Illuminating the Diffuse Radio Emission in Low-Mass Cluster: Abell 13
Nasmi S Anand, Swarna Chatterjee, Ramij Raja, Majidul Rahaman, Abhirup Datta
TL;DR
This paper investigates diffuse radio emission in the low-mass merging cluster Abell 13 using four-frequency, high-sensitivity radio data. The authors obtain a detailed morphological and spectral view, including the first spectral index and curvature maps for this emission, and find a largest linear size of about 521 kpc with a central origin and westward extension. The integrated spectrum is steep and curved (α ≈ −1.85 at 400 MHz and SC ≈ −0.93), consistent with re-energization of fossil AGN plasma via adiabatic compression, i.e., a radio phoenix. The results support a phoenix scenario associated with past AGN activity in the BCG and redistribution by ICM motions during the merger, highlighting the role of fossil plasma in shaping non-thermal phenomena in low-mass clusters and motivating polarization studies for further constraints on magnetic fields and dynamics.
Abstract
Recent advances in high-sensitivity radio observations have uncovered a population of faint, ultra-steep-spectrum sources in galaxy clusters, commonly known as radio phoenixes. However, their observational classification remains poorly constrained due to the limited number of confirmed detections. This study presents a detailed multi-frequency, high-sensitivity, and high-resolution analysis of diffuse radio emission in the merging galaxy cluster Abell 13. Using GMRT (147.5 MHz), uGMRT (400 MHz), ASKAP-low (887.5 MHz), and MGCLS (1284 MHz) images, we detect complex, filamentary diffuse emission with a largest linear extent of 521 kpc. This emission originates from the cluster center and extends westward, confined within the X-ray-emitting intra-cluster medium (ICM). Chandra X-ray data confirm that Abell 13 is undergoing a merger, and the radio morphology reflects signatures of this ongoing dynamical activity. We observed filamentary structures extending towards east-northeast and southwest directions. The spectral index across the emission appears irregular and lacks a coherent spatial gradient. The integrated spectrum reveals a steep spectral index of -1.85 +/- 0.05 and a spectral curvature of -0.93 +/- 0.21. These spectral properties, along with the observed morphology and brightness distribution, are consistent with a re-energization of a fossil radio plasma driven by adiabatic compression, supporting the classification of the emission as a radio phoenix.
