Artículo

A high-energy study of the supernova remnant G296.5+10.0

Eppens, Laura Karina Icon; Combi, Jorge Ariel Icon; Reynoso, Estela Marta Icon; García, Federico Icon; Mestre, E. ; Abaroa, Leandro Icon; Romero, Gustavo Esteban Icon; Luque Escamilla, Pedro L. Icon; Martí, J.

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Fecha

02/2024

Editorial

Oxford University Press

Revista

Monthly Notices of the Royal Astronomical Society

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Institución organizadora

ISSN

0035-8711

eISSN

1365-2966

ISBN

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Inglés

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Clasificación temática

Resumen

We report a detailed multi-wavelength study of the supernova remnant G296.5+10.0 using archival data from XMM–Newton and Fermi-LAT complemented with ATCA observations. In the X-ray band, we performed an adaptive smoothing on the double background subtracted images to construct an X-ray mosaic map with six individual observations. Below 2.0 keV, G296.5+10.0 is asymmetrical, with the south-east side of the radio shell brighter than the south-west one. The spatially resolved X-ray spectral study confirms the thermal origin of the plasma, with enhanced metal abundances, probably arising from ejecta material according to the H I and infrared (140 μm) distributions. In the γ -ray band, we analysed 14 years of accumulated Fermi observations below 500 GeV via different fitting processes. To discuss the origin of the γ -ray emission, we compare the GeV results with H I structures probably associated with the SNR and with the radio spectral indices found at various positions towards the radio shell. Moreover, we identified diverse sources candidates to contribute γ -ray emissions observed. Also, we calculated the lepto-hadronic spectral energy distribution of the remnant for synchrotron, inverse Compton, Bremsstrahlung, and proton–proton processes. The emission at low energies can be explained by electron-synchrotron radiation, with a weak magnetic field of B = 25 μG, while the γ -ray data can be explained by hadronic interactions. Employing the reddening-distance method, we computed a distance of 1.4 kpc for the SNR, implying an age of 14 000 yr.

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