Black Hole Formation by Rossby Vortices

Physics

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Scientific paper

The central galactic black hole, BH, mass is predicted from the collapse of an initial Lyman-α cloud. Damped Lyman-α clouds are the first large scale, (R_Lyman_α ~= 300 kpc, M_Lyman_α ~= 10^11 M_solar, and Σ_Baryonic ~= 10-4 g cm-2) structures. The rotation velocity of the combined dark and baryonic matter compared to that required for Keplerian support is small, λ ~= .07. The baryonic matter collapses homologously by shocks and cooling with conserved angular momentum. Upon reaching a radius of partial Keplerian support where the Mclauren spheroid instability, λ_spheroid ~= 0.4 is initiated then tidal torquing produces the "flat rotation curve" (FRC). This occurs when R_spheroid/R_cloud ~= (λ_cloud/ λ_spheroid)^2 , and where the mass thickness Σ_spheroid ~= Σ_Lyman_α (R_spheroid/R_cloud)^2 ~= Σ_Lyman-α (λ_cloud/ λ_spheroid)^4 ~= 0.1 g cm-2. The interior baryonic mass following the FRC condition then becomes M_flat = M_spheroid (R/R_spheroid) and Σ_flat = Σ_spheroid (R_spheroid/R). Thus as the FRC forms, the mass thickness increases as ∝ 1/R. At a critical thickness Σ_Rossby ~= 100 g cm-2, the Rossby vortex instability forms because of the confinement of heat. All of the mass of the resulting accretion disk collapses to a BH where M_BH = M_spheroid (Σ_spheroid/Σ_Rossby) = M_Lyman_α (λ_cloud/ λ_spheroid)^4 (Σ_Lyman_α/ Σ_Rossby) ~= 10^8 M_solar.

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