X-ray echoes from iron fluorescence near black holes, revealing accretion disk structure.Iron K-alpha reverberation is a technique that uses X-ray echoes from iron atoms near black holes to map the structure of the accretion disk. When a black hole's corona flares in X-rays, it illuminates the inner disk, causing iron atoms to fluoresce at 6.4 keV. The time delay between the flare and the fluorescence, and its spectral shape, reveal the disk's geometry, radius, and inclination. This method provides a direct probe of the strong gravity regime near the event horizon.
The iron K-alpha line was first detected in the 1990s by the ASCA satellite, and the reverberation mapping technique was developed in the early 2000s, notably by Andrew Fabian and colleagues.
A sudden X-ray flare from the corona irradiates the accretion disk. Iron atoms in the disk absorb these X-rays and re-emit fluorescent lines, primarily at 6.4 keV. Due to relativistic effects (Doppler boosting, gravitational redshift), the line is broadened and skewed. By measuring the time lag between the continuum flare and the iron line, astronomers infer the light travel time from corona to disk, giving the disk's radius. The line profile encodes the disk's inclination and the black hole's spin.
Used to measure black hole masses and spins, test general relativity in strong fields, and study accretion disk physics in active galactic nuclei and X-ray binaries.
The iron K-alpha line is so broadened near a black hole that its width can correspond to velocities exceeding 30% of the speed of light.




















