Bibcode
Meikle, W. P. S.; Cumming, R. J.; Geballe, T. R.; Lewis, J. R.; Walton, N. A.; Balcells, M.; Cimatti, A.; Croom, S. M.; Dhillon, V. S.; Economou, F.; Jenkins, C. R.; Knapen, J. H.; Meadows, V. S.; Morris, P. W.; Perez-Fournon, I.; Shanks, T.; Smith, L. J.; Tanvir, N. R.; Veilleux, S.; Vilchez, J.; Wall, J. V.; Lucey, J. R.
Referencia bibliográfica
Monthly Notices of the Royal Astronomical Society, Volume 281, Issue 1, pp. 263-280.
Fecha de publicación:
7
1996
Número de citas
105
Número de citas referidas
93
Descripción
We present early-time infrared (IR) and optical spectroscopy, and
optical photometry, of the Type Ia supernova 1994D. These observations
provide the most complete optical-IR spectral coverage ever achieved for
a Type Ia at this phase. Optical and IR spectra were obtained as early
as 9d before maximum light. The combined optical and IR spectra of SN
1994D reveal a flux `deficit' in the R, I and J bands as early as
maximum light. They also illustrate the dramatic deepening of the J-band
deficit after maximum light. We also present a maximum light IR spectrum
of the peculiar Type Ia SN 1991T. This also shows a deficit in the J
band, but it does not show such a pronounced deficit in the R and I
bands as SN 1994D. Both supernovae show a P Cygni-like feature with the
absorption at ~1.05 μm and the emission at ~1.08 mum. In SN 1994D the
absorption shows no wavelength shift during the period between -8.5 and
-1.5 d before maximum light. After this the feature rapidly weakened. We
argue that, in this event, the P Cygni line feature formed in a discrete
shell-like zone lying above the photosphere. In SN 1991T a continuous,
shallow density gradient scattering zone seems more appropriate. For
both supernovae we explore possible identifications with HeI 1.0830
μm and MgII 1.0926 mum, but there are difficulties with either
option. In SN 1994D it may be that the feature is actually the result of
a blend of the helium and magnesium lines. However, for both supernovae
it is not ruled out that the J-band feature is really the result of a
transition in one or more unidentified species. Consideration of the
velocities associated with the feature indicates that, if its origin is
helium, then in SN 1994D it is more likely that it formed in the
alpha-rich freeze-out, but some mixing to higher velocities is also
required. In contrast, in SN 1991T we favour an origin in the form of a
residual or accreted layer on the surface of the progenitor white dwarf.
If the feature is due to magnesium then the derived velocities for SN
1994D are in good agreement with the predictions of explosion model W7.
In SN 1991T, identification with magnesium presents problems in
accounting for the inferred velocity structure.