Bibcode
Vallely, Patrick; Moreno-Raya, M. E.; Baron, E.; Ruiz-Lapuente, Pilar; Domínguez, I.; Galbany, Lluís; González Hernández, J. I.; Méndez, J.; Hamuy, M.; López-Sánchez, A. R.; Catalán, S.; Cooke, E.; Fariña, C.; Génova-Santos, R.; Karjalainen, R.; Lietzen, H.; McCormac, J.; Riddick, F.; Rubiño-Martín, J. A.; Skillen, I.; Tudor, V.; Vaduvescu, O.
Bibliographical reference
Monthly Notices of the Royal Astronomical Society, Volume 460, Issue 2, p.1614-1624
Advertised on:
8
2016
Citations
6
Refereed citations
6
Description
We analyse a time series of optical spectra of SN 2014J from almost two
weeks prior to maximum to nearly four months after maximum. We perform
our analysis using the SYNOW code, which is well suited to track the
distribution of the ions with velocity in the ejecta. We show that
almost all of the spectral features during the entire epoch can be
identified with permitted transitions of the common ions found in normal
supernovae (SNe) Ia in agreement with previous studies. We show that
2014J is a relatively normal SN Ia. At early times the spectral features
are dominated by Si II, S II, Mg II, and Ca II. These ions persist to
maximum light with the appearance of Na I and Mg I. At later times
iron-group elements also appear, as expected in the stratified abundance
model of the formation of normal Type Ia SNe. We do not find significant
spectroscopic evidence for oxygen, until 100 d after maximum light. The
+100 d identification of oxygen is tentative, and would imply
significant mixing of unburned or only slight processed elements down to
a velocity of 6000 kms-1. Our results are in relatively good
agreement with other analyses in the infrared. We briefly compare SN
2011fe to SN 2014J and conclude that the differences could be due to
different central densities at ignition or differences in the C/O ratio
of the progenitors.