On the physical nature of accretion disc viscosity
We use well-established observational evidence to draw conclusions about the fundamental nature of the viscosity in accretion discs. To do this, we first summarise the observational evidence for the value of the dimensionless accretion disc viscosity parameter $α$, defined by Shakura & Sunyaev (1973, 1976). We find that, for fully ionized discs, the value of $α$ is readily amenable to reliable estimation and that the observations are consistent with the hypothesis that $α\sim 0.2 - 0.3$. In contrast in discs that are not fully ionized, estimates of the value of $α$ are generally less direct and the values obtained are generally $ < 0.01$ and often $ \ll 0.01$. We conclude that this gives us crucial information about the nature of viscosity in accretion discs. First, in fully ionized discs the strength of the turbulence is always limited by being at most trans-sonic. This implies that it is necessary that credible models of the turbulence reflect this fact. Second, the smaller values of $α$ found for less ionized, and therefore less strongly conducting, discs imply that magnetism plays a dominant role. This provides important observational support for the concept of magneto-rotational instability (MRI) driven hydromagnetic turbulence.