the Keplerian viscous diffusion equationNo assumption of height-independent kinematic viscosity is needed; its density-weighted average is the one appearing in the integrated stress. A wind or surface magnetic stress would add terms and must not be silently discarded.
Viscous instability of an accretion disk Created 2026-09-28 Updated 2026-10-07
The negative-diffusion criterion for viscous disk instability is . A surface density enhancement then transports angular momentum less effectively and grows. Freezing the Keplerian viscous diffusion equation locally gives growth proportional to the square of radial wavenumber, within the thin-disc transport range; wavelengths must still be sufficiently long compared with the disk scale height for that closure. The formal short-wave limit is a backward heat equation.
Viscous stability of an accretion disk 2026-10-07
Within an instantaneous vertically averaged transport closure, the local Keplerian viscous diffusion equation has effective diffusion coefficient . A positive coefficient smooths short radial Fourier modes in the allowed thin-disc wavelength range; a negative coefficient gives the negative-diffusion criterion for viscous disk instability. A zero coefficient is linearly degenerate and does not establish strict decay. This local response criterion alone does not settle thermal, self-gravitating or boundary-driven stability.