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Astron. Astrophys. 346, 831-842 (1999)
44Ti: its effective decay rate in young supernova remnants, and its abundance in Cassiopeia A
Y. Mochizuki 1,
K. Takahashi 2,
H.-Th. Janka 2,
W. Hillebrandt 2 and
R. Diehl 3
1 The Institute of Physical and Chemical Research (RIKEN), Hirosawa 2-1, Wako, Saitama 351-0198, Japan
2 Max-Planck-Institut für Astrophysik, Karl-Schwarzschild-Strasse 1, D-85740 Garching, Germany
3 Max-Planck-Institut für Extraterrestrische Physik, Giessenbachstrasse 1, D-85740 Garching, Germany
Received 18 February 1999 / Accepted 30 March 1999
Abstract
Radioactive isotopes such as 44Ti offer probably the
most direct probe into nucleosynthesis environments in the interior of
exploding stars, when the associated
-ray activities in the explosion
remnant are detected and translated back to the isotopic abundances at
the time of the explosion. In this paper, we assert that the procedure
may not necessarily be straightforward, at least in the case of
44Ti, an orbital-electron capture decay isotope. Using the
analytic model of McKee & Truelove (1995) for young supernova
remnants, and assuming the existence of overdense
56Fe-dominated clumps that contain also 44Ti, we
show that a high degree of ionization may be caused by the reverse
shock so that the electron-capture rate of 44Ti could be
significantly reduced from its laboratory value. When applied to
Cas A, this increases under certain conditions the current
44Ti-activity by a factor ,
which yields a better compatibility between the COMPTEL observation of
the 1.16 MeV line activity associated with the 44Ti decay
and the SN model predictions of the initial 44Ti abundance.
This possibility is, however, subject to various uncertainties, and in
particular to the unknown properties and radial distribution of the
clumps in the ejecta.
Key words: stars: supernovae:
general
stars: supernovae: individual:
Cas A
ISM: supernova
remnants
nuclear reactions, nucleosynthesis, abundances
Send offprint requests to: Y. Mochizuki (motizuki@postman. riken.go.jp)
SIMBAD Objects
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© European Southern Observatory (ESO) 1999
Online publication: June 17, 1999
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