The unusually weak and exceptionally steep radio relic in Abell 2108

TL;DR

This paper reports the discovery of an unusually weak and steep-spectrum radio relic in the low-mass galaxy cluster Abell 2108, highlighting its unique properties and potential shock re-acceleration scenario.

Contribution

It presents the first detailed analysis of a faint, steep-spectrum radio relic in a low-mass merging galaxy cluster, expanding understanding of relics in such environments.

Findings

Radio relic in Abell 2108 is exceptionally steep and weak.

The relic is associated with a temperature discontinuity indicating a shock.

A re-acceleration scenario explains the relic's offset and properties.

Abstract

Mergers between galaxy clusters often drive shocks into the intra cluster medium (ICM), the effects of which are sometimes visible via temperature and density jumps in the X-ray, and via radio emission from relativistic particles energized by the shock's passage. Abell2108 was selected as a likely merger system through comparing the X-ray luminosity to the Planck Sunyaev-Zeldovich signal, where this cluster appeared highly X-ray underluminous. Follow up observations confirmed it to be a merging low mass cluster featuring two distinct subclusters, both with a highly disturbed X-ray morphology. Giant Metrewave Radio Telescope (GMRT) data covering 120-750MHz show an extended radio feature resembling a radio relic, near the location of a temperature discontinuity in the X-rays. We measure a Mach number from the X-ray temperature jump. Several characteristics of radio relics are found in Abell2108, making this cluster one of the few low mass mergers likely hosting a radio relic. The radio spectrum is exceptionally steep, and the radio power is very weak (P1.4GHz=1E22W/Hz). To account for the shock/relic offset, we propose a scenario in which the shock created the relic by re-accelerating a cloud of pre-existing relativistic electrons and then moved away, leaving behind a fading relic. The electron aging timescale derived from the high-frequency steepening in the relic spectrum is consistent with the shock travel time to the observed X-ray discontinuity. However, the lower flux in GMRT band 4 data causing the steepening could be due to instrumental limitations, and deeper radio data are needed to constrain the spectral slope of the relic at high frequencies.