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ASASSN-14ms:the Most Energetic Known Explosion of a Type Ibn Supernova and its Physical Origin

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arxiv 2106.06690 v1 pith:RY5MRVH4 submitted 2021-06-12 astro-ph.HE astro-ph.SR

classification astro-ph.HEastro-ph.SR
keywords asassn-14mslightpost-peakaroundconsistentcurvesdeclineejecta
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ASASSN-14ms may represent the most luminous Type Ibn supernova (SN~Ibn) ever detected, with an absolute U-band magnitude brighter than -22.0 mag and a total bolometric luminosity >1.0x10^{44} erg/s near maximum light. The early-time spectra of this SN are characterized by a blue continuum on which are superimposed narrow P~Cygni profile lines of He I, suggesting the presence of slowly moving (~1000 km/s), He-rich circumstellar material (CSM). At 1--2 months after maximum brightness, the He I line profiles become only slightly broader, with blueshifted velocities of 2000--3000 km/s, consistent with the CSM shell being continuously accelerated by the SN light and ejecta. Like most SNe~Ibn, the light curves of ASASSN-14ms show rapid post-peak evolution, dropping by ~7 mag in the V band over three months. Such a rapid post-peak decline and high luminosity can be explained with interaction between SN ejecta and helium-rich CSM of 0.9~M_{\odot} at a distance of~10^{15} cm. The CSM around ASASSN-14ms is estimated to originate from a pre-explosion event with a mass-loss rate of 6.7~M_\odot /yr (assuming a velocity of ~1000 km/s), which is consistent with abundant He-rich material violently ejected during the late Wolf-Rayet (WN9-11 or Opfe) stage. After examining the light curves for a sample of SNe~Ibn, we find that the more luminous ones tend to have slower post-peak decline rates, reflecting that the observed differences may arise primarily from discrepancies in the CSM distribution around the massive progenitors.

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  1. Wild behaviour near the finish line: the Type Ibn SN 2020able and its stratified environment

    astro-ph.HE 2026-08 conditional novelty 6.0 of 10

    The Type Ibn supernova SN 2020able exploded inside a stratified, three-component helium-rich envelope, with an inner dense shell from a pre-explosion eruption and an outer shell consistent with a Wolf-Rayet wind.

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