3.1. Reverberation Mapping Assumptions
There are a number of simplifying assumptions that we can now make:
(17) |
The time it takes a Lyman photon to diffuse outward from the Strömgren depth is about 20 times the direct light-travel time 35,
(18) |
We also need to carry out our reverberation-mapping experiment on a time scale short enough that the structure of the BLR can be assumed to be stable. The dynamical, or cloud-crossing, time scale for the BLR is typically
(19) |
where VFWHM is the Doppler width of the broad line for which the response time = r/c has been measured. Any reverberation-mapping experiment has to be short relative to the crossing time or the structural information might be washed out by cloud motions.