SNR 1987A : Spitzer data from days 6000 to 8000 revisited
Patrice Bouchet, René Gastaud, Alain Coulais, Richard G. Arendt
TL;DR
This study revisits the Spitzer-derived SED of SN 1987A between days 6000–8000, testing whether the near-IR excess at 3–5 μm can be explained by self-absorbed free-free emission rather than warm amorphous carbon dust. By decomposing the IR–radio SED into five components (warm carbon dust, silicates, cold dust, free-free, and synchrotron) and fitting days 7200 and 7400, the authors find that a self-absorbed free-free model yields statistically competitive fits and a physically plausible, though tightly constrained, set of parameters (gas temperature ≈ 1.3–1.4×10^3 K, ionization proxy (1−ξ) ≈ 0.07–0.08, and a cold-dust mass around ∼0.16–0.18 M_⊙). The analysis reveals a linear growth of warm carbon and silicate dust masses over the period and suggests that collisionally heated, relatively cool gas in the ER could power the short-wavelength excess under specific conditions, with the free-free cut-off frequency tied to the total emitting gas mass. The findings motivate continued JWST observations and coordinated radio data to test the persistence and origin of the free-free hypothesis across later epochs. Overall, the work demonstrates that free-free emission can formally describe the 3–5 μm excess, though it requires particular parameter choices and remains subject to interpretation regarding the gas heating and mass in the ER.
Abstract
An excess emission has been observed by Spitzer in the [3, 5] micron range of the SNR 1987A spectrum. It is generally argued that this excess could be due to the presence of warm amorphous carbon dust in the equatorial ring (ER) around the supernova, but the proposed models all have problems. This prompted us to present an alternative view on the interpretation of the Spectral Energy Distribution (SED) of SNR 1987A from the near-IR wavelengths to the radio frequencies (from 3 micron up to 1.4 GHz), between 6000 and 8000 days after outburst. We argue that the origin of that excess could be attributed instead to a free-free emission. We show that under very specific conditions (the free-free is self-absorbed at a cut-off frequency imposed by the mass of the emitting region), it could be produced by collisional heating of the gas. We then discuss the time evolution of the various components of the SED. We establish a linear relationship between the growth of the warm carbon dust mass and that of the silicates dust during the analyzed period. Finally, we build the Spitzer light curves and we show that our models reproduce the observations pretty well, although our study clearly favors the free-free case. In conclusion, we argue that the free-free model provides a formally very good description of the data, however the model does require some very specific parameter choices, and results in an unusually low temperature for the ionized gas.
