Supernova 2018cuf: A Type IIP supernova with a slow fall from plateau

TL;DR

This paper presents detailed photometric and spectroscopic observations of SN 2018cuf, a typical Type IIP supernova with a slow decline from its plateau, providing insights into its progenitor, explosion characteristics, and circumstellar environment.

Contribution

It offers the first comprehensive analysis of SN 2018cuf, including progenitor constraints, explosion parameters, and evidence of circumstellar interaction, which were not previously documented for this supernova.

Findings

Progenitor was a ~14.5 solar mass red supergiant.

Produced approximately 0.04 solar masses of nickel-56.

Detected circumstellar material around the progenitor.

Abstract

We present multi-band photometry and spectroscopy of SN 2018cuf, a Type IIP ("P" for plateau) supernova (SN) discovered by the Distance Less Than 40 Mpc survey (DLT40) within 24 hours of explosion. SN 2018cuf appears to be a typical Type IIP SN, with an absolute $V$-band magnitude of $-$16.73 $\pm$ 0.32 at maximum and a decline rate of 0.21 $\pm$ 0.05 mag/50d during the plateau phase. The distance of the object is constrained to be 41.8 $\pm$ 5.7 Mpc by using the expanding photosphere method. We use spectroscopic and photometric observations from the first year after the explosion to constrain the progenitor of SN 2018cuf using both hydrodynamic light curve modelling and late-time spectroscopic modelling. The progenitor of SN 2018cuf was most likely a red supergiant of about 14.5 $\rm M_{\odot}$ that produced 0.04 $\pm$ 0.01 $\rm M_{\odot}$ $\rm ^{56}Ni$ during the explosion. We also found $\sim$ 0.07 $\rm M_{\odot}$ of circumstellar material (CSM) around the progenitor is needed to fit the early light curves, where the CSM may originate from pre-supernova outbursts. During the plateau phase, high velocity features at $\rm \sim 11000\ km~s^{-1}$ are detected both in the optical and near-infrared spectra, supporting the possibility that the ejecta were interacting with some CSM. A very shallow slope during the post-plateau phase is also observed and it is likely due to a low degree of nickel mixing or the relatively high nickel mass in the SN.