SN 2016coi (ASASSN-16fp): an energetic H-stripped core-collapse supernova from a massive stellar progenitor with large mass loss
G. Terreran, R. Margutti, D. Bersier, J. Brimacombe, D. Caprioli, P., Challis, R. Chornock, D. L. Coppejans, Subo Dong, C. Guidorzi, K. Hurley, R., Kirshner, G. Migliori, D. Milisavljevic, D. M. Palmer, J. L. Prieto, L., Tomasella, P. Marchant, A. Pastorello, B. J. Shappee

TL;DR
SN 2016coi is an energetic hydrogen-stripped supernova from a massive star with significant pre-explosion mass loss, showing evidence of helium in ejecta, large ejecta mass, and strong X-ray and radio emissions, but no shock breakout detection.
Contribution
This study provides comprehensive multi-wavelength observations and modeling of SN 2016coi, revealing its progenitor's large mass, significant mass loss, and properties bridging normal and relativistic supernovae.
Findings
Ejecta mass ~4-7 solar masses and kinetic energy ~7-8 x 10^{51} erg.
Presence of helium in ejecta due to Ni mixing.
High pre-explosion mass-loss rate (~1-2 x 10^{-4} M_sun/yr).
Abstract
We present comprehensive observations and analysis of the energetic H-stripped SN 2016coi (a.k.a. ASASSN-16fp), spanning the -ray through optical and radio wavelengths, acquired within the first hours to 420 days post explosion. Our campaign confirms the identification of He in the SN ejecta, which we interpret to be caused by a larger mixing of Ni into the outer ejecta layers. From the modeling of the broad bolometric light curve we derive a large ejecta mass to kinetic energy ratio (, ). The small [\ion{Ca}{ii}] \lam\lam7291,7324 to [\ion{O}{i}] \lam\lam6300,6364 ratio (0.2) observed in our late-time optical spectra is suggestive of a large progenitor core mass at the time of collapse. We find that SN 2016coi is a luminous source of X-rays ( in the…
| Yamanaka et al. (2017) | Kumar et al. (2018) | Prentice et al. (2018) | This Work | |
|---|---|---|---|---|
| Distance (modulus ) | 17.2 Mpc (31.18 mag) | 18.1 Mpc (31.29 mag) | 15.8 Mpc (31 mag) | Mpc (31.29 mag) |
| Color Excess | 0.075 mag | 0.074 mag | 0.205 mag | 0.075 mag |
| Explosion Date | MJD 57532.5 | MJD 57533.9 | MJD 57533.5 | MJD 57531.9 |
| Nickel Mass | 0.15 M⊙ | 0.10 M⊙ | 0.14 M⊙ | 0.15 M⊙ |
| Ejecta Mass | 10 M⊙ | M⊙ | M⊙ | M⊙ |
| Kinetic Energy | erg | erg | erg | erg |
| He Velocity | km s-1 | km s-1 | km s-1 | km s-1 |
| Code | Telescope | Instrument | Pixel size | FoV | Filters | ||
|---|---|---|---|---|---|---|---|
| ASA | 14cm Brutus121212Operated by the ASAS-SN team (Shappee et al., 2014). | Fairchild CCD3041 | 7.8″ | 4.47° | 4.47° | V | |
| \rowcolorgray!20 RK | 25cm Meade SCT 131313Operated by R. A. Koff at Antelope Hills Observatory, Bennett, CO, USA. | Apogee AP-47 | 1.02″ | 17.4′ | 17.4′ | BVRI | |
| JB | 43cm PlaneWave CDK 141414Operated by Joseph Brimacombe at New Mexico Skies, New Mexico, USA. | SBIG STL-6303 | 0.63″ | 34′ | 22′ | BVri | |
| \rowcolorgray!20 GS | 43cm PlaneWave CDK 151515Operated by Geoffrey Stone at Sierra Remote Observatories, Auberry, CA, USA. | SBIG STXL-11002 | 0.63″ | 42′ | 28′ | BV | |
| T50 | T50 161616Operated by the Astronomical Observatory of the University of Valencia (OAUV) at Aras de los Olmos, Valencia, Spain. | ProLine PL16801 | 0.54″ | 36.9′ | 36.9′ | BVri | |
| \rowcolorgray!20 Gem | Gem171717Operated by the University of Iowa at Iowa Robotic Observatory. | SBIG 6303e | 1.08″ | 27.6′ | 18.4′ | BVgri | |
| DEM | 51cm PlaneWave CDK181818Operated by DEMONEXT (Villanueva et al., 2018). | Fairchild CCD3041 | 0.90″ | 30.7′ | 30.7′ | BVri | |
| \rowcolorgray!20 WHO | WHO 1m telescope 191919Operated by the Weihai Observatory of Shandong University, China. | Andor iKon-L DZ936-N | 0.35″ | 12′ | 12′ | BVri | |
| LCOGT | Las Cumbres Observatory (LCOGT) | Sinistro | 0.40″ | 26′ | 26′ | BVgri | |
| \rowcolorgray!20 1.82 | 1.82m Copernico | AFOSC | 0.52″ | 8.7′ | 8.7′ | UBVRIugriz | |
| REM-IR | 0.58″ | 9.1′ | 9.1′ | JHK | |||
| REM | Rapid Eye Mount (REM) | ROSS2 | 1.22″ | 9.9′ | 9.9′ | griz | |
| \rowcolorgray!20 | IO:O | 0.30″ | 10′ | 10′ | BVgriz | ||
| \rowcolorgray!20 LT | Liverpool Telescope | IO:I | 0.18″ | 6.3′ | 6.3′ | H | |
| NOTCam | 0.24″ | 4′ | 4′ | JHK | |||
| NOT | Nordic Optical Telescope (NOT) | ALFOSC | 0.19″ | 6.4′ | 6.4′ | UBVugriz | |
| \rowcolorgray!20 MMT | Multiple Mirror Telescope (MMT) | MMTCam | 0.08″ | 2.7′ | 2.7′ | gri | |
| UV-W1,M2,W2 | |||||||
| UVOT | Ultraviolet Optical Telescope (UVOT)202020on board the Neil Gehrels Swift Observatory. | MIC212121Microchannel plate intensified CCD. | 0.50″ | 17′ | 17′ | UBV | |
| MJD | u | g | r | i | z | Instrument |
|---|---|---|---|---|---|---|
| (mag) | (mag) | (mag) | (mag) | (mag) | ||
| 57536.14 | 15.20 (0.04) | 15.46 (0.03) | NOT | |||
| 57536.40 | 15.80 (0.05) | 15.17 (0.05) | 15.55 (0.10) | Gem | ||
| 57537.15 | 14.84 (0.15) | 15.09 (0.11) | NOT | |||
| 57537.41 | 15.43 (0.04) | 14.87 (0.05) | 15.25 (0.10) | Gem | ||
| 57538.39 | 15.17 (0.04) | 14.63 (0.05) | 15.03 (0.10) | Gem | ||
| 57539.39 | 14.93 (0.04) | 14.43 (0.05) | 14.83 (0.10) | Gem | ||
| 57539.76 | 14.69 (0.16) | WHO | ||||
| 57540.17 | 15.68 (0.03) | 14.76 (0.03) | 14.25 (0.03) | 14.61 (0.02) | 14.56 (0.03) | LT |
| 57540.76 | 14.14 (0.05) | 14.59 (0.04) | WHO | |||
| 57541.40 | 14.59 (0.04) | 14.14 (0.05) | 14.54 (0.10) | Gem | ||
| 57541.75 | 14.11 (0.06) | 14.48 (0.06) | WHO | |||
| 57542.21 | 15.61 (0.04) | 14.47 (0.02) | 14.04 (0.03) | 14.39 (0.03) | 14.24 (0.02) | LT |
| 57542.38 | 13.99 (0.03) | 14.39 (0.06) | DEM | |||
| 57543.37 | 14.35 (0.05) | 13.90 (0.06) | 14.32 (0.10) | Gem | ||
| 57543.41 | 13.89 (0.03) | 14.30 (0.06) | DEM | |||
| 57544.37 | 14.29 (0.04) | 13.86 (0.05) | 14.22 (0.10) | Gem | ||
| 57544.44 | 13.80 (0.03) | 14.23 (0.06) | DEM | |||
| 57545.34 | 13.74 (0.03) | 14.17 (0.06) | DEM | |||
| 57545.39 | 14.21 (0.05) | 13.77 (0.07) | 14.15 (0.10) | Gem | ||
| 57546.22 | 14.20 (0.10) | NOT | ||||
| 57546.29 | 14.22 (0.09) | 13.70 (0.06) | 14.13 (0.13) | REM | ||
| 57546.39 | 14.19 (0.04) | 13.72 (0.06) | 14.09 (0.10) | Gem | ||
| 57546.43 | 13.68 (0.06) | 14.10 (0.06) | LCOGT | |||
| 57546.44 | 13.68 (0.03) | 14.10 (0.06) | DEM | |||
| 57547.33 | 13.65 (0.03) | 14.07 (0.06) | DEM | |||
| 57547.37 | 13.65 (0.07) | 14.06 (0.10) | REM | |||
| 57547.37 | 14.16 (0.04) | 13.71 (0.05) | 14.08 (0.10) | Gem | ||
| 57548.38 | 13.62 (0.08) | 14.04 (0.11) | REM | |||
| 57549.42 | 14.15 (0.06) | 13.59 (0.06) | 14.02 (0.11) | REM | ||
| 57549.43 | 13.60 (0.03) | 13.96 (0.05) | LCOGT | |||
| 57550.41 | 13.62 (0.03) | 13.97 (0.05) | LCOGT | |||
| 57550.44 | 13.59 (0.06) | 13.95 (0.12) | REM | |||
| 57551.19 | 15.92 (0.06) | 14.19 (0.02) | 13.54 (0.04) | 13.97 (0.04) | 13.69 (0.03) | LT |
| 57551.42 | 13.56 (0.04) | 13.93 (0.06) | DEM | |||
| 57552.06 | 15.96 (0.06) | 14.19 (0.03) | 13.58 (0.02) | 13.95 (0.03) | 13.64 (0.03) | LT |
| 57552.35 | 14.22 (0.04) | 13.62 (0.05) | 13.95 (0.10) | Gem | ||
| 57553.17 | 16.10 (0.06) | 14.29 (0.05) | 13.59 (0.06) | 13.89 (0.06) | 13.55 (0.04) | LT |
| 57553.19 | 16.10 (0.08) | NOT | ||||
| 57553.35 | 14.26 (0.05) | 13.62 (0.05) | 13.95 (0.10) | Gem | ||
| 57553.37 | 13.57 (0.03) | 13.92 (0.06) | DEM | |||
| 57554.12 | 16.23 (0.04) | 14.32 (0.04) | 13.64 (0.07) | 13.95 (0.06) | 13.55 (0.04) | LT |
| 57554.42 | 13.57 (0.03) | DEM | ||||
| 57555.24 | 14.39 (0.25) | 13.59 (0.10) | 13.91 (0.11) | REM | ||
| 57556.37 | 14.43 (0.04) | 13.67 (0.05) | 13.95 (0.10) | Gem | ||
| 57557.03 | 16.39 (0.03) | 14.44 (0.10) | 13.70 (0.07) | 13.54 (0.07) | 1.82 | |
| 57557.13 | 16.59 (0.04) | 14.45 (0.02) | 13.58 (0.04) | 13.91 (0.03) | 13.59 (0.03) | LT |
| 57557.22 | 13.62 (0.08) | 13.91 (0.12) | REM | |||
| 57557.43 | 13.64 (0.04) | 13.90 (0.05) | LCOGT | |||
| 57558.10 | 16.70 (0.04) | 14.55 (0.02) | 13.65 (0.03) | 13.98 (0.03) | 13.69 (0.04) | LT |
| 57558.23 | 13.68 (0.06) | 13.93 (0.15) | REM | |||
| MJD | u | g | r | i | z | Instrument |
|---|---|---|---|---|---|---|
| (mag) | (mag) | (mag) | (mag) | (mag) | ||
| 57558.40 | 13.68 (0.06) | 13.94 (0.11) | LCOGT | |||
| 57559.07 | 16.89 (0.05) | 14.60 (0.03) | 13.65 (0.03) | 13.95 (0.03) | 13.59 (0.03) | LT |
| 57559.24 | 13.70 (0.08) | 13.90 (0.13) | REM | |||
| 57559.44 | 13.73 (0.03) | 13.97 (0.05) | LCOGT | |||
| 57560.30 | 14.76 (0.35) | 13.74 (0.08) | 13.94 (0.11) | REM | ||
| 57560.40 | 14.00 (0.05) | LCOGT | ||||
| 57561.06 | 17.22 (0.06) | 14.72 (0.03) | 13.81 (0.06) | 14.04 (0.06) | 13.70 (0.03) | LT |
| 57561.30 | 13.75 (0.08) | 13.92 (0.14) | REM | |||
| 57562.07 | 17.26 (0.07) | 14.81 (0.10) | 13.76 (0.10) | 14.02 (0.09) | 13.48 (0.08) | 1.82 |
| 57562.11 | 17.27 (0.05) | 14.90 (0.02) | 13.72 (0.04) | 14.05 (0.03) | 13.61 (0.03) | LT |
| 57562.40 | 13.81 (0.06) | 14.00 (0.07) | LCOGT | |||
| 57563.13 | 17.47 (0.05) | 14.99 (0.03) | 13.86 (0.05) | 14.09 (0.04) | 13.90 (0.07) | LT |
| 57563.43 | 14.05 (0.05) | LCOGT | ||||
| 57566.32 | 14.00 (0.07) | 14.12 (0.11) | REM | |||
| 57566.41 | 14.01 (0.03) | 14.18 (0.05) | LCOGT | |||
| 57567.33 | 14.03 (0.06) | 14.14 (0.13) | REM | |||
| 57567.40 | 14.07 (0.03) | 14.22 (0.05) | LCOGT | |||
| 57568.15 | 17.93 (0.05) | 15.34 (0.02) | 14.04 (0.03) | 14.19 (0.03) | 13.84 (0.02) | LT |
| 57568.35 | 14.08 (0.09) | 14.16 (0.11) | REM | |||
| 57568.40 | 14.12 (0.03) | 14.24 (0.05) | LCOGT | |||
| 57569.08 | 18.05 (0.08) | 15.38 (0.01) | 14.03 (0.03) | 14.21 (0.03) | 13.90 (0.03) | LT |
| 57569.36 | 14.13 (0.07) | 14.22 (0.12) | REM | |||
| 57570.17 | 18.06 (0.05) | 15.46 (0.03) | 14.15 (0.04) | 14.28 (0.03) | 13.85 (0.03) | LT |
| 57572.98 | 14.31 (0.04) | 14.39 (0.06) | LCOGT | |||
| 57573.02 | 18.14 (0.07) | 15.67 (0.14) | 14.33 (0.11) | 14.37 (0.11) | NOT | |
| 57576.09 | 14.47 (0.04) | 14.49 (0.06) | LCOGT | |||
| 57577.10 | 18.46 (0.05) | 15.71 (0.04) | 14.54 (0.05) | 14.51 (0.03) | 14.05 (0.03) | LT |
| 57577.13 | 14.51 (0.04) | 14.53 (0.06) | LCOGT | |||
| 57578.13 | 14.56 (0.04) | 14.56 (0.06) | LCOGT | |||
| 57579.11 | 18.44 (0.06) | 15.79 (0.03) | 14.52 (0.03) | 14.63 (0.03) | 14.14 (0.03) | LT |
| 57580.06 | 14.64 (0.04) | 14.61 (0.06) | LCOGT | |||
| 57580.11 | 18.48 (0.05) | 15.88 (0.03) | 14.59 (0.04) | 14.67 (0.03) | 14.26 (0.04) | LT |
| 57581.10 | 18.48 (0.04) | 15.99 (0.03) | 14.58 (0.04) | 14.63 (0.05) | 14.13 (0.03) | LT |
| 57581.13 | 14.66 (0.04) | 14.65 (0.06) | LCOGT | |||
| 57582.13 | 14.73 (0.04) | 14.70 (0.05) | LCOGT | |||
| 57583.13 | 14.75 (0.04) | 14.72 (0.06) | LCOGT | |||
| 57584.11 | 15.98 (0.03) | 14.79 (0.04) | 14.75 (0.07) | LCOGT | ||
| 57585.29 | 14.82 (0.04) | 14.76 (0.06) | LCOGT | |||
| 57586.13 | 14.85 (0.05) | 14.77 (0.08) | LCOGT | |||
| 57586.13 | 18.61 (0.04) | 16.15 (0.04) | 14.80 (0.05) | 14.79 (0.03) | 14.31 (0.02) | LT |
| 57587.34 | 14.89 (0.04) | 14.83 (0.07) | LCOGT | |||
| 57588.13 | 18.66 (0.04) | 16.01 (0.02) | 14.93 (0.03) | 14.87 (0.02) | 14.36 (0.03) | LT |
| 57590.10 | 18.93 (0.15) | 16.14 (0.15) | 14.95 (0.13) | 14.84 (0.08) | NOT | |
| 57591.32 | 14.99 (0.06) | 14.92 (0.08) | LCOGT | |||
| 57593.07 | 15.01 (0.07) | 14.97 (0.05) | T50 | |||
| 57593.11 | 18.78 (0.05) | 16.16 (0.04) | 14.97 (0.03) | 14.98 (0.03) | 14.42 (0.03) | LT |
| 57594.05 | 15.11 (0.08) | 15.04 (0.07) | T50 | |||
| 57594.70 | 15.11 (0.04) | 15.00 (0.06) | LCOGT | |||
| 57596.01 | 18.86 (0.06) | 16.22 (0.05) | 15.05 (0.05) | 15.07 (0.03) | 14.52 (0.08) | LT |
| 57596.07 | 15.17 (0.06) | 15.06 (0.04) | T50 |
| MJD | u | g | r | i | z | Instrument |
|---|---|---|---|---|---|---|
| (mag) | (mag) | (mag) | (mag) | (mag) | ||
| 57597.07 | 15.16 (0.28) | T50 | ||||
| 57597.73 | 15.18 (0.04) | 15.07 (0.06) | LCOGT | |||
| 57598.20 | 18.80 (0.04) | 16.29 (0.03) | 15.13 (0.04) | 15.08 (0.04) | 14.46 (0.03) | LT |
| 57598.72 | 15.20 (0.04) | 15.08 (0.06) | LCOGT | |||
| 57599.70 | 15.24 (0.04) | 15.09 (0.06) | LCOGT | |||
| 57601.14 | 18.92 (0.07) | 16.40 (0.03) | 15.25 (0.04) | 15.14 (0.03) | NOT | |
| 57604.99 | 15.37 (0.04) | 15.24 (0.06) | LCOGT | |||
| 57607.06 | 15.38 (0.09) | LCOGT | ||||
| 57609.00 | 19.20 (0.09) | 16.41 (0.09) | 15.44 (0.10) | 15.29 (0.09) | 14.73 (0.15) | 1.82 |
| 57610.68 | 15.50 (0.04) | 15.29 (0.06) | LCOGT | |||
| 57612.65 | 15.52 (0.04) | 15.37 (0.06) | LCOGT | |||
| 57619.04 | 19.08 (0.14) | 16.53 (0.09) | 15.61 (0.11) | 15.59 (0.08) | NOT | |
| 57621.27 | 15.68 (0.04) | 15.46 (0.06) | LCOGT | |||
| 57623.06 | 19.41 (0.15) | 16.52 (0.12) | 15.76 (0.14) | 15.61 (0.11) | 14.93 (0.14) | 1.82 |
| 57623.29 | 15.69 (0.04) | 15.52 (0.06) | LCOGT | |||
| 57624.99 | 15.72 (0.04) | 15.58 (0.06) | LCOGT | |||
| 57625.92 | 19.14 (0.10) | 16.63 (0.08) | 15.86 (0.07) | 15.78 (0.04) | 15.10 (0.06) | 1.82 |
| 57627.00 | 15.75 (0.04) | 15.62 (0.06) | LCOGT | |||
| 57628.98 | 15.75 (0.05) | 15.59 (0.07) | LCOGT | |||
| 57636.22 | 15.91 (0.04) | 15.79 (0.06) | LCOGT | |||
| 57638.63 | 15.94 (0.04) | 15.82 (0.06) | LCOGT | |||
| 57640.24 | 15.98 (0.04) | 15.81 (0.06) | LCOGT | |||
| 57644.01 | 19.53 (0.12) | 16.91 (0.05) | 16.04 (0.05) | 15.93 (0.04) | 15.32 (0.05) | NOT |
| 57644.17 | 16.03 (0.05) | 15.86 (0.08) | LCOGT | |||
| 57650.92 | 16.14 (0.05) | 16.00 (0.07) | LCOGT | |||
| 57652.18 | 16.16 (0.04) | 16.04 (0.06) | LCOGT | |||
| 57654.83 | 16.20 (0.04) | 16.10 (0.06) | LCOGT | |||
| 57654.90 | 19.55 (0.12) | 16.92 (0.10) | 16.22 (0.11) | 16.16 (0.05) | 15.35 (0.12) | 1.82 |
| 57655.11 | 19.71 (0.07) | 17.01 (0.03) | 16.20 (0.04) | 16.04 (0.03) | 15.43 (0.04) | NOT |
| 57662.15 | 17.19 (0.06) | 16.38 (0.04) | 16.18 (0.03) | 15.58 (0.03) | NOT | |
| 57663.90 | 16.34 (0.05) | 16.31 (0.07) | LCOGT | |||
| 57665.84 | 16.34 (0.04) | 16.27 (0.06) | LCOGT | |||
| 57667.86 | 16.33 (0.04) | 16.28 (0.07) | LCOGT | |||
| 57670.08 | 16.35 (0.04) | 16.30 (0.06) | LCOGT | |||
| 57672.85 | 16.43 (0.09) | 16.34 (0.10) | LCOGT | |||
| 57680.10 | 16.55 (0.04) | 16.47 (0.06) | LCOGT | |||
| 57687.84 | 16.58 (0.04) | 16.61 (0.06) | LCOGT | |||
| 57694.82 | 16.70 (0.04) | 16.71 (0.06) | LCOGT | |||
| 57699.81 | 16.81 (0.04) | 16.85 (0.06) | LCOGT | |||
| 57704.77 | 16.81 (0.05) | 16.89 (0.07) | LCOGT | |||
| 57707.79 | 17.11 (0.05) | 16.94 (0.06) | LCOGT | |||
| 57719.17 | 17.06 (0.13) | 17.38 (0.29) | LCOGT | |||
| 57727.71 | 18.08 (0.06) | 17.30 (0.04) | 17.20 (0.09) | 17.06 (0.07) | 1.82 | |
| 57728.06 | 17.18 (0.04) | 17.26 (0.07) | LCOGT | |||
| 57728.86 | 20.89 (0.36) | 18.34 (0.14) | 17.34 (0.10) | 17.32 (0.07) | 17.27 (0.15) | 1.82 |
| 57736.06 | 17.27 (0.07) | 17.32 (0.10) | LCOGT | |||
| 57906.38 | 21.38 (0.61) | 19.57 (0.51) | 19.98 (0.53) | MMT |
| MJD | U | B | V | R | I | Instrument |
|---|---|---|---|---|---|---|
| (mag) | (mag) | (mag) | (mag) | (mag) | ||
| 57527.53 | 17.43 | ASA | ||||
| 57529.54 | 17.29 | ASA | ||||
| 57535.55 | 15.74 (0.07) | ASA | ||||
| 57535.77 | 15.86 (0.06) | 16.51 (0.15) | 15.86 (0.09) | UVOT | ||
| 57536.14 | 16.30 (0.03) | 15.51 (0.03) | NOT | |||
| 57536.36 | 16.29 (0.04) | 15.46 (0.03) | 15.10 (0.04) | 15.19 (0.07) | RK | |
| 57536.40 | 16.27 (0.10) | 15.45 (0.06) | Gem | |||
| 57537.14 | 15.88 (0.14) | 15.14 (0.09) | NOT | |||
| 57537.35 | 15.95 (0.04) | 15.11 (0.03) | 14.78 (0.04) | 14.95 (0.07) | RK | |
| 57537.41 | 15.95 (0.09) | 15.07 (0.06) | Gem | |||
| 57538.37 | 14.80 (0.03) | 14.51 (0.04) | 14.69 (0.07) | RK | ||
| 57538.39 | 15.70 (0.09) | 14.80 (0.05) | Gem | |||
| 57539.09 | 15.09 (0.05) | 15.61 (0.10) | 15.07 (0.06) | UVOT | ||
| 57539.39 | 15.49 (0.09) | 14.55 (0.05) | Gem | |||
| 57539.57 | 14.56 (0.02) | ASA | ||||
| 57539.76 | 15.42 (0.09) | 14.50 (0.08) | WHO | |||
| 57540.76 | 15.27 (0.08) | 14.28 (0.06) | WHO | |||
| 57541.21 | 14.84 (0.11) | 15.16 (0.08) | 14.08 (0.06) | NOT | ||
| 57541.36 | 15.18 (0.04) | 14.21 (0.03) | 14.01 (0.04) | 14.24 (0.06) | RK | |
| 57541.40 | 15.18 (0.09) | 14.19 (0.05) | Gem | |||
| 57541.75 | 15.14 (0.09) | 14.14 (0.07) | WHO | |||
| 57542.36 | 15.09 (0.04) | 14.07 (0.03) | 13.88 (0.04) | 14.14 (0.07) | RK | |
| 57542.38 | 15.05 (0.05) | 14.06 (0.04) | DEM | |||
| 57542.61 | 14.69 (0.06) | 15.01 (0.06) | 14.09 (0.05) | UVOT | ||
| 57543.37 | 15.00 (0.09) | 13.96 (0.06) | Gem | |||
| 57543.41 | 14.96 (0.04) | 13.93 (0.04) | DEM | |||
| 57543.97 | 14.68 (0.06) | 14.93 (0.06) | 13.94 (0.05) | UVOT | ||
| 57544.37 | 14.91 (0.09) | 13.85 (0.06) | Gem | |||
| 57544.44 | 14.90 (0.04) | 13.83 (0.04) | DEM | |||
| 57544.57 | 13.90 (0.02) | ASA | ||||
| 57545.34 | 14.86 (0.05) | 13.78 (0.04) | DEM | |||
| 57545.39 | 14.87 (0.09) | 13.76 (0.06) | Gem | |||
| 57545.94 | 14.74 (0.05) | 14.87 (0.06) | 13.81 (0.04) | UVOT | ||
| 57546.39 | 14.84 (0.09) | 13.73 (0.07) | Gem | |||
| 57546.43 | 14.84 (0.05) | 13.79 (0.05) | LCOGT | |||
| 57546.44 | 14.82 (0.04) | 13.73 (0.04) | DEM | |||
| 57547.33 | 14.83 (0.04) | 13.71 (0.04) | DEM | |||
| 57547.37 | 14.85 (0.09) | 13.72 (0.06) | Gem | |||
| 57547.47 | 14.86 (0.06) | 14.82 (0.06) | 13.73 (0.04) | UVOT | ||
| 57549.31 | 14.98 (0.06) | 14.85 (0.06) | 13.71 (0.05) | UVOT | ||
| 57549.43 | 14.85 (0.06) | 13.71 (0.03) | LCOGT | |||
| 57549.50 | 13.76 (0.02) | ASA | ||||
| 57550.41 | 14.89 (0.06) | 13.74 (0.03) | LCOGT | |||
| 57550.58 | 15.04 (0.06) | 14.85 (0.06) | 13.62 (0.04) | UVOT | ||
| 57551.42 | 14.89 (0.04) | 13.68 (0.04) | DEM | |||
| 57552.18 | 14.88 (0.11) | 13.61 (0.14) | NOT | |||
| 57552.35 | 14.96 (0.09) | 13.72 (0.05) | Gem | |||
| 57552.40 | 15.14 (0.06) | 14.94 (0.06) | 13.69 (0.05) | UVOT | ||
| 57553.19 | 14.98 (0.07) | 13.73 (0.07) | NOT | |||
| 57553.35 | 15.01 (0.09) | 13.75 (0.05) | Gem | |||
| MJD | U | B | V | R | I | Instrument |
|---|---|---|---|---|---|---|
| (mag) | (mag) | (mag) | (mag) | (mag) | ||
| 57553.37 | 14.99 (0.04) | 13.74 (0.04) | DEM | |||
| 57554.20 | 15.45 (0.06) | 15.05 (0.06) | 13.73 (0.05) | UVOT | ||
| 57554.30 | 15.09 (0.05) | 13.77 (0.04) | 13.47 (0.05) | 13.68 (0.08) | RK | |
| 57554.42 | 15.05 (0.04) | 13.76 (0.04) | DEM | |||
| 57555.34 | 15.12 (0.04) | 13.82 (0.03) | 13.46 (0.05) | 13.63 (0.07) | RK | |
| 57555.56 | 15.55 (0.06) | 15.07 (0.06) | 13.78 (0.04) | UVOT | ||
| 57556.37 | 15.18 (0.10) | 13.87 (0.06) | Gem | |||
| 57557.03 | 15.06 (0.08) | 13.89 (0.05) | 1.82 | |||
| 57557.34 | 15.28 (0.10) | 13.99 (0.15) | 13.52 (0.12) | 13.60 (0.16) | JB | |
| 57557.43 | 15.29 (0.06) | 13.89 (0.04) | LCOGT | |||
| 57557.75 | 15.88 (0.07) | 15.32 (0.07) | 13.90 (0.05) | UVOT | ||
| 57558.40 | 15.38 (0.08) | 13.98 (0.09) | LCOGT | |||
| 57558.45 | 13.97 (0.02) | ASA | ||||
| 57559.44 | 15.51 (0.06) | 14.03 (0.03) | LCOGT | |||
| 57560.57 | 16.24 (0.07) | 15.62 (0.08) | 14.08 (0.05) | UVOT | ||
| 57561.52 | 14.16 (0.03) | ASA | ||||
| 57562.06 | 15.77 (0.11) | 14.28 (0.11) | 1.82 | |||
| 57562.40 | 15.78 (0.09) | 14.21 (0.05) | LCOGT | |||
| 57563.43 | 15.85 (0.06) | 14.25 (0.04) | LCOGT | |||
| 57566.23 | 16.90 (0.09) | 16.07 (0.10) | 14.49 (0.05) | UVOT | ||
| 57566.33 | 16.05 (0.04) | 14.46 (0.04) | 13.83 (0.04) | 13.89 (0.07) | RK | |
| 57566.41 | 16.11 (0.06) | 14.47 (0.03) | LCOGT | |||
| 57567.40 | 16.19 (0.06) | 14.55 (0.03) | LCOGT | |||
| 57568.40 | 16.25 (0.07) | 14.60 (0.03) | LCOGT | |||
| 57568.53 | 14.64 (0.02) | ASA | ||||
| 57569.38 | 16.29 (0.10) | 14.55 (0.13) | 13.97 (0.13) | 13.81 (0.17) | JB | |
| 57569.42 | 16.18 (0.04) | 14.65 (0.02) | GS | |||
| 57570.43 | 14.77 (0.03) | ASA | ||||
| 57572.28 | 16.39 (0.05) | 14.79 (0.03) | 14.08 (0.04) | 14.05 (0.07) | RK | |
| 57572.98 | 14.83 (0.04) | LCOGT | ||||
| 57572.98 | 17.45 (0.16) | 16.45 (0.12) | 14.92 (0.07) | UVOT | ||
| 57573.02 | 16.46 (0.13) | 14.81 (0.14) | NOT | |||
| 57573.35 | 16.55 (0.08) | 14.80 (0.12) | 14.16 (0.12) | 14.03 (0.16) | JB | |
| 57574.35 | 16.44 (0.05) | 14.90 (0.03) | GS | |||
| 57574.52 | 14.92 (0.03) | ASA | ||||
| 57575.29 | 16.50 (0.06) | 14.92 (0.13) | 14.22 (0.22) | 14.14 (0.16) | RK | |
| 57575.44 | 16.67 (0.13) | 14.91 (0.14) | 14.25 (0.13) | 14.09 (0.19) | JB | |
| 57576.09 | 16.69 (0.08) | 15.00 (0.04) | LCOGT | |||
| 57576.77 | 17.58 (0.14) | 16.48 (0.12) | 15.04 (0.06) | UVOT | ||
| 57577.13 | 15.04 (0.04) | LCOGT | ||||
| 57577.54 | 15.09 (0.03) | ASA | ||||
| 57578.13 | 15.07 (0.04) | LCOGT | ||||
| 57578.73 | 17.72 (0.15) | 16.65 (0.13) | 15.19 (0.06) | UVOT | ||
| 57579.14 | 15.09 (0.04) | LCOGT | ||||
| 57580.06 | 15.17 (0.04) | LCOGT | ||||
| 57580.33 | 16.69 (0.09) | 15.12 (0.13) | 14.40 (0.12) | 14.18 (0.17) | JB | |
| 57580.50 | 15.23 (0.03) | ASA | ||||
| 57581.13 | 16.80 (0.07) | 15.19 (0.04) | LCOGT |
| MJD | U | B | V | R | I | Instrument |
|---|---|---|---|---|---|---|
| (mag) | (mag) | (mag) | (mag) | (mag) | ||
| 57581.30 | 17.59 (0.14) | 16.74 (0.14) | 15.20 (0.06) | UVOT | ||
| 57582.13 | 16.85 (0.07) | 15.24 (0.04) | LCOGT | |||
| 57582.34 | 16.77 (0.10) | 15.22 (0.13) | 14.49 (0.13) | 14.28 (0.17) | JB | |
| 57583.13 | 15.28 (0.04) | LCOGT | ||||
| 57583.27 | 16.66 (0.06) | 15.24 (0.06) | 14.47 (0.25) | 14.25 (0.15) | RK | |
| 57583.42 | 15.38 (0.04) | ASA | ||||
| 57583.45 | 16.70 (0.04) | 15.25 (0.03) | GS | |||
| 57584.11 | 15.28 (0.04) | LCOGT | ||||
| 57585.29 | 16.84 (0.06) | 15.34 (0.04) | LCOGT | |||
| 57586.13 | 15.42 (0.06) | LCOGT | ||||
| 57586.57 | 17.90 (0.16) | 16.84 (0.16) | 15.41 (0.06) | UVOT | ||
| 57587.34 | 16.80 (0.11) | 15.40 (0.06) | LCOGT | |||
| 57587.41 | 15.38 (0.06) | ASA | ||||
| 57587.42 | 16.73 (0.05) | 15.39 (0.03) | GS | |||
| 57589.39 | 16.88 (0.06) | 15.42 (0.04) | GS | |||
| 57590.10 | 16.86 (0.09) | 15.37 (0.09) | NOT | |||
| 57590.15 | 17.77 (0.14) | 16.90 (0.17) | 15.53 (0.07) | UVOT | ||
| 57591.32 | 16.80 (0.09) | 15.49 (0.06) | LCOGT | |||
| 57591.41 | 15.47 (0.03) | GS | ||||
| 57593.07 | 16.82 (0.07) | 15.55 (0.05) | T50 | |||
| 57594.05 | 16.92 (0.06) | 15.61 (0.10) | T50 | |||
| 57594.33 | 16.90 (0.06) | 15.49 (0.14) | 14.83 (0.14) | 14.63 (0.17) | JB | |
| 57594.54 | 17.83 (0.15) | 16.95 (0.17) | 15.63 (0.07) | UVOT | ||
| 57594.70 | 17.01 (0.08) | 15.53 (0.04) | LCOGT | |||
| 57595.46 | 15.65 (0.05) | ASA | ||||
| 57596.07 | 16.82 (0.15) | 15.49 (0.13) | T50 | |||
| 57597.06 | 16.95 (0.06) | 15.57 (0.08) | T50 | |||
| 57597.29 | 17.11 (0.08) | 15.56 (0.12) | 14.87 (0.13) | 14.69 (0.17) | JB | |
| 57597.41 | 15.65 (0.04) | ASA | ||||
| 57597.73 | 15.61 (0.04) | LCOGT | ||||
| 57598.26 | 17.07 (0.09) | 15.57 (0.13) | 14.88 (0.13) | 14.69 (0.17) | JB | |
| 57598.72 | 16.86 (0.06) | 15.67 (0.04) | LCOGT | |||
| 57598.77 | 16.91 (0.16) | 15.71 (0.10) | UVOT | |||
| 57599.70 | 17.00 (0.07) | 15.65 (0.04) | LCOGT | |||
| 57600.24 | 17.11 (0.06) | 15.66 (0.11) | 14.95 (0.10) | 14.76 (0.15) | JB | |
| 57601.13 | 17.07 (0.07) | 15.66 (0.04) | NOT | |||
| 57601.44 | 15.77 (0.04) | ASA | ||||
| 57603.62 | 18.24 (0.26) | 17.11 (0.20) | 15.83 (0.08) | UVOT | ||
| 57604.31 | 17.12 (0.04) | 15.68 (0.09) | 15.15 (0.09) | 14.83 (0.14) | JB | |
| 57604.53 | 15.75 (0.04) | ASA | ||||
| 57604.99 | 15.82 (0.04) | LCOGT | ||||
| 57606.84 | 17.11 (0.18) | 15.90 (0.10) | UVOT | |||
| 57607.06 | 15.74 (0.12) | LCOGT | ||||
| 57607.50 | 15.85 (0.05) | ASA | ||||
| 57608.47 | 17.11 (0.18) | 15.95 (0.10) | UVOT | |||
| 57609.00 | 16.95 (0.09) | 15.84 (0.09) | 1.82 | |||
| 57609.24 | 17.12 (0.08) | 15.71 (0.15) | 15.19 (0.18) | 14.80 (0.13) | RK | |
| 57610.35 | 15.91 (0.02) | GS | ||||
| 57610.37 | 15.80 (0.05) | ASA | ||||
| 57610.68 | 15.88 (0.04) | LCOGT |
| MJD | U | B | V | R | I | Instrument |
|---|---|---|---|---|---|---|
| (mag) | (mag) | (mag) | (mag) | (mag) | ||
| 57611.53 | 15.97 (0.05) | ASA | ||||
| 57612.40 | 17.16 (0.05) | 15.89 (0.01) | GS | |||
| 57612.65 | 15.91 (0.04) | LCOGT | ||||
| 57613.20 | 17.17 (0.06) | 15.78 (0.11) | 15.24 (0.24) | 14.90 (0.18) | RK | |
| 57613.31 | 15.90 (0.06) | ASA | ||||
| 57613.51 | 17.96 (0.21) | 17.26 (0.20) | 15.94 (0.10) | UVOT | ||
| 57614.36 | 17.07 (0.05) | 15.91 (0.03) | GS | |||
| 57614.56 | 15.87 (0.05) | ASA | ||||
| 57615.28 | 16.09 (0.10) | ASA | ||||
| 57615.74 | 18.29 (0.22) | 17.27 (0.21) | 15.97 (0.09) | UVOT | ||
| 57618.48 | 15.97 (0.12) | ASA | ||||
| 57619.04 | 17.21 (0.07) | 16.13 (0.07) | NOT | |||
| 57621.27 | 17.12 (0.07) | 16.03 (0.04) | LCOGT | |||
| 57623.05 | 17.23 (0.09) | 16.02 (0.12) | 1.82 | |||
| 57623.29 | 16.09 (0.04) | LCOGT | ||||
| 57624.99 | 17.24 (0.07) | 16.09 (0.04) | LCOGT | |||
| 57625.92 | 17.02 (0.09) | 16.14 (0.06) | 1.82 | |||
| 57626.53 | 16.07 (0.06) | ASA | ||||
| 57627.00 | 16.12 (0.04) | LCOGT | ||||
| 57627.28 | 17.30 (0.21) | 16.20 (0.10) | UVOT | |||
| 57628.98 | 16.23 (0.06) | LCOGT | ||||
| 57629.64 | 18.34 (0.31) | 17.55 (0.26) | 16.24 (0.11) | UVOT | ||
| 57630.48 | 16.33 (0.07) | ASA | ||||
| 57632.00 | 17.12 (0.19) | 16.36 (0.15) | UVOT | |||
| 57634.24 | 17.26 (0.17) | 16.10 (0.11) | 15.54 (0.13) | 15.31 (0.07) | RK | |
| 57635.08 | 16.36 (0.08) | ASA | ||||
| 57636.08 | 16.25 (0.09) | ASA | ||||
| 57636.22 | 16.28 (0.04) | LCOGT | ||||
| 57636.28 | 18.40 (0.24) | 17.47 (0.24) | 16.38 (0.11) | UVOT | ||
| 57637.50 | 16.36 (0.07) | ASA | ||||
| 57638.63 | 17.33 (0.07) | 16.30 (0.04) | LCOGT | |||
| 57639.40 | 16.35 (0.06) | ASA | ||||
| 57640.24 | 16.35 (0.04) | LCOGT | ||||
| 57642.16 | 16.29 (0.14) | ASA | ||||
| 57643.52 | 18.10 (0.18) | 17.52 (0.26) | 16.57 (0.12) | UVOT | ||
| 57644.00 | 17.58 (0.06) | 16.45 (0.05) | NOT | |||
| 57644.17 | 17.11 (0.11) | 16.36 (0.06) | LCOGT | |||
| 57650.36 | UVOT | |||||
| 57650.41 | 16.68 (0.13) | ASA | ||||
| 57650.92 | 16.53 (0.06) | LCOGT | ||||
| 57652.18 | 17.63 (0.85) | 16.55 (0.04) | LCOGT | |||
| 57654.83 | 17.63 (0.09) | 16.60 (0.04) | LCOGT | |||
| 57654.90 | 17.32 (0.10) | 16.53 (0.06) | 1.82 | |||
| 57655.04 | 16.61 (0.10) | ASA | ||||
| 57655.11 | 17.63 (0.04) | 16.50 (0.03) | NOT | |||
| 57656.22 | 17.49 (0.10) | 16.89 (0.14) | 15.94 (0.20) | 15.65 (0.13) | RK | |
| 57657.35 | 16.68 (0.07) | ASA | ||||
| 57657.96 | 18.66 (0.50) | 17.56 (0.26) | 16.87 (0.21) | UVOT | ||
| 57660.11 | 16.62 (0.10) | ASA | ||||
| 57660.83 | 17.79 (0.31) | 16.80 (0.15) | UVOT |
| MJD | U | B | V | R | I | Instrument |
|---|---|---|---|---|---|---|
| (mag) | (mag) | (mag) | (mag) | (mag) | ||
| 57662.15 | 17.73 (0.08) | 16.70 (0.03) | NOT | |||
| 57662.69 | 18.81 (0.31) | 17.84 (0.33) | 16.93 (0.15) | UVOT | ||
| 57663.90 | 16.75 (0.06) | LCOGT | ||||
| 57665.84 | 17.96 (0.09) | 16.77 (0.04) | LCOGT | |||
| 57667.42 | 16.80 (0.11) | ASA | ||||
| 57667.86 | 17.85 (0.10) | 16.75 (0.05) | LCOGT | |||
| 57668.33 | 17.00 (0.10) | ASA | ||||
| 57670.08 | 17.81 (0.07) | 16.81 (0.04) | LCOGT | |||
| 57671.29 | 16.96 (0.18) | ASA | ||||
| 57671.53 | 18.66 (0.29) | 17.93 (0.35) | 17.15 (0.19) | UVOT | ||
| 57672.85 | 17.76 (0.21) | 16.95 (0.13) | LCOGT | |||
| 57675.22 | 16.90 (0.20) | ASA | ||||
| 57678.36 | 17.25 (0.27) | ASA | ||||
| 57680.10 | 17.94 (0.09) | 16.98 (0.05) | LCOGT | |||
| 57680.26 | 17.10 (0.10) | ASA | ||||
| 57681.37 | 18.81 (0.29) | 18.14 (0.43) | 17.13 (0.17) | UVOT | ||
| 57687.36 | 17.17 (0.14) | ASA | ||||
| 57687.84 | 18.03 (0.07) | 17.09 (0.04) | LCOGT | |||
| 57690.35 | 17.03 (0.09) | ASA | ||||
| 57691.39 | 19.35 (0.45) | 18.36 (0.53) | 17.41 (0.21) | UVOT | ||
| 57692.26 | 16.96 (0.10) | ASA | ||||
| 57694.82 | 18.14 (0.08) | 17.20 (0.05) | LCOGT | |||
| 57695.34 | 17.39 (0.15) | ASA | ||||
| 57697.33 | 17.11 (0.12) | ASA | ||||
| 57699.81 | 18.32 (0.08) | 17.36 (0.05) | LCOGT | |||
| 57702.25 | 17.61 (0.23) | ASA | ||||
| 57702.88 | 18.57 (0.62) | 17.52 (0.23) | UVOT | |||
| 57704.77 | 18.43 (0.16) | 17.30 (0.08) | LCOGT | |||
| 57707.21 | 17.78 (0.33) | ASA | ||||
| 57707.79 | 18.66 (0.09) | 17.73 (0.06) | LCOGT | |||
| 57710.21 | 17.35 (0.12) | ASA | ||||
| 57711.22 | 18.93 (0.34) | 18.58 (0.61) | 17.69 (0.27) | UVOT | ||
| 57715.05 | 17.60 (0.23) | ASA | ||||
| 57718.26 | 18.04 (0.27) | ASA | ||||
| 57719.17 | 17.59 (0.77) | LCOGT | ||||
| 57721.26 | 18.15 (0.27) | ASA | ||||
| 57723.42 | 19.26 (0.45) | 18.98 (0.60) | 17.98 (0.60) | UVOT | ||
| 57727.71 | 18.77 (0.06) | 17.71 (0.07) | 1.82 | |||
| 57728.06 | 18.68 (0.09) | 17.87 (0.06) | LCOGT | |||
| 57728.85 | 18.60 (0.10) | 17.81 (0.10) | 1.82 | |||
| 57730.81 | 18.93 (0.81) | 18.02 (0.36) | UVOT | |||
| 57736.06 | 18.94 (0.18) | 18.00 (0.11) | LCOGT | |||
| 57737.19 | 17.45 (0.34) | ASA | ||||
| 57851.63 | 18.17 | ASA | ||||
| 57860.49 | 19.69 | 19.89 | 18.99 | UVOT | ||
| 57870.60 | 18.40 | ASA | ||||
| 57876.58 | 18.29 | ASA | ||||
| 57880.57 | 17.80 | ASA | ||||
| 57885.55 | 17.65 | ASA | ||||
| 57893.59 | 18.55 | ASA |
| MJD | J | H | K | Instrument |
|---|---|---|---|---|
| (mag) | (mag) | (mag) | ||
| 57540.17 | 13.78 (0.27) | LT | ||
| 57542.21 | 13.55 (0.30) | LT | ||
| 57546.29 | 13.33 (0.03) | 13.21 (0.02) | 13.14 (0.03) | REM |
| 57547.37 | 13.30 (0.02) | 13.12 (0.02) | 13.00 (0.04) | REM |
| 57548.38 | 13.26 (0.04) | 13.08 (0.02) | 12.94 (0.04) | REM |
| 57549.42 | 13.25 (0.04) | 13.09 (0.02) | 12.98 (0.06) | REM |
| 57550.44 | 13.12 (0.03) | 13.00 (0.02) | 12.86 (0.05) | REM |
| 57551.14 | 13.09 (0.35) | 12.97 (0.31) | 12.95 (0.33) | NOT |
| 57551.19 | 13.03 (0.27) | LT | ||
| 57552.06 | 13.01 (0.25) | LT | ||
| 57553.17 | 12.94 (0.29) | LT | ||
| 57554.12 | 12.96 (0.26) | LT | ||
| 57554.23 | 13.12 (0.06) | 12.91 (0.03) | 12.77 (0.05) | REM |
| 57555.24 | 13.01 (0.01) | 12.88 (0.02) | REM | |
| 57557.13 | 12.86 (0.25) | LT | ||
| 57557.22 | 13.04 (0.03) | 12.93 (0.02) | 12.74 (0.09) | REM |
| 57558.10 | 12.86 (0.29) | LT | ||
| 57558.23 | 13.02 (0.06) | 12.89 (0.03) | 12.79 (0.12) | REM |
| 57559.07 | 12.82 (0.30) | LT | ||
| 57559.24 | 13.01 (0.01) | 12.86 (0.02) | 12.69 (0.02) | REM |
| 57560.30 | 13.04 (0.05) | 12.88 (0.02) | 12.76 (0.09) | REM |
| 57561.06 | 12.91 (0.23) | LT | ||
| 57561.30 | 13.01 (0.03) | 12.85 (0.02) | 12.69 (0.03) | REM |
| 57562.12 | 12.84 (0.25) | LT | ||
| 57562.31 | 13.14 (0.05) | 12.96 (0.04) | REM | |
| 57563.13 | 12.90 (0.32) | LT | ||
| 57566.32 | 13.14 (0.04) | 13.01 (0.02) | 12.79 (0.07) | REM |
| 57567.33 | 13.13 (0.03) | 12.94 (0.02) | 12.78 (0.04) | REM |
| 57568.35 | 13.23 (0.05) | 13.00 (0.02) | 12.84 (0.10) | REM |
| 57569.08 | 13.06 (0.20) | LT | ||
| 57569.36 | 13.19 (0.03) | 13.00 (0.03) | REM | |
| 57570.17 | 13.03 (0.26) | LT | ||
| 57575.35 | 13.45 (0.02) | 13.22 (0.02) | 13.03 (0.04) | REM |
| 57577.10 | 13.25 (0.24) | LT | ||
| 57579.11 | 13.34 (0.20) | LT | ||
| 57580.12 | 13.28 (0.30) | LT | ||
| 57581.10 | 13.34 (0.27) | LT | ||
| 57583.34 | 13.78 (0.05) | 13.43 (0.02) | 13.22 (0.06) | REM |
| 57586.13 | 13.47 (0.29) | LT | ||
| 57587.43 | 13.92 (0.04) | 13.54 (0.03) | 13.43 (0.05) | REM |
| 57588.14 | 13.58 (0.23) | LT | ||
| 57591.43 | 14.14 (0.04) | 13.68 (0.03) | 13.44 (0.06) | REM |
| 57593.12 | 13.71 (0.23) | LT | ||
| 57596.31 | 14.23 (0.04) | 13.79 (0.03) | REM | |
| 57600.32 | 14.55 (0.10) | 13.87 (0.05) | REM | |
| 57604.32 | 14.55 (0.06) | REM | ||
| 57608.36 | 14.70 (0.07) | 14.23 (0.04) | 13.92 (0.11) | REM |
| 57612.38 | 14.80 (0.05) | 14.21 (0.03) | 14.01 (0.14) | REM |
| 57617.22 | 14.98 (0.06) | 14.37 (0.04) | 14.15 (0.11) | REM |
| 57622.36 | 15.28 (0.05) | 14.57 (0.05) | 14.44 (0.20) | REM |
| MJD | J | H | K | Instrument |
|---|---|---|---|---|
| (mag) | (mag) | (mag) | ||
| 57623.15 | 15.11 (0.40) | 14.69 (0.34) | 14.19 (0.39) | NOT |
| 57629.11 | 15.47 (0.06) | 14.72 (0.07) | 14.70 (0.17) | REM |
| 57634.96 | 14.80 (0.28) | LT | ||
| 57636.95 | 14.82 (0.30) | LT | ||
| 57638.94 | 14.89 (0.28) | LT | ||
| 57642.93 | 15.02 (0.28) | LT | ||
| 57650.92 | 15.17 (0.29) | LT | ||
| 57654.96 | 15.32 (0.25) | LT | ||
| 57657.92 | 15.42 (0.23) | LT | ||
| 57663.93 | 15.58 (0.26) | LT | ||
| 57666.87 | 15.58 (0.22) | LT | ||
| 57669.88 | 15.64 (0.31) | LT | ||
| 57672.86 | 15.69 (0.30) | LT | ||
| 57675.84 | 15.70 (0.28) | LT | ||
| 57678.87 | 15.87 (0.30) | LT | ||
| 57681.88 | 15.87 (0.28) | LT | ||
| 57689.87 | 15.97 (0.27) | LT | ||
| 57693.83 | 16.02 (0.23) | LT | ||
| 57700.84 | 16.15 (0.26) | LT | ||
| 57708.86 | 16.38 (0.26) | LT | ||
| 57711.85 | 16.33 (0.27) | LT | ||
| 57732.87 | 16.71 (0.26) | LT | ||
| 57856.24 | 18.56 (0.35) | LT | ||
| 57863.21 | 17.65 | LT | ||
| 57866.22 | 18.61 (0.35) | LT |
| MJD | UV-W2 | UV-M2 | UV-W1 | Instrument |
|---|---|---|---|---|
| (mag) | (mag) | (mag) | ||
| 57535.77 | 17.74 (0.26) | 17.71 (0.22) | 16.74 (0.17) | UVOT |
| 57539.09 | 17.11 (0.21) | 17.06 (0.14) | 16.07 (0.13) | UVOT |
| 57542.61 | 17.01 (0.16) | 17.26 (0.16) | 15.88 (0.10) | UVOT |
| 57543.98 | 17.02 (0.16) | 17.50 (0.18) | 15.98 (0.11) | UVOT |
| 57545.94 | 17.25 (0.19) | 17.58 (0.20) | 16.08 (0.11) | UVOT |
| 57547.47 | 17.31 (0.19) | 17.84 (0.23) | 16.28 (0.12) | UVOT |
| 57549.32 | 17.37 (0.19) | 18.13 (0.29) | 16.45 (0.14) | UVOT |
| 57550.58 | 17.43 (0.21) | 18.04 (0.27) | 16.45 (0.14) | UVOT |
| 57552.40 | 17.75 (0.25) | 18.46 (0.37) | 16.49 (0.14) | UVOT |
| 57554.20 | 17.81 (0.26) | 18.39 (0.35) | 16.78 (0.17) | UVOT |
| 57555.56 | 17.91 (0.28) | 18.38 (0.38) | 17.04 (0.20) | UVOT |
| 57557.75 | 18.20 (0.34) | 17.20 (0.22) | UVOT | |
| 57560.58 | 18.37 (0.40) | 19.33 (0.76) | 17.47 (0.27) | UVOT |
| 57569.56 | 19.09 (0.69) | 18.74 (0.74) | UVOT | |
| 57579.06 | 19.50 | 19.22 | 18.85 | UVOT |
| 57588.37 | 19.67 | 18.91 | UVOT | |
| 57592.35 | 19.70 | UVOT | ||
| 57596.65 | 19.18 | 18.87 | UVOT | |
| 57603.62 | 19.59 | 19.52 | 19.18 | UVOT |
| 57612.13 | 19.83 | 19.53 | 18.93 | UVOT |
| 57619.20 | 19.23 | UVOT | ||
| 57631.56 | 19.75 | 19.81 | 19.32 | UVOT |
| 57646.94 | 19.88 | 19.73 | 19.31 | UVOT |
| 57659.40 | 19.85 | 19.81 | 19.28 | UVOT |
| 57668.01 | 19.85 | 19.80 | 19.35 | UVOT |
| 57681.37 | 20.10 | 19.94 | 19.56 | UVOT |
| 57691.39 | 20.14 | 19.98 | 19.62 | UVOT |
| 57707.04 | 20.11 | 19.90 | 19.54 | UVOT |
| 57726.19 | 19.90 | 19.89 | 19.43 | UVOT |
| 57860.49 | 20.29 | 20.08 | 19.76 | UVOT |
| Band | MJD max | Phase max [d] | Mag max | |
|---|---|---|---|---|
| (from disc.) | (from expl.) | |||
| UV-W2 | ||||
| UV-M2 | ||||
| UV-W1 | ||||
| u | ||||
| U | ||||
| B | ||||
| g | ||||
| V | ||||
| r | ||||
| R | ||||
| i | ||||
| I | ||||
| z | ||||
| J | ||||
| H | ||||
| K | ||||
| Telescope | Instrument | Grism/Grating | Slit | Resolution [R] | Wavelength range | ||
|---|---|---|---|---|---|---|---|
| \rowcolorgray!20 1.22m Galileo | B&C spectrograph | 300 ln/mm | 3.93″ | 636 | 3800 | 8000 Å | |
| Gr#4 | 363 | 3360 | 7740 Å | ||||
| VPH6 | 300 | 4500 | 10000 Å | ||||
| 1.82m Copernico | AFOSC | VPH7 | 1.69″ | 375 | 3200 | 7300 Å | |
| \rowcolorgray!20 du Pont Telescope | B&C spectrograph | 300 ln/mm | 2.71″ | 1667 | 3300 | 9500 Å | |
| Red | 2300 | 5500 | 10500 Å | ||||
| Large Binocular Telescope (LBT) | MODS | Blue | 0.6″ | 1850 | 3200 | 6000 Å | |
| \rowcolorgray!20 Magellan | IMACS | 300 ln/mm | 0.9″ | 1100 | 3650 | 9740 Å | |
| VPH-Blue | 1.2″ | 1600 | 3900 | 6800 Å | |||
| 1.0″ | 1600 | 3920 | 9050 Å | ||||
| MDM Hiltner 2.4 m | OSMOS | VPH-Red | 1.2″ | 1500 | 5350 | 10500 Å | |
| \rowcolorgray!20 Multiple Mirror Telescope (MMT) | Blue Channel | 300 ln/mm | 1.0″ | 750 | 3300 | 8600 Å | |
| LT | SPRAT | Blue | 1.8″ | 350 | 4000 | 8000 Å | |
| \rowcolorgray!20NOT | ALFOSC | Gr#4 | 1.0″ | 360 | 3200 | 9600 Å | |
| Tillinghast 1.5m (FLWO) | FAST | 300 ln/mm | 3.0″ | 900 | 3530 | 7470 Å | |
| \rowcolorgray!20 | LR-B | 585 | 3000 | 8430 Å | |||
| \rowcolorgray!20TNG | DOLORES | LR-R | 1.0″ | 714 | 4470 | 10070 Å | |
| Date obs. | MJD | Tel.+Inst. | Slit | Grism/Grating |
|---|---|---|---|---|
| 20160528 | 57536.2 | NOT+ALFOSC | 1.0″ | Gr#4 |
| 20160528 | 57536.2 | LT+SPRAT | 1.8″ | Blue |
| 20160529 | 57537.2 | LT+SPRAT | 1.8″ | Blue |
| 20160529 | 57537.1 | NOT+ALFOSC | 1.0″ | Gr#4 |
| 20160531 | 57539.4 | MDM+OSMOS | 1.2″ | VPH-Blue |
| 20160601 | 57540.1 | LT+SPRAT | 1.8″ | Blue |
| 20160602 | 57541.4 | Till+FAST | 3.0″ | 300 ln/mm |
| 20160602 | 57541.4 | MDM+OSMOS | 1.2″ | VPH-Blue |
| 20160603 | 57542.5 | Till+FAST | 3.0″ | 300 ln/mm |
| 20160604 | 57543.4 | Till+FAST | 3.0″ | 300 ln/mm |
| 20160605 | 57544.5 | Till+FAST | 3.0″ | 300 ln/mm |
| 20160606 | 57545.4 | Till+FAST | 3.0″ | 300 ln/mm |
| 20160607 | 57546.2 | NOT+ALFOSC | 1.0″ | Gr#4 |
| 20160608 | 57547.4 | Till+FAST | 3.0″ | 300 ln/mm |
| 20160609 | 57548.5 | Till+FAST | 3.0″ | 300 ln/mm |
| 20160610 | 57549.2 | LT+SPRAT | 1.8″ | Blue |
| 20160612 | 57551.2 | LT+SPRAT | 1.8″ | Blue |
| 20160613 | 57552.2 | NOT+ALFOSC | 1.0″ | Gr#4 |
| 20160614 | 57553.1 | LT+SPRAT | 1.8″ | Blue |
| 20160614 | 57553.4 | LBT+MODS | 0.6″ | Red+Blue |
| 20160615 | 57554.1 | LT+SPRAT | 1.8″ | Blue |
| 20160618 | 57557.0 | 1.82+AFOSC | 1.69″ | VHP6+VPH7 |
| 20160619 | 57558.1 | LT+SPRAT | 1.8″ | Blue |
| 20160622 | 57561.1 | LT+SPRAT | 1.8″ | Blue |
| 20160623 | 57562.0 | 1.82+AFOSC | 1.69″ | VHP6+VPH7 |
| 20160623 | 57562.1 | LT+SPRAT | 1.8″ | Blue |
| 20160624 | 57563.1 | LT+SPRAT | 1.8″ | Blue |
| 20160626 | 57565.0 | LT+SPRAT | 1.8″ | Blue |
| 20160702 | 57571.2 | LT+SPRAT | 1.8″ | Blue |
| 20160705 | 57574.4 | Till+FAST | 3.0″ | 300 ln/mm |
| 20160707 | 57576.1 | 1.22+B&C | 3.93″ | 300 ln/mm |
| 20160710 | 57579.4 | Till+FAST | 3.0″ | 300 ln/mm |
| 20160710 | 57579.3 | MMT+Blue Channel | 1.0″ | 300 ln/mm |
| 20160712 | 57581.1 | LT+SPRAT | 1.8″ | Blue |
| 20160717 | 57586.1 | LT+SPRAT | 1.8″ | Blue |
| 20160718 | 57587.0 | LT+SPRAT | 1.8″ | Blue |
| 20160721 | 57590.1 | NOT+ALFOSC | 1.0″ | Gr#4 |
| 20160726 | 57596.0 | LT+SPRAT | 1.8″ | Blue |
| 20160801 | 57601.1 | NOT+ALFOSC | 1.0″ | Gr#4 |
| 20160809 | 57609.0 | 1.82+AFOSC | 1.69″ | VHP6+VPH7 |
| 20160812 | 57613.0 | TNG+LRS | 1.0″ | LR-B+LT-R |
| 20160822 | 57623.0 | 1.82+AFOSC | 1.69″ | VHP6+VPH7 |
| 20160824 | 57624.0 | LT+SPRAT | 1.8″ | Blue |
| 20160825 | 57625.9 | 1.82+AFOSC | 1.69″ | VHP6+Gr#4 |
| 20160903 | 57634.8 | 1.82+AFOSC | 1.69″ | VHP6+VPH7 |
| 20160903 | 57635.0 | LT+SPRAT | 1.8″ | Blue |
| 20160908 | 57639.1 | du Pont+B&C | 2.71″ | 300 ln/mm |
| 20160916 | 57647.9 | LT+SPRAT | 1.8″ | Blue |
| 20160923 | 57654.9 | 1.82+AFOSC | 1.69″ | VHP6+VPH7 |
| Date obs. | MJD | Tel.+Inst. | Slit | Grism/Grating |
|---|---|---|---|---|
| 20160924 | 57655.1 | NOT+ALFOSC | 1.0″ | Gr#4 |
| 20160930 | 57662.0 | LT+SPRAT | 1.8″ | Blue |
| 20161001 | 57662.1 | NOT+ALFOSC | 1.0″ | Gr#4 |
| 20161011 | 57672.9 | LT+SPRAT | 1.8″ | Blue |
| 20161013 | 57674.8 | LT+SPRAT | 1.8″ | Blue |
| 20161102 | 57694.1 | LBT+MODS | 0.6″ | Red+Blue |
| 20161101 | 57693.9 | LT+SPRAT | 1.8″ | Blue |
| 20161115 | 57707.8 | MDM+OSMOS | 1.2″ | VPH-Red |
| 20161118 | 57710.8 | LT+SPRAT | 1.8″ | Blue |
| 20161205 | 57727.7 | 1.82+AFOSC | 1.69″ | VHP6+VPH7 |
| 20161206 | 57728.8 | 1.82+AFOSC | 1.69″ | VHP6+VPH7 |
| 20161210 | 57732.8 | LT+SPRAT | 1.8″ | Blue |
| 20170617 | 57921.8 | MDM+OSMOS | 1.0″ | VPH-Red |
| 20170628 | 57932.4 | MMT+Blue Channel | 1.0″ | 300 ln/mm |
| 20170720 | 57954.2 | Magellan+IMACS | 0.9″ | 300ln/mm |
| Start Date | Time since First Light | Frequency | Flux Density | Project | |
|---|---|---|---|---|---|
| (UT) | (days) | (GHz) | (GHz) | (mJy) | |
| 2016-06-03 | 11 | 5.95 | 2.048 | 16A-477 | |
| 2016-06-03 | 11 | 9.80 | 2.048 | 16A-477 | |
| 2016-06-03 | 11 | 14.75 | 2.048 | 16A-477 | |
| 2016-06-03 | 11 | 21.85 | 2.048 | 16A-477 | |
| 2016-06-13 | 21 | 5.95 | 2.048 | 16A-477 | |
| 2016-06-13 | 21 | 9.80 | 2.048 | 16A-477 | |
| 2016-06-13 | 21 | 14.75 | 2.048 | 16A-477 | |
| 2016-06-13 | 21 | 21.85 | 2.048 | 16A-477 | |
| 2016-07-08 | 46 | 3.00 | 2.048 | 16A-477 | |
| 2016-07-08 | 46 | 5.95 | 2.048 | 16A-477 | |
| 2016-07-08 | 46 | 9.80 | 2.048 | 16A-477 | |
| 2016-07-08 | 46 | 21.85 | 2.048 | 16A-477 | |
| 2016-09-07 | 106 | 3.00 | 2.048 | 16A-477 | |
| 2016-09-07 | 106 | 5.95 | 2.048 | 16A-477 | |
| 2016-09-07 | 106 | 9.80 | 2.048 | 16A-477 | |
| 2016-09-07 | 106 | 21.85 | 2.048 | 16A-477 | |
| 2017-02-17 | 270 | 5.50 | 2.048 | 17A-167 | |
| 2017-02-17 | 270 | 9.00 | 2.048 | 17A-167 | |
| 2017-02-25 | 278 | 3.00 | 2.048 | 17A-167 |
| MJD | Time since Explosion | Time Range | Count-rate | Unabsorbed Flux | Instrument |
|---|---|---|---|---|---|
| (days) | (days) | ||||
| 57538.0 | 6.1 | (1.8-10.0) | XRT | ||
| 57543.4 | 11.5 | - | ( | XMM | |
| 57545.6 | 13.7 | (10.1-16.8) | XRT | ||
| 57553.3 | 21.4 | (17.9-24.0) | XRT | ||
| 57559.4 | 27.5 | - | XMM | ||
| 57626.0 | 94.1 | (26.6-157.6) | XRT | ||
| 57785.1 | 253.2 | (168.9-326.9) | XRT |
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SN 2016coi (ASASSN-16fp): an energetic H-stripped core-collapse supernova from a massive stellar progenitor with large mass loss
Center for Interdisciplinary Exploration and Research in Astrophysics (CIERA) and Department of Physics and Astronomy, Northwestern University, Evanston, IL 60208
Center for Interdisciplinary Exploration and Research in Astrophysics (CIERA) and Department of Physics and Astronomy, Northwestern University, Evanston, IL 60208
Astrophysics Research Institute, Liverpool John Moores University, 146 Brownlow Hill, Liverpool L3 5RF, UK
J. Brimacombe
Coral Towers Observatory, Cairns, QLD 4870, Australia
D. Caprioli
Department of Astrophysical Sciences, Princeton University, 4 Ivy Ln., Princeton NJ 08544, USA
P. Challis
Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, Massachusetts, 02138, USA
R. Chornock
Astrophysical Institute, Department of Physics and Astronomy, 251B Clippinger Lab, Ohio University, Athens, OH 45701, USA
D. L. Coppejans
Center for Interdisciplinary Exploration and Research in Astrophysics (CIERA) and Department of Physics and Astronomy, Northwestern University, Evanston, IL 60208
Subo Dong
Kavli Institute for Astronomy and Astrophysics, Peking University, Yi He Yuan Road 5, Hai Dian District, Beijing 100871, China
C. Guidorzi
Department of Physics and Earth Science, University of Ferrara, via Saragat 1, I-44122, Ferrara, Italy
K. Hurley
University of California, Berkeley, Space Sciences Laboratory, 7 Gauss Way, Berkeley, CA 94720-7450, USA
R. Kirshner
Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, Massachusetts, 02138, USA
G. Migliori
Dipartimento di Fisica e Astronomia, Alma Mater Studiorum, Università degli Studi di Bologna, Via Gobetti 93/2, I-40129 Bologna, Italy
INAF Istituto di Radioastronomia, via Gobetti 101, I-40129 Bologna, Italy
D. Milisavljevic
Department of Physics and Astronomy, Purdue University, 525 Northwestern Avenue, West Lafayette, IN 47906, USA
D. M. Palmer
Los Alamos National Laboratory, Los Alamos, NM, 87545, USA
J. L. Prieto
Núcleo de Astronomía de la Facultad de Ingeniería, Universidad Diego Portales, Av. Ejército 441, Santiago, Chile
Millennium Institute of Astrophysics, Santiago, Chile
L. Tomasella
INAFOsservatorio Astronomico di Padova, vicolo dell’Osservatorio 5, Padova I-35122, Italy
P. Marchant
Center for Interdisciplinary Exploration and Research in Astrophysics (CIERA) and Department of Physics and Astronomy, Northwestern University, Evanston, IL 60208
A. Pastorello
INAFOsservatorio Astronomico di Padova, vicolo dell’Osservatorio 5, Padova I-35122, Italy
B. J. Shappee
Institute for Astronomy, University of Hawai’i, 2680 Woodlawn Drive, Honolulu, HI 96822, USA
K. Z. Stanek
Department of Astronomy, The Ohio State University, 140 West 18th Avenue, Columbus, OH 43210, USA
Center for Cosmology and Astroparticle Physics, The Ohio State University, 191 W. Woodruff Avenue, Columbus, OH 43210, USA
M. D. Stritzinger
Department of Physics and Astronomy, Aarhus University, Ny Munkegade 120, 8000 Aarhus C, Denmark
S. Benetti
INAFOsservatorio Astronomico di Padova, vicolo dell’Osservatorio 5, Padova I-35122, Italy
Ping Chen
Kavli Institute for Astronomy and Astrophysics, Peking University, Yi He Yuan Road 5, Hai Dian District, Beijing 100871, China
L. DeMarchi
Center for Interdisciplinary Exploration and Research in Astrophysics (CIERA) and Department of Physics and Astronomy, Northwestern University, Evanston, IL 60208
N. Elias-Rosa
Institute of Space Sciences (ICE, CSIC), Campus UAB, Carrer de Can Magrans s/n, 08193 Barcelona, Spain
Institut d’Estudis Espacials de Catalunya (IEEC), c/Gran Capitá 2-4, Edif. Nexus 201, 08034 Barcelona, Spain
C. Gall
DARK, Niels Bohr Institute, University of Copenhagen, Lyngbyvej 2, 2100 Copenhagen, Denmark
J. Harmanen
Tuorla Observatory, Department of Physics and Astronomy, FI-20014 University of Turku, Finland
S. Mattila
Tuorla Observatory, Department of Physics and Astronomy, FI-20014 University of Turku, Finland
Abstract
We present comprehensive observations and analysis of the energetic H-stripped SN 2016coi (a.k.a. ASASSN-16fp), spanning the -ray through optical and radio wavelengths, acquired within the first hours to 420 days post explosion. Our observational campaign confirms the identification of He in the SN ejecta, which we interpret to be caused by a larger mixing of Ni into the outer ejecta layers. From the modeling of the broad bolometric light curve we derive a large ejecta mass to kinetic energy ratio (, ). The small [Ca ii] \lambda$$\lambda7291,7324 to [O i] \lambda$$\lambda6300,6364 ratio (0.2) observed in our late-time optical spectra is suggestive of a large progenitor core mass at the time of collapse. We find that SN 2016coi is a luminous source of X-rays ( in the first days post explosion) and radio emission ( at peak). These values are in line with those of relativistic SNe (2009bb, 2012ap). However, for SN 2016coi we infer substantial pre-explosion progenitor mass-loss with rate and a sub-relativistic shock velocity , in stark contrast with relativistic SNe and similar to normal SNe. Finally, we find no evidence for a SN-associated shock breakout -ray pulse with energy . While we cannot exclude the presence of a companion in a binary system, taken together, our findings are consistent with a massive single star progenitor that experienced large mass loss in the years leading up to core-collapse, but was unable to achieve complete stripping of its outer layers before explosion.
supernovae,SN 2016coi, ASASSN-16fp
††journal: ApJ
1 Introduction
Hydrogen-stripped core-collapse supernovae (i.e., type Ibc SNe), also called stripped-envelope SNe (SESNe; Clocchiatti et al., 1996), have enjoyed a surge of interest in the last two decades thanks to the association of the most energetic elements of the class with Gamma-Ray Bursts (GRBs). Yet, the stellar progenitors of type Ibc SNe have so far eluded uncontroversial detection in pre-explosion images (Gal-Yam et al. 2005; Maund et al. 2005; Elias-Rosa et al. 2013; Eldridge et al. 2013). Relevant in this respect is the discovery of a progenitor in pre-explosion images of the type Ib SN iPTF13bvn, interpreted to be a single Wolf-Rayet (WR) star with a mass at zero-age main-sequence (ZAMS) MZAMS M*⊙* (Cao et al., 2013; Groh et al., 2013). This result was later disputed by Bersten et al. (2014a). More recently, Van Dyk et al. (2018), Kilpatrick et al. (2018) and Xiang et al. (2019) identified a source in archival Hubble Space Telescope (HST) images covering the location of the type Ic SN 2017ein, with properties compatible with a WR star of MZAMS\sim$$55 M*⊙* (although the presence of a companion star could not be ruled out).
The stripping of the hydrogen and helium envelope in massive stars mainly occurs through two channels: (i) line-driven winds, which dominate the mass-loss yield in single star evolution; or (ii) interaction with a companion star in a binary system. In the former scenario, the progenitor is expected to be an isolated, massive WR star (MZAMSM*⊙; Hamann et al., 2006), consistent with the inferences by Cao et al. (2013), Groh et al. (2013), Van Dyk et al. (2018) and Kilpatrick et al. (2018) with typical mass-loss rate (Maeder, 1981; Woosley et al., 1995; Begelman & Sarazin, 1986). In the binary progenitor scenario, instead, the primary exploding star is expected to be a helium star (or a C+O star in case of type Ic SNe) with lower-mass MZAMS M⊙* (Podsiadlowski et al., 1992; Yoon et al., 2010; Eldridge et al., 2013; Dessart et al., 2015). The lower mass of the progenitor stars in the binary progenitor scenario naturally accounts for the discrepancy between the large inferred rate of SESNe compared to massive WR stars (Georgy et al., 2009; Smith et al., 2011; Eldridge et al., 2013; Smith, 2014), and for the low ejecta masses inferred from the modeling of the bolometric light-curves of type Ibc SNe ( M*⊙*; e.g., Ensman & Woosley, 1988; Drout et al., 2011; Dessart et al., 2012; Bersten et al., 2014b; Eldridge et al., 2015; Lyman et al., 2016; Taddia et al., 2018). In reality, both scenarios are likely contributing in different amounts to the observed population of SESNe.
Here we present the results from an extensive multi-wavelength campaign of the H-poor SN 2016coi (a.k.a. ASASSN-16fp) from -rays to radio wavelengths, from a few hrs to days post explosion. From our comprehensive analysis we infer that SN 2016coi originated from a compact massive progenitor with large mass loss before explosion, potentially consistent with a single WR progenitor star. SN 2016coi was discovered on 2016 May 27.55 UT (Holoien et al., 2016, MJD 57535.55;) by the All Sky Automated Survey for SuperNovae111http://www.astronomy.ohio-state.edu/~assassin/index.shtml (ASAS-SN; Shappee et al., 2014) in the irregular galaxy UGC 11868 (Fig. 1). SN 2016coi was initially classified by the NOT Unbiased Transient Survey (NUTS; Mattila et al., 2016) as a type Ic-BL SN similar to those that accompany GRBs (Elias-Rosa et al., 2016), although it was soon realized that traces of He might have been present at early times (Yamanaka et al., 2016). The optical/UV properties of SN 2016coi have been studied by Yamanaka et al. (2017), Prentice et al. (2018) and Kumar et al. (2018). These authors conclude that SN 2016coi is an energetic SN with large ejecta mass and spectroscopic similarities to type Ic-BL SNe. In terms of SN classification, SN 2016coi is intermediate between type Ib and Ic SNe. Unlike type Ib SNe, where He lines become more prominent with time (e.g., Gal-Yam, 2017), the He features of SN 2016coi disappear after maximum light.
This paper is organized as follows. We first describe our UV, optical and NIR photometry data analysis and derive the explosion properties through modeling of the SN bolometric emission in §2. Our spectroscopic campaign and inferences on the spectral properties of SN 2016coi are described in §3. In §4 we present radio observations of SN 2016coi, along with the modeling of the blast-wave synchrotron emission, while §5 is dedicated to the analysis of the luminous X-ray emission of SN 2016coi and the constraints on the progenitor mass-loss history. We describe our search for a shock breakout signal in the -rays in §6. We discuss our findings in the context of properties of potential stellar progenitors in §7 and draw our conclusions in §8.
In this paper we follow Kumar et al. (2018) and adopt , which corrected for Virgo infall corresponds to a distance of Mpc ( km s*-1* Mpc*-1*, , ), equivalent to a distance modulus of mag (Mould et al., 2000). We further adopt a total color excess in the direction of SN 2016coi mag (Schlafly & Finkbeiner, 2011) as in Yamanaka et al. (2017) and Kumar et al. (2018). Unless otherwise stated, time is referred to the inferred time of first light (§2), which is UT May 23.9 2016 (MJD 57531.9; see §2.2). The presence of a “dark phase” with a duration of a few hours to a few days (e.g., Piro & Nakar 2013) has no impact on our major conclusions. Therefore we use the term “from explosion” and “from first light” interchangeably. A summary of our adopted and inferred parameters is provided in Table 1. Uncertainties are listed at the confidence level (c. l.), and upper limits are provided at the c.l. unless otherwise noted.
2 UV, Optical and NIR photometry
2.1 Data Analysis
Our photometric data have been obtained from several different telescopes and instruments, which are listed in Table A1. UV data have been acquired with the Ultraviolet Optical Telescope (UVOT; Roming et al., 2005), on the Neil Gehrels Swift Observatory (Gehrels et al., 2004). We measured the SN instrumental magnitudes by performing aperture photometry with the uvotsource task within the HEAsoft v6.22, and following the guidelines in Brown et al. (2009). An aperture of 3″ was used. We estimated the level of contamination from the host galaxy flux using late-time observations acquired at d after first light, when the SN contribution is negligible. We then subtracted the measured count-rate at the location of the SN from the count rates in the SN images following the prescriptions in Brown et al. (2014).
Images acquired with the Liverpool Telescope have been processed with a custom-made pipeline, while we use standard overscan, bias and flatfielding within iraf222IRAF is distributed by the National Optical Astronomy Observatory, which is operated by the Association of Universities for Research in Astronomy (AURA) under a cooperative agreement with the National Science Foundation. http://iraf.noao.edu/ for the remaining optical photometry. NOTCam NIR images were reduced with a modified version of the external IRAF package IRAF (v. 2.5)333http://www.not.iac.es/instruments/notcam/guide/observe.html#reductions. The remaining NIR data reduction has been performed through standard flat-field correction, sky background subtraction and stacking of the individual exposures for an improved signal-to-noise ratio. The photometry has been extracted using the SNOoPY444Cappellaro, E. (2014). SNOoPY: a package for SN photometry, http://sngroup.oapd.inaf.it/snoopy.html package. We performed point-spread-function (PSF) photometry with DAOPHOT (Stetson, 1987). For non-detections we calculated upper limits corresponding to a S/N of 3. Zero points and color terms for each night have been estimated based on the magnitudes of field stars in the Sloan Digital Sky Survey555http://www.sdss.org (SDSS; York et al., 2000) catalog (DR9). We converted the SDSS ugriz magnitudes to Johnson/Cousins UBVRI filters following Chonis & Gaskell (2008). For NIR images, we used the Two Micron All Sky Survey (2MASS) catalog666http://www.ipac.caltech.edu/2mass/ (Skrutskie et al., 2006). We quantified the uncertainty on the instrumental magnitude injecting artificial stars (e.g., Hu et al., 2011). The resulting uncertainty was then added in quadrature to the fit uncertainties returned by DAOPHOT and the uncertainties from the photometric calibration to obtain the total uncertainty on the photometry. Our final values are reported in Tables A2A5 and shown in Fig. 2.
Our UV-to-NIR campaign densely samples the evolution of SN 2016coi in its first days post explosion, with more than 1100 observations distributed over 166 nights (the gap around 200-300 days corresponds to when SN 2016coi was behind to the Sun). As Fig. 2 shows, SN 2016coi rises to peak considerably faster in the bluer bands. The UV filters also show the fastest decline post peak, before relaxing on a significantly slower decay at . This sharp change of decay rate is not present in the redder bands, which instead show a roughly constant decay rate after peak. The late-time -band decays as 1.7 mag 100d*-1*, faster than expected from the radioactive decay of 56Co, suggesting leakage of -rays. Our last detections of SN 2016coi at d post explosion are consistent with the temporal decay inferred from earlier observations at (Fig. 2). Finally, by using a low-order polynomial fit we measure the time of maximum light in the V band V d after discovery, corresponding to MJD 57550.24 (2016 June 11.24 UT). The time of peak in other bands is reported in Table A6.
2.2 Bolometric Luminosity and Explosion Parameters
Our extensive photometric coverage allows us to reconstruct the bolometric emission from SN 2016coi from the UV to the NIR from a few days to days after explosion. As a comparison, the bolometric light-curve from Prentice et al. (2018) has similar temporal coverage but does not include the NIR and UV contributions, while Kumar et al. (2018) and Yamanaka et al. (2017) include either the UV emission or the NIR emission until days post explosion, respectively. We build the bolometric luminosity curve of SN 2016coi starting from extinction-corrected flux densities, and we interpolate the flux densities in each filter to estimate the SN emission at any given time of interest. In case of incomplete UV-to-NIR photometric coverage we assume constant color from the previous closest epochs. Finally, we integrate the resulting spectral energy distributions (SEDs) from the UV to the NIR with the trapezoidal rule to obtain the bolometric light-curve shown in Fig. 3.
We compare the bolometric light curve of SN 2016coi with a sample of well-observed H-stripped core-collapse SNe from Lyman et al. (2016) in Fig. 3. Lyman et al. (2016) used the parameter as an estimator of the broadness of the light curve, defined as the the difference in magnitude between the luminosity at peak at the luminosity 15 d after that. The smaller the , the “slower” the event, i.e., the broader the light curve. The SN with the broadest light curve in the sample of Lyman et al. (2016) is the type-Ic SN 2011bm, which has 0.2 mag. Other slow events are the type-Ic SNe 2004aw, 2005az (with =0.41 and =0.42 mag, respectively) and the type-Ib SNe 1999dn and 2004dk (with =0.32 and =0.41 mag, respectively). Figure 3 shows that with =0.41 mag, SN 2016coi is among the SNe with the broadest light-curves. Kumar et al. (2018) did a similar analysis looking at the in the single bands and reached the same conclusion.
The broad light curve indicates a large photon diffusion time scale, and hence a large ejecta mass () to kinetic energy () ratio. Assuming standard energetics, this translates to a considerably large ejecta mass, in agreement with previous findings by Prentice et al. (2018) and Kumar et al. (2018). Interestingly, SN 2016coi shows a very slow post-peak decline with a standard time to peak days (Fig. 3). This phenomenology might result from mixing of 56Ni in the outer stellar ejecta, as opposed of having all the 56Ni located at the centre of the explosion. We quantify these statements below.
We model the bolometric light-curve of SN 2016coi adopting the formalism by Arnett (1982) modified following Valenti et al. (2008) and Wheeler et al. (2015). We adopt a mean opacity and break the model degeneracy using a photospheric velocity around maximum light, as inferred from Fe ii spectral lines (§3). We find that during the photospheric phase at days the light-curve is well described by a model with kinetic energy , 56Ni mass and ejecta mass , consistent with the findings of Kumar et al. (2018). However, this model significantly underestimates the bolometric emission during the nebular phase. This is a common outcome of the modeling of energetic type-Ic SN light-curves, which motivated Maeda et al. (2003) and Valenti et al. (2008) to consider a two-component model. In two-component models the “outer component” dominates the early-time emission during the photospheric phase, while the late-time nebular emission receives a significant contribution from a denser inner core (“inner component”). Applying this modeling we find a total ejecta mass , and , with a larger fraction of Ni per unit mass in the outer component. This model also allows us to constrain the time of first light to MJD days (May 23.9, 2016 UT).
As a comparison, the spectral modeling by Prentice et al. (2018) indicates , . Scaling the emission of SN 2016coi to the GRB-associated SN 2006aj and SN 2008D, Yamanaka et al. (2017) find , (Table 1). The rough agreement among the results is not surprising given the very different methods used (with different assumptions) and the fact that the modeling of Prentice et al. (2018) is limited to optical spectra, and Yamanaka et al. (2017) only consider the optical/NIR emission of SN 2016coi during the early photospheric phase.
3 Optical Spectroscopy
3.1 Data Analysis
We obtained optical spectroscopy of SN 2016coi from a few days until days post explosion with a variety of instruments on different telescopes (Table A7). The spectroscopic log can be found in Table LABEL:fig:_spec_log. We extracted our time series of optical spectra with IRAF following standard procedures. Comparison lamps and standard stars acquired during the same night and with the same instrumental setting have been used for the wavelength and flux calibrations, respectively. When possible, we further removed telluric bands using standard stars.
Our spectroscopic campaign comprises 65 spectra (Fig. 4). The overall evolution of SN 2016coi is similar to that of type-Ic SNe. At early times d the blue part of the spectrum at Å is dominated by blends of several Fe ii multiplets. We identify the main spectral feature at Å as Si ii 6355. Before maximum light, we associate the absorption feature around Å to He i 5876, with possible contamination by Na i D. Na i dominates after maximum light. At Å the spectra of SN 2016coi show emission associated with O i \lambda$$\lambda7771,7774,7775 and the Ca ii NIR triplet. Nebular features start to appear d after explosion, when the forbidden [O i] \lambda$$\lambda6300,6364 and the [Ca ii] \lambda$$\lambda7291,7323 doublets begin to emerge.
In Fig. 5 we show a zoomed-in plot of the nebular spectrum acquired with MMT+BlueChannel at d after explosion. We plot the region of the forbidden [O i] \lambda$$\lambda6300,6364, [Ca ii] \lambda$$\lambda7291,7323 doublets, and semi-forbidden Mg i] 4571 emission line. We use gaussian profiles to model each emission line. For the doublets, we kept the separation between the two components fixed, while allowing for rigid shifts of the overall profile (this scheme will also be followed in §7.1). This simple approach allows us to adequately reproduce the emission line profiles (Fig. 5). We find that the ratio between the oxygen lines fluxes is , in reasonable agreement with the theoretical expectation of . However, the doublet is blue-shifted by Å ( km s*-1*). We find similar blue-shifts for the Ca and Mg lines. Blue-shifted oxygen line profiles of this kind are not uncommon in type Ibc SN nebular spectra, and several causes have been invoked to explain this observed phenomenology, including dust obscuration, internal scattering, contamination from other lines or residual opacity in the core of the ejecta (Modjaz et al., 2008; Taubenberger et al., 2009; Milisavljevic et al., 2010). We do not observe asymmetric structures in the spectral lines, nor do we detect any sharp decrease in the light curve of SN 2016coi, therefore we can confidently exclude the presence of dust (Elmhamdi et al., 2003, 2004). As the [O i] forbidden doublet is fairly isolated, we disfavour contamination from other lines as the origin for the blue-shift. The fact that lines of different species show this behaviour might suggest a geometrical effect. An asymmetric explosion with a bulk of material moving towards the observer could indeed cause the blue-shift. Qualitative inferences on the geometry and distribution of the oxygen-rich ejecta in SN 2016coi can be drawn from the line profile of the forbidden [O i] \lambda$$\lambda6300,6364 (Modjaz et al., 2008; Taubenberger et al., 2009; Milisavljevic et al., 2010). Double-peaked oxygen lines are usually interpreted to be formed in asymmetric explosions viewed at a high angle between the observer point of view and the jet direction (Maeda et al., 2008; Taubenberger et al., 2009). As shown in Fig. 5, the oxygen doublet in SN 2016coi presents a single, symmetric profile, reproducible with simple Gaussian functions. This result is consistent with spherically symmetric ejecta. As Maeda et al. (2008) have shown that an asymmetric profile would not develop for asymmetric explosions viewed from angles below , an asymmetric explosion cannot be ruled out. However, the asymmetric explosion scenario might actually be supported by the red excess visible in both the oxygen and magnesium line. Indeed, magnesium and oxygen are expected to have similar spatial distribution within the SN ejecta (e.g., Maeda et al., 2006; Taubenberger et al., 2009). Such an excess, visible in both features, is unlikely to be caused by line contamination, and is rather the result of ejecta asymmetries common to both line emission regions.
We conclude with a consideration on intrinsic reddening. In our highest resolution spectra acquired on November 2, 2016 UT ( days after first light) with LBT+MODS, we find a weak narrow Na i D absorption at the redshift of the host galaxy, from which we infer mag (Turatto et al., 2003; Poznanski et al., 2012). However, given the large uncertainties of this method (Phillips et al., 2013), and the lack of evidence for significant , in the following we assume mag.777This is in agreement with the assumption by Yamanaka et al. (2017) and Kumar et al. (2018). On the other hand, Prentice et al. (2018) assumed a host extinction of =0.125 mag. This assumption has no impact on our conclusions. Following Schlafly & Finkbeiner (2011), the Milky Way color excess in the direction of SN 2016coi is =0.075 mag, which we use to correct our spectro-photometric data for extinction.
3.2 SN Classification and presence of Helium in the ejecta
SN 2016coi initially showed spectral similarities to type Ic-BL SNe (and in particular to SN 2006aj, associated with GRB 060218) but later evolved to resemble a normal type Ic SN (Fig. 4). Indeed, both Kumar et al. (2018) and Prentice et al. (2018) identified SN 2016coi as being an intermediate object between the two classes, while Yamanaka et al. (2017) classified SN 2016coi as a BL-Ib SN, because of the presence of helium in the spectra and expansion velocities larger than in normal type Ib SNe. We quantitatively explore the questions of how the ejecta velocity of SN 2016coi compares to other H-stripped SNe, and the presence of He in its ejecta below.
We compare SN 2016coi to the spectral templates of normal type Ic SNe and BL-Ic SNe from Modjaz et al. (2016) in Fig. 6 after applying the same renormalization procedure. The result is presented for three different epochs: 10 days before maximum light, around maximum light, and 20 days after maximum light. Fig. 6 demonstrates that the typically prominent Ca ii H+K absorption feature of type Ic SNe spectra is almost absent in SN 2016coi (Fig. 6, top and middle panels), in closer similarity to type Ic-BL SN spectra. Notably, SN 2016coi shows a prominent absorption feature at Å that we identify as Si ii with km s*-1*, which is typically not present with this strength in normal type Ic SNe (e.g., Parrent et al., 2016).
From our comparison, SN 2016coi more closely resembles normal type Ic SNe, especially before maximum light. Compared to type Ic-BL SNe, SN 2016coi shows more prominent peaks and troughs (upper panels in Fig. 6), as a result of its lower ejecta velocities before maximum light, which cause less severe blending of the spectral features. Compared to normal type Ic SNe, however, SN 2016coi shows systematically blue-shifted spectral features. Modjaz et al. (2016) showed that in type Ic SNe (both normal and broad-line) the “broadness” of the spectral features correlates with the blue-shift of their minima, as is expected from an expanding atmosphere (e.g., Dessart et al., 2011). However, with very blue-shifted absorption minima similar to type Ic-BL, but less prominent broadening, SN 2016coi seems to deviate from this trend.
Modjaz et al. (2016) used the Fe ii 5169 to show this correlation between the blue-shift of the minima and the broadening of the absorption feature. We use the same fitting technique as in Modjaz et al. (2016) to measure the broadening of this same line for SN 2016coi at maximum light, obtaining km s*-1*. Comparing this value with their Fig. 7, it is possible to see how this is quite low for a BL-Ic, while the velocity inferred from the position of the minimum of the line profile is km s*-1*, well within the range of the other BL-Ic of their sample. Another event that had very blue-shifted minima but relatively low broadening was PTF 12gzk (Ben-Ami et al., 2012). These observations were interpreted as resulting from either the departure from spherical symmetry, or from a steep gradient of the density profile of the progenitor envelope. Interestingly, Ben-Ami et al. (2012) inferred a massive ejecta of 25-35M*⊙* and a large kinetic energy of erg for PTF 12gzk, which is comparable to SN 2016coi. SN 2016coi thus shows spectral properties that are intermediate between type Ic-BL SNe (with which SN 2016coi also shares the large kinetic energy but lower velocities before peak) and normal type Ic SNe. These results agree with the findings by Kumar et al. (2018) and Prentice et al. (2018).
We next address the presence of He in the ejecta of SN 2016coi (in Fig. 6 we marked the position of the He i 4472, 5876 6678 and 7065 lines). We investigate the velocity evolution of the most prominent spectral features among those associated with He i at 5876 Å in Fig. 7, and use the velocity evolution inferred from Si ii 6355 as a comparison. From Fig. 7 we find that He and Si show a very similar temporal evolution, with expansion velocities evolving from at 2 weeks before maximum light, to around peak. The identification of He might inspire a connection with type Ib SNe. However, we note that in SN 2016coi the He features slowly subside (by the time of maximum light He absorption is no longer prominent, Fig. 7), while in type Ib SNe He features develop with time (e.g., Filippenko, 1997; Gal-Yam, 2017). The presence of He in SN 2016coi has been recognized as a peculiar characteristic of SN 2016coi by Yamanaka et al. (2017), Kumar et al. (2018) and Prentice et al. (2018). Yamanaka et al. (2017) concluded the presence of He in SN 2016coi based on the comparison with a smoothed out and blueshifted version of the type Ib SN 2012au (Takaki et al., 2013), finding a correspondence with the position of the main helium features. They also cross-checked this result with synthetic spectra generated with the code SYN++ (Thomas et al., 2011). Kumar et al. (2018) adopted a similar strategy to the one presented in this work, performing a detailed velocity analysis of the single features. With their 1D Monte Carlo spectra synthesis code, Prentice et al. (2018) investigated what other elements could be responsible for the absorption at Å. They showed that He is indeed the favored interpretation, and that in the absence of He, unphysical amounts of Al ii and Na i would be necessary to reproduce the observed spectra.
Similar velocities between Si-rich and He-rich ejecta indicates a clear departure from the expectations of a homologous explosion of a stratified progenitor star where the outer He-rich layers are expected to expand significantly faster than the inner Si-rich layers of ejecta. This finding suggests a higher level of mixing of the ejecta, which might be connected with the capability to excite He (and hence the detection of He in our spectra).
4 Radio
4.1 VLA Data Analysis
We present in Fig. 8 multi-band observations of SN 2016coi taken up to 278 days post explosion with the Karl G. Jansky Very Large Array (VLA, projects 16A-447 and 17A-167). The details of these data are given in Table LABEL:Tab:radio. We used standard phase referencing mode and the standard flux density calibrators 3C48 and 3C286 were used to set the absolute flux density scale. The data were calibrated using the VLA pipeline in CASA version 5.4.1, and imaged in CASA (McMullin et al., 2007) following standard routines. We used Briggs weighting with a robust parameter of one to image. In the epochs where SN 2016coi was sufficiently bright, we performed phase-only self-calibration on the target. We subsequently fitted the sources in the image plane using the Python Blob Detector and Source Finder (PyBDSF, Mohan & Rafferty 2015). The uncertainties listed in Table LABEL:Tab:radio take into consideration the errors on the fit and a 5% uncertainty on the absolute flux density scale. The flux density evolution of SN 2016coi at 8.5 GHz is presented in Fig. 9 (left panel), together with a comparison with other SESNe and GRBs at the same frequency.
4.2 Inferences on the Progenitor Properties and Mass-loss History from Radio Observations
Radio emission in type Ibc SNe is well explained as synchrotron emission from relativistic electrons with a power-law distribution of Lorentz factors () that gyrate in shock amplified magnetic fields (e.g., Chevalier & Fransson 2006). SN 2016coi shows the characteristic “bell-shaped” spectrum of radio sources dominated by synchrotron self-absorption (SSA), with spectral peak flux and peak frequency . By fitting a broken power-law to the radio data of SN 2016coi we find that the optically thin part of the spectrum scales as , which implies , as typically found in radio SNe (e.g., Chevalier & Fransson 2006). For the optically thick part of the spectrum our fits indicate , consistent with the SSA expectation . We find no evidence for free-free external absorption (e.g., Weiler et al. 2002), which would cause the optically thick spectrum to be steeper than .
Using the SSA formalism by Chevalier (1998), the best fitting and above translate into a constrain on the outer shock radius evolution , magnetic field and circumstellar density profile . We find evidence for a slightly decelerating blastwave with and propagating into a medium with density profile . The inferred profile is steeper than the scaling typically observed in H-stripped SNe (e.g., Horesh et al. 2013) and causes the observed decay of with time. Normal non-decelerating type Ibc SNe typically show a constant (Chevalier, 1998). The inferred is slightly flatter than a pure wind density profile , which implies an increasing effective mass-loss with radius . We find , where is the blast wave radius at days and is the blast wave radius at the end of the radio monitoring presented here, at days. For an assumed wind velocity (appropriate for compact massive stars like WRs; Crowther 2007), these results imply that the stellar progenitor of SN 2016coi experienced a phase of enhanced mass-loss yrs before collapse. We estimate that yrs before death, the stellar progenitor of SN 2016coi was loosing twice the amount of material per unit time compared to 10 yrs before stellar demise.
According to the self-similar solutions by Chevalier (1982) the interaction of a steep SN outer ejecta profile with a shallower medium with produces an interaction region that expands as with . For SN 2016coi, the inferred and thus imply . This result is consistent with the theoretical calculations of the post-explosion outer-ejecta density profiles of compact stars (e.g., WRs), for which Matzner & McKee (1999) find . Extended red supergiants can have steeper outer density gradients (e.g. ; Fransson et al., 1996). We conclude that radio observations of SN 2016coi favor a compact progenitor star at the time of collapse.
All the considerations above do not depend on the assumed shock microphysical parameters and (i.e., the fraction of post-shock energy in magnetic fields and electrons, respectively). Below we provide the best-fitting values of the shock radius , internal energy , magnetic field and effective mass loss at a given reference epoch under the assumption of equipartition of energy between electrons, protons and (i.e., ). Following Chevalier (1998), we find:
[TABLE]
[TABLE]
The outer shock radius of Eq. 2 does not strongly depend on the assumed microphysical parameter values. From Eq. 2, we can thus derive a solid estimate of the average SN shock velocity at days . This value is similar to normal type Ibc SNe (e.g., Chevalier & Fransson 2006) and different from GRB-SNe and relativistic SNe, which show evidence for ultra-relativistic and mildly relativistic outflows (Soderberg et al., 2010b; Margutti et al., 2014; Chakraborti et al., 2015). The effective mass-loss is:
[TABLE]
and the shock internal energy is:
[TABLE]
Under the assumption of equipartition, the internal energy value sets a lower limit on the true internal energy of the system at d, and on the kinetic energy of the radio emitting material. increases with time, as the shock decelerates and more kinetic energy of the shock wave is converted into internal energy. At d we measure c and erg (in equipartition), which places SN 2016coi among energetic shocks from normal H-stripped SNe (Fig. 2 in Margutti et al. 2014).
Realistic values of and in SN shocks are likely , implying that both the equipartition and are lower limits on the true values of the system. For comparison, for more realistic values of and (typical values for relativistic shocks; Sironi & Spitkovsky, 2011), we infer and erg. Recent kinetic simulations of trans-relativistic shocks suggest values of and (Park et al., 2015; Crumley et al., 2019). An would imply a very energetic explosion, with erg, however it also yields an unrealistic . Similar values of mass-loss are more typical of progenitor stars of Type IIn SNe and are likely too high for SN 2016coi. In general, the theory of particle acceleration at strong trans-relativistic shocks not only does not explain large values of , but also does not produce the typical often inferred in radio SNe. The explanation of Chevalier & Fransson 2006 invokes shocks modified by the dynamical backreaction of the accelerated particles, which was thought to lead to concave spectra, steeper than below a few GeV, but such an argument is at odds with observations of Galactic SN remnants (Caprioli, 2012).
A robust upper limit on the effective mass-loss can be inferred from the lack of free-free external absorption in the radio spectra. Indeed, the absence of a low-frequency cut-off can be used to constrain the environment density independently from the shock microphysics. From Weiler et al. (2002), the free-free optical depth of unshocked ionized gas in a wind density profile is:
[TABLE]
where is in units of for , is the temperature of the gas, normalized to a value K typical of photoionized gas, and time is units of 1 week. Furthermore, we used cm2 g*-1* for fully ionized solar-composition ejecta and cm*-1* as the free-free absorption coefficient. The lack of evidence for free-free absorption at 10.5 days at GHz, and at 45.5 days at GHz demands , which translates into for .
5 X-rays
5.1 Swift-XRT and XMM-Newton Data Analysis
The X-Ray Telescope (XRT; Burrows et al., 2005), on board the Neil Gehrels Swift Observatory, started observing SN 2016coi on May 27, 2016 ( days post explosion) until April 17, 2017 ( days), for a total exposure time of 94.4 ks. Swift-XRT data have been analyzed using the latest HEAsoft release v6.22 and corresponding calibration files. Standard filtering and screening criteria have been applied (see Margutti et al. 2013 for details). An X-ray source is clearly detected at the location of SN 2016coi until days post explosion. The X-ray source is located from the host galaxy nucleus (which is not detected by Swift-XRT and does not represent a source of contaminating X-ray emission; see Fig. 1, bottom panel) and shows a fading behavior with time, from which we conclude that the detected X-ray emission is physically associated with SN 2016coi. The spectrum can be fit with an absorbed power-law spectral model with best fitting photon index . We find no evidence for intrinsic absorption and we place a limit for the neutral hydrogen absorption column . The Galactic in the direction of SN 2016coi is (Kalberla et al., 2005). For this spectrum, the 0.3-10 keV count-to-flux conversion factor is (unabsorbed). The Swift-XRT count-rate and flux-calibrated light-curve is reported in Table LABEL:Tab:xrays and shown in Fig. 9 (right panel).
We started deep X-ray observations of the field of SN 2016coi with XMM-Newton on June 6, 2016 (PI Margutti). We obtained two epochs of observations at days (exposure time of 29 ks, observation ID 0782420201) and days (exposure of 28 ks, observation ID 0782420301). XMM data have been analyzed with SAS (v15.0). The first observation was heavily affected by proton flaring and the net exposure time of the EPIC-pn camera after filtering out the intervals of high background was reduced to 1.1 ks, whereas for the second epoch we have 13.4 ks net exposure time. SN 2016coi is clearly detected by all three cameras in both epochs. The inferred EPIC-pn count-rate is and (0.3-10 keV) for the first and second epoch, respectively. A spectrum extracted from the first (second) epoch can be fitted with an absorbed power-law model with (). The corresponding flux is and for the first and the second epoch, respectively, consistent with the results from our Swift-XRT monitoring (Table LABEL:Tab:xrays and Fig. 9).
We do not find evidence for significant spectral evolution. From a joint fit of Swift-XRT and XMM data we find a best-fitting and .
5.2 Inferences on the Mass-loss History of the Stellar Progenitor from X-ray Observations
In normal H-poor SNe, the early time ( days) X-ray emission is expected to be dominated by Inverse Compton (IC) scattering of optical photospheric photons by relativistic electrons accelerated at the shock fronts (e.g., Björnsson & Fransson 2004; Chevalier & Fransson 2006). The non-thermal X-ray spectrum of SN 2016coi with and lacking evidence for intrinsic absorption is consistent with this expectation. Adopting the formalism by Margutti et al. (2012), the IC emission depends on: (i) density profile of the SN ejecta ; (ii) properties of the electron distribution responsible for the up-scattering ; (iii) blastwave velocity, which, in turns, depends on the circumstellar medium (CSM) density and explosion’s parameters (kinetic energy and ejecta mass ); (iv) optical bolometric luminosity of the SN (from §2.2), which is the ultimate source of photons that are upscattered to X-ray energies . We parametrize the CSM density as a wind medium (where is the progenitor wind and is the mass-loss rate) and we use with , as appropriate for SNe with compact progenitors (e.g., Matzner & McKee 1999; Chevalier & Li 2000), consistently with the results from the modeling of radio data in §4.2. We further assume a power-law distribution of electrons with and for consistency with the modeling of other SNe (e.g., Chevalier & Fransson 2006).
Considering the range of explosion parameters of §2.2 and assuming a wind velocity of , for a shock velocity of c (§4.2) we infer a mass-loss rate of . Our X-ray analysis thus provides independent evidence that SN 2016coi exploded in a dense environment when compared to type Ic-BL SNe (Fig. 10). This suggests that the stellar progenitor of SN 2016coi experienced significant mass loss in the last years before core-collapse. This result is independent of . A comparison to Eq. 3 suggests that for .
The right panel of Fig. 9 clearly shows that IC (dashed orange line) fails to reproduce the bright X-ray emission at 100 days by a large factor. At these times, synchrotron emission is expected to dominate (e.g., Chevalier & Fransson 2006). The extrapolation of the optically thin radio spectrum to the X-ray band under-predicts the observed X-ray emission by a large factor . The discrepancy between the extrapolation of synchrotron spectrum that best fits the radio and the observed X-ray data is even larger when we consider that the synchrotron cooling frequency is at days using from Eq. 1 and (where is the electron charge and is the electron mass). Above the flux density steepens as , leading to an even lower expected X-ray flux. The conclusion is that the late time days X-ray emission from SN 2016coi is too luminous to be explained within the standard framework of synchrotron radiation from a population of electrons accelerated into a simple power-law distribution .
The problem of having very luminous X-ray emission from H-stripped core-collapse SNe at late times is not new and was explored in detail by Chevalier & Fransson (2006). These authors favor an interpretation where the particle spectrum is modified and becomes flatter for . The net effect is an increase of the X-ray synchrotron emission, while the effect on the radio synchrotron emission is minor (see their Fig. 1). At the time of writing it is unclear what physical effect might produce this shape of the particle spectrum, as the cosmic-ray dominated shocks invoked by Chevalier & Fransson (2006) have not been confirmed by recent particle-in-cell (PIC) simulations (Park et al., 2015). We end by noting that at the large mass-loss rates inferred for SN 2016coi in the case of deviation from equipartition , the X-rays are likely to receive a contribution from free-free emission. From Chevalier & Fransson (2006), their Eq. 30, for this mass-loss rate we estimate at days, which is a factor lower than the observed X-ray emission at this epoch.
6 Search for shock breakout emission at high energies
For compact massive H-stripped stars that are progenitors of (some) type Ibc SNe, the very first electromagnetic signal able to escape from the explosion site and reach the observer (i.e., the breakout pulse) is expected to peak at X-ray and -ray energies (e.g., SN 2008D; Soderberg et al. 2008). We searched for a high-energy pulse associated with the shock breakout of SN 2016coi using data collected by the InterPlanetary Network (IPN), which includes Mars Odyssey, Konus-Wind, RHESSI, INTEGRAL (SPI-ACS; SPectrometer on INTEGRAL-Anti-Coincidence System), Swift-BAT (Burst Alert Telescope) and Fermi-GBM (Gamma-Ray Burst Monitor). The IPN observes the entire sky with temporal duty cycle % when all the experiments are considered. A total of 6 bursts were detected by the spacecraft of the IPN between May 22.4, 2016 and May 25.6, 2016, which covers the most likely explosion date window May days that we inferred in §2.2. None has a localization region consistent with the position of SN 2016coi. We thus conclude that there is no evidence for a SN-associated shock breakout pulse down to the IPN sensitivity threshold with fluence ( at the distance of SN 2016coi).
6.1 Comparison to Breakout Models
Following Katz et al. (2012) (and references therein), the expected shock breakout energy is (their Eq. 40), where is the stellar radius, is the opacity and is the shock velocity at breakout. For SN 2016coi we assume and adopt (i.e., a shock velocity at breakout similar to the maximum ejecta velocity as inferred from the X-ray observations, see Katz et al. 2012, their Eq. 25). For compact progenitors like WR stars with we find , significantly below the IPN sensitivity. Fermi-GBM and Swift-BAT are more sensitive and reach fluence limits of and , respectively, corresponding to and . The Swift-BAT threshold for detection is comparable to the expected . Swift-BAT observes of the sky with % temporal duty cycle. It is thus possible that Swift-BAT missed the breakout pulse, or that the breakout pulse lies just below the Swift-BAT threshold of detection. For comparison the breakout pulse in SN 2008D showed (0.3-10 keV) at peak with a duration of minutes.
More extended progenitors with radii would lead to inferred . In this case however the spectrum of breakout pulse is expected to peak at lower frequencies keV which are not probed by the hard X-ray/-ray observations presented here. A similar reasoning and conclusion apply if the radiation breakout occurred in a thick medium outside the star.
7 Discussion
Our data analysis and modeling characterize SN 2016coi as an energetic H-stripped SN with (i) He in the ejecta, (ii) a broad bolometric light-curve, and (iii) luminous X-ray and radio emission. These three observables distinguish SN 2016coi from the rest of the population of known H-stripped SNe and directly map into properties of its progenitor star: a massive, well-mixed star that experienced substantial mass loss in the years preceding core-collapse. We discuss below the implications of these findings in the broader context of stellar progenitors of H-stripped SNe.
7.1 Broad Bolometric Light-Curve and Nebular Spectroscopy Indicate a Massive Progenitor
Among H-stripped SNe, SN 2016coi shows one of the broadest bolometric light-curves (Fig. 3), from which we infer (§2.2; Kumar et al., 2018; Prentice et al., 2018). This value is larger than the typical ejecta mass inferred for H-stripped SNe (e.g., Drout et al., 2011; Bianco et al., 2014; Lyman et al., 2016; Taddia et al., 2018).
Other type Ic SNe with broad light-curves are SNe 2004aw (Taubenberger et al., 2006) and 2011bm (the broadest light curve in Fig. 3; Valenti et al., 2012), for which the inferred ejecta mass is and M*⊙, respectively. Additionally, SN 2004aw also displayed relatively high ejecta velocities ( km/s-1*) around maximum light, similar to SN 2016coi. Interestingly, a tentative identification of He in the ejecta of SN 2004aw has also been reported based on NIR spectroscopy (Taubenberger et al., 2006).
Nebular spectroscopy of SN 2016coi provides additional constraints on the mass of its stellar progenitor. The relative abundances of different elements in a stellar envelope depend on the core mass. In particular, in the models by Fransson & Chevalier (1989) the ratio of the integrated fluxes of the [Ca ii] \lambda$$\lambda7291,7324 doublet and the [O i] \lambda$$\lambda6300,6364 doublet can be used as an indicator of the progenitor core mass, with lower values signifying of more massive cores. This fact mainly results from two factors: first, in the models by Fransson & Chevalier (1989) the relative abundance Ca/O is lower for progenitors with a more massive core, producing a lower [Ca ii]/[O i] flux ratio; second, in stars with a smaller core mass and with a stratified envelope like the ones in Fransson & Chevalier (1989) models, the Ca is more mixed within the oxygen layers. Since Ca is a significantly more efficient coolant, this translates into more prominent [Ca ii]/[O i] ratio. However, several other factors can play a role in determining the observed [Ca ii]/[O i] flux ratio. Fransson & Chevalier (1989), for example, showed that higher densities of the ejecta (i.e., lower kinetic energies) would also lead to lower [Ca ii]/[O i] flux ratios. Additionally, a high degree of mixing of the entire stellar envelope, where oxygen is more centrally located, also leads to a lower [Ca ii]/[O i] flux ratio (as in this case cooling through oxygen would act as a competitor to calcium in the inner envelope). These factors make the observed [Ca ii]/[O i] flux ratio a non-monotonic tracer of the stellar core-mass.
With these caveats in mind, the [Ca ii]/[O i] flux ratio has been used in the past as a diagnostic for the progenitor star MZAMS in core-collapse SNe (e.g., Fransson & Chevalier, 1987, 1989; Elmhamdi, 2011; Kuncarayakti et al., 2015). We therefore compute this ratio as a function of time in SN 2016coi and show the results in Fig. 11. To build a homogeneous comparison sample, we retrieved late-time spectra of stripped-envelope SNe available from the literature888The spectra were retrieved from WISeREP (https://wiserep.weizmann.ac.il Yaron & Gal-Yam, 2012) and the OSC (https://sne.space; Guillochon et al., 2017).. We select all the SNe with observations at 100 days after explosion, and with at least one spectrum covering both the [O i] and the [Ca ii] region. We focus on those SNe with a [Ca ii]/[O i] ratio below 1.3. Our sample comprises 83 spectra from 29 different SNe. We then fit the line doublets with two Gaussian profiles (see Fig. 5). The position of the first centroid is kept as a free parameter, but the separation between the two lines of each doublet is kept fixed at the expected value.
From Fig. 11 it is clear that at very late phases SN 2016coi occupies the lower part of the plot, and at d has the lowest [Ca ii]/[O i] ratio, close to . For reference, Fransson & Chevalier (1989) found ratios of and for their 8 M*⊙* and 4 M*⊙* He-core progenitor models, respectively. This analysis independently supports the idea that SN 2016coi originated from a stellar progenitor with larger mass than the average progenitor of H-stripped core-collapse SNe. However, as described above, other factors can contribute to the observed [Ca ii]/[O i] ratio, like mixing and ejecta densities. Indeed, the values measured by Fransson & Chevalier (1989) would become and for the same progenitor models as above, with lower explosion kinetic energies (8 times higher densities).
Other SNe with low flux ratios () are the type Ib SN 1985F (Schlegel & Kirshner, 1989; Elmhamdi et al., 2004), and the two type Ic SNe 1997B (spectra retrieved from the Asiago Supernova Archive) and 2004aw (Taubenberger et al., 2006). Interestingly, at least two of these SNe also have broad light curves. The bolometric light-curve of SN 2004aw is very similar to SN 2016coi (Fig. 3), while SN 1985F has an even broader light curve, with a in -band of 0.52 mag (Tsvetkov, 1986) (=1.01 mag for SN 2016coi Kumar et al. 2018). Unfortunately, SN 1997B was discovered after peak. Consistent with the caveats above, some SNe with broad light curve have large [Ca ii]/[O i] ratio (e.g., SN 2011bm, Lyman et al. 2016).
Based on the estimated M*⊙* (§2.2), and assuming a fiducial mass for the remnant compact object between 1.5 M*⊙* (for a neutron star) and 3 M*⊙* (for a black hole), we estimate a mass of the C+O stellar progenitor of SN 2016coi at the time of collapse of 6-10 M*⊙. Similar values have been inferred for the progenitor of SN 2004aw, for which Mazzali et al. (2017) estimated a ZAMS mass of M⊙*.999The field of SN 2016coi was not serendipitously observed by HST before explosion, which prevents a constraining search for a progenitor star in pre-explosion images. The H Galaxy Survey (James et al., 2004) observed the field of SN 2016coi on June 6th, 2000. A compact source of H emission is clearly detected ″ from the SN location, (yellow mark in Fig. 1). At the distance of SN 2016coi, this angular separation corresponds to a projected distance of 0.43 kpc. Prentice et al. (2018) estimated 0.375 kpc, using however a shorter distance to the host galaxy (see Table 1). The actual value of the inferred ZAMS mass strongly dependends on the adopted mass loss prescriptions (e.g., Smith, 2014).
7.2 Luminous Radio and X-ray Emission from Large Progenitor Mass-loss before Explosion
The recent mass-loss history of the progenitor star in the centuries leading up to the explosion can be constrained with radio and X-ray observations, which sample the emission originating from the interaction between the fastest SN ejecta and the CSM. The resulting luminosity mainly depends on the shock velocity and on the environment density, with faster shocks and denser environments powering the most luminous radio and X-ray displays.
We compare the properties of SN 2016coi that we inferred in §4.2 and 5.2 to a sample of H-stripped SNe in Fig. 10. SNe with fast ejecta velocities like Ic-BL SNe (orange squares and triangles in Fig. 10) tend to be associated with low-density environments, while type IIb SNe are located within the densest circumstellar media. From the radio we inferred a shock velocity of for SN 2016coi. This sub-relativistic shock can be caused either by a lower shock velocity at breakout, or by a denser-than-average environment surrounding the progenitor. In the latter case, the CSM was sculpted by a prolonged enhanced mass-loss phase of the stellar progenitor in the years before stellar death. The environment of SN 2016coi is among the densest in the sample of type Ibc SNe. Assuming equipartion of energy, from the radio data we obtained a lower limit for the mass-loss of SN 2016coi of M*⊙yr-1* (for km s*-1*). X-ray analysis pushed this value even higher, with M*⊙yr-1*. Such a large mass-loss rate is consistent with those associated with extreme line-driven winds in WR stars (Crowther, 2007), as we show in Fig. 10-12. This result is also supported by the radio modelling, which showed that the post-explosion density profile of the outer ejecta is consistent with having originated from a compact object like a WR star. The inferred , if sustained for the entire duration of the WR phase, implies a total mass-loss of several possibly sufficient to strip the progenitor star of a large fraction of its helium envelope even in the absence of interactions with a binary companion 101010The measured mass-loss refers to the WR-phase of the progenitor, therefore little could be said about the process responsible for the stripping of its hydrogen envelope.. This scenario is consistent with the indication of a massive stellar progenitor of §7.1.
7.3 He Spectral Features as a Signature of Asymmetries?
The presence of He in SN 2016coi is supported by the comparison with the velocity profile of Si ii 6355 (§3.2), and by the detailed spectral modeling of Prentice et al. (2018). He i lines are formed through non-thermal excitation and ionization (Lucy, 1991), for example by -rays produced by the radioactive decay of 56Ni and 56Co. For this excitation channel to be effective, plumes of 56Ni-rich material must have been able to reach the outer He-rich layers of the progenitor star of SN 2016coi, consistent with the results from our two-zone modeling of the bolometric emission from SN 2016coi in §2.2, and consistent with the results from recent 3D simulations of stellar explosions (e.g., Wongwathanarat et al. 2015) and studies of SN remnants (Milisavljevic & Fesen, 2015). Indeed, models of Dessart et al. (2012) showed that a single plume of 56Ni-rich material injected into the outer layers (e.g., in the form of a jet) is capable of producing weak He features. Alternatively, 3D simulations of neutrino-driven explosions have shown mixing instabilities that are capable of injecting 56Ni- and Si-rich plumes to the higher velocities layers of the ejecta (e.g., Hammer et al., 2010). Indeed, we observed a very similar velocity evolution for Si ii and He i, supporting this scenario. In their spectral modelling, Prentice et al. (2018) also showed that at early phases heavy ions were travelling at a very high speed; Fe ii was the fastest species at 26 000 km s*-1*. Also the Ca ii showed similar high velocities, possibly hinting to some high velocity material coming from the progenitor core, as seen in GRB-SNe (e.g. Bufano et al., 2012; Toy et al., 2016; Ashall et al., 2019).
Among type Ic SNe with broad lines, SNe 2009bb and 2012ap have been reported to have signatures of He in their spectra111111There is also a disputed claim of He in SN 1998bw (Patat et al., 2001), and in the more recent SN 2017iuk (Izzo et al., 2019). (Pignata et al., 2011; Milisavljevic et al., 2015b). Interestingly, SNe 2009bb and 2012ap are currently the only two cases of SNe with mildly relativistic ejecta not associated with a GRB (Soderberg et al., 2010b; Margutti et al., 2014; Chakraborti et al., 2015). This phenomenology has been suggested to be the result of a jet-driven stellar explosion where the jet fails to break through the stellar envelope (Morsony et al., 2007; Lazzati et al., 2012; Margutti et al., 2014). In this picture, relativistic SNe and GRBs are intrinsically different types of explosions, as opposed to similar explosions viewed from different perspectives. In relativistic SNe the jet is possibly choked by the more extended stellar envelope, but manages to “transport” some 56Ni-rich material outwards and then excites some residual He that the stellar progenitor failed to shed before stellar death (Maeda et al., 2002; Suzuki & Maeda, 2018; Izzo et al., 2019).
We speculate that a similar scenario applies to SN 2016coi, for which the lack of evidence for mildly relativistic ejecta can be explained as the result of a jet that died deep inside the star, leaving no imprint on the dynamics of the fastest ejected material, yet accelerating the inner layers to velocities larger than in normal type Ic SNe (Fig. 6), and at the same time injecting metal-rich material into the outer layer of the ejecta. In this context, the difference between normal type Ibc SNe and those with large ejecta velocities (including type Ic-BL and SN 2016coi) would be ascribed to the absence/presence of a jet at the time of core-collapse (Khokhlov et al., 1999; Granot & Ramirez-Ruiz, 2004; Wheeler & Akiyama, 2010; Lazzati et al., 2012; Nagakura et al., 2012; Margutti et al., 2014; Soker, 2016).
8 Summary and Conclusions
We present the results of a multi-wavelength, -rays to radio campaign on the peculiar SN 2016coi (Yamanaka et al., 2017; Kumar et al., 2018; Prentice et al., 2018) during its first 420 days of evolution. Our findings can be summarized as follows:
- •
From extensive UV/optical/NIR photometry we derive a broad bolometric light-curve (Fig. 3), which is suggestive of a larger-than-average explosion ejecta mass. From our two-zone modeling we infer (consistent with previous findings by Kumar et al. 2018), with a larger fraction of 56Ni per unit mass in the outer part of the ejecta. We also constrain a total kinetic energy of .
- •
Our spectroscopic analysis supports the presence of He in the SN ejecta, confirming the previous findings by Yamanaka et al. (2017), Kumar et al. (2018) and Prentice et al. (2018). We furthermore find a low [Ca ii] \lambda$$\lambda7291,7324 to [O i] \lambda$$\lambda6300,6364 ratio, suggestive of a large progenitor core mass at the time of collapse.
- •
SN 2016coi is a luminous source of radio and X-rays, which result from the propagation of a sub-relativistic blast wave with into a dense environment sculpted by sustained mass-loss from the progenitor star before core-collapse. We infer a lower limit on the mass-loss rate of (for wind velocity and assuming energy equipartion), significantly larger than in type Ic-BL SNe.
- •
Radio modelling also revealed a phase of higher mass-loss rate lasting until years before explosion. Additionally, we inferred a post-explosion density profile of the outer ejecta compatible with the explosion of a compact star (e.g., a WR, as opposed to extended progenitors like red and yellow supergiant stars).
- •
We investigated the presence of a high-energy prompt pulse of emission in the -rays. From our analysis we can rule out a SN-associated shock breakout pulse with energy , consistent with the theoretical expectations of shock break out from WR stars or from extended winds.
The emerging picture is that of a massive compact progenitor star that was able to retain some He until collapse, despite the heavy mass loss experienced in the years leading up to stellar demise. The combination of (i) large ejecta mass and (ii) large mass-loss in a H-stripped core-collapse SN with (iii) weak He features in the spectra, set SN 2016coi apart from all SNe with similar data coverage and quality in the literature. We speculate that the energetic SN 2016coi might be the result of a failed jet that was choked by the extended envelope mass of its progenitor star, in analogy with the relativistic type Ic-BL SNe 2009bb and 2012ap for which He has been identified in the ejecta. It is possible that this picture of a jet-driven explosion where the jet has been choked while trying to pierce through the He-rich stellar envelope extends to the entire class of type Ic-BL SNe that are not associated with GRBs. Future observing campaigns of type Ic-BL SNe with coordinated optical and NIR spectroscopy will reveal if traces of He in type Ic-BL SNe are more common than currently thought.
Acknowledgments
We thank N. Morrell for observing at du Pont telescope, and E. Falco for observing at FLWO.
ASAS-SN is supported by the Gordon and Betty Moore Foundation through grant GBMF5490 to the Ohio State University and NSF grant AST-1515927. Development of ASAS-SN has been supported by NSF grant AST-0908816, the Mt. Cuba Astronomical Foundation, the Center for Cosmology and AstroParticle Physics at the Ohio State University, the Chinese Academy of Sciences South America Center for Astronomy (CASSACA), the Villum Foundation, and George Skestos. We thank the Las Cumbres Observatory (LCOGT) and its staff for its continuing support of the ASAS-SN project. The Liverpool Telescope is operated on the island of La Palma by Liverpool John Moores University in the Spanish Observatorio del Roque de los Muchachos of the Instituto de Astrofísica de Canarias with financial support from the UK Science and Technology Facilities Council. Based on observations made with the Nordic Optical Telescope Scientific Association at the Observatorio Roque de los Muchachos, La Palma, Spain, of the Instituto de Astrofísica de Canarias. Partially based on observations obtained with Copernico 1.82m Telescope (Asiago) operated by INAF Osservatorio Astronomico di Padova. This work makes use of data gathered with the 6.5-m Magellan Telescopes, at Las Campanas Observatory in Chile. Based on observations obtained with XMM-Newton, an ESA science mission with instruments and contributions directly funded by ESA Member States and NASA. We acknowledge the use of public data from the Swift data archive. This work made use of the data products generated by the NYU SN group, and released under DOI:10.5281/zenodo.58766, available at https://github.com/nyusngroup/SESNtemple/. This work has made use of the Weizmann Interactive Supernova Data Repository (https://wiserep.weizmann.ac.il). This work has made use of the Berkeley Supernova Database (http://heracles.astro.berkeley.edu/sndb/). This research has made use of the NASA/IPAC Extragalactic Database (NED), which is operated by the Jet Propulsion Laboratory, California Institute of Technology, under contract with NASA. The National Radio Astronomy Observatory is a facility of the National Science Foundation operated under cooperative agreement by Associated Universities, Inc. The RM group at Northwestern is partially supported by the National Aeronautics and Space Administration through Chandra Award Number GO6-17053A issued by the Chandra X-ray Center, which is operated by the Smithsonian Astrophysical Observatory for and on behalf of the National Aeronautics Space Administration under contract NAS8-03060, the Swift Guest Investigator program, NASA Grants NNX17AD82G and 80NSSC18K0575 and the XMM Guest Investigator program, NASA Grant NNX16AT58G. SD and PC acknowledge Project 11573003 supported by NSFC. This research uses data obtained through the Telescope Access Program (TAP), which has been funded by the National Astronomical Observatories of China, the Chinese Academy of Sciences, and the Special Fund for Astronomy from the Ministry of Finance. KH is grateful for support under the Fermi Guest Investigator program, NASA Grant NNX15AU74G. Support for JLP is provided in part by FONDECYT through the grant 1191038 and by the Ministry of Economy, Development, and Tourism’s Millennium Science Initiative through grant IC120009, awarded to The Millennium Institute of Astrophysics, MAS. LT and SB are partially supported by PRIN INAF 2017 “Towards the SKA and CTA era: discovery, localisation and physics of transient sources (PI M. Giroletti).” MS is supported by a generous grant (13261) from VILLUM FONDEN and a project grant (8021-00170B) from the Independent Research Fund Denmark. NER acknowledges support from the Spanish MICINN grant ESP2017-82674-R and FEDER funds. CG is supported by a VILLUM FONDEN Investigator grant (project number 16599). JH acknowledges financial support from the Finnish Cultural Foundation.
ASAS-SN, Liverpool Telescope, Neil Gehrels Swift Observatory, XMM-Newton, Nordic Optical Telescope, Multiple Mirror Telescope, Rapid Eye Mount, 1.82m Copernico, 1.22m Galileo, du Pont Telescope, Large Binocular Telescope, Magellan, Telescopio Nazionale Galileo, Tillinghast 1.5m, Las Cumbres Observatory, DEMONEXT, WHO 1m (Weihai Observatory), T50 (OAUV), Gem (University of Iowa).
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1Arnett (1982) Arnett, W. D. 1982, Ap J, 253, 785
- 2Ashall et al. (2019) Ashall, C., et al. 2019, MNRAS, 1522
- 3Barbon et al. (1999) Barbon, R., Buondí, V., Cappellaro, E., & Turatto, M. 1999, A&AS, 139, 531
- 4Begelman & Sarazin (1986) Begelman, M. C., & Sarazin, C. L. 1986, Ap J, 302, L 59
- 5Ben-Ami et al. (2012) Ben-Ami, S., et al. 2012, Ap J, 760, L 33
- 6Ben-Ami et al. (2014) Ben-Ami, S., et al. 2014, Ap J, 785, 37
- 7Benetti et al. (2011) Benetti, S., et al. 2011, MNRAS, 411, 2726
- 8Berger et al. (2002) Berger, E., Kulkarni, S. R., & Chevalier, R. A. 2002, Ap J, 577, L 5
