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Dust survivability

Dust grains are highly efficient radiators and hence can thermally decouple from the surrounding hot gas. Under the conditions envisaged here, there are two grain destruction mechanisms that must be considered. First, if the grains themselves become too hot, they will rapidly sublime. The grain temperature will be set by the thermal equilibrium between the AGN radiation incident on a given grain and the thermal radiation emitted by that grain (e.g. see Barvainis 1987). For MCG-6-30-15, the sublimation radius (i.e. the radius from the AGN within which dust grains become so hot that they sublime) is tex2html_wrap_inline2172 . Thus, any dust grains within the inner warm absorber would be rapidly sublimed by the intense radiation field. Dust in the outer warm absorber would not be subject to significant sublimation.

The second dust destruction mechanism that we must consider is thermal sputtering. If we make the standard assumption that the (outer) warm absorber is photoionized, then photoionization models suggest that the gas temperature is only tex2html_wrap_inline2174 and thermal sputtering is negligible. If, instead, we suppose that the outer warm absorber is purely collisionally-ionized, gas temperatures of tex2html_wrap_inline2176 are required in order to achieve the observed ionization states (Shull & van Steenberg 1982). From the expressions of Burke & Silk (1974), the thermal sputtering timescale for this temperature is

equation383

where n is the electron number density in the gas. Suppose that r is the distance of the outer warm absorber from the central engine, and L is the (ionizing) luminosity of the central engine. Furthermore, define tex2html_wrap_inline2186 to be the ionization parameter of a photoionized plasma in which oxygen is ionized to the same degree as seen in the outer warm absorber of MCG-6-30-15. Given our (temporary) hypothesis that the plasma is collisionally-ionized, the density must satisfy

equation390

or else photoionization would dominate the ionization state. Evaluating the sputtering timescale for the parameters of MCG-6-30-15 gives

equation394

For comparison, the flow timescale of the outer warm absorber is

equation399

where we have adopted a typical value of tex2html_wrap_inline2196 for the velocity of the outer warm absorber, as indicated by UV absorption line studies of other AGN (Mathur, Elvis & Wilkes 1995). It can be seen that the flow timescale of the warm absorber always exceeds the sputtering timescale unless tex2html_wrap_inline2198 . If the outer warm absorber was situated at such a large distance, then either we would have to be viewing the AGN along a very special line of sight, or else the mass, M, and kinetic energy, tex2html_wrap_inline2202 , associated with the outflow would both be huge. From the expressions of Reynolds & Fabian (1995), and assuming a global covering fraction of tex2html_wrap_inline2204 , we get tex2html_wrap_inline2206 and tex2html_wrap_inline2208 . The initial acceleration of this material would be extremely problematic to understand. We consider this possibility to be unphysical. Thus, in the absence of a viable, collisionally-ionized model, the observation of a dusty warm absorber may be taken as further evidence that photoionization dominates the state of this plasma.

Whilst dust can survive in warm photoionized gas, it is extremely difficult to form dust in such an environment: the grains could never assemble at such temperatures. Furthermore, a comparison of the column density of the warm absorber with the cold column expected to be associated with the reddening reveals that the warm-gas/dust ratio in the warm absorber must be very similar to the cold-gas/dust ratio in our Galaxy. These two facts taken together suggest that the warm material originates from dusty cold material, possibility via radiative heating, and that a substantial fraction of the dust survives the heating process. The putative dusty molecular torus of Seyfert unification schemes might be a possible progenitor of such a radiatively-driven, warm, dusty outflow.


next up previous
Next: Photoionization models Up: Dusty warm absorbers Previous: Dusty warm absorbers

Chris Reynolds
Wed Jul 2 14:33:32 MDT 1997