Astron. Astrophys. 343, 990-996 (1999)
Helioseismology and the solar age
W.A. Dziembowski 1,2,
G. Fiorentini 3,4,
B. Ricci 3,4 and
R. Sienkiewicz 2
1 Warsaw University Observatory, Al. Ujazdowskie 4, PL-00-478 Warszawa, Poland
2 N. Copernicus Astronomical Center, Polish Academy of Sciences, Bartycka 18, PL-00-716 Warszawa, Poland
3 Dipartimento di Fisica dell'Università di Ferrara, via Paradiso 12, I-44100 Ferrara, Italy
4 Istituto Nazionale di Fisica Nucleare, Sezione di Ferrara, via Paradiso 12, I-44100 Ferrara, Italy
Received 5 October 1998 / Accepted 21 December 1998
Abstract
The problem of measuring the solar age by means of helioseismology
has been recently revisited by Guenther & Demarque (1997) and by
Weiss & Schlattl (1998). Different best values for
and different assessment of the
uncertainty resulted from these two works. We show that depending on
the way seismic data are used, one may obtain
Gy close to the age of the oldest
meteorites, Gy, like in the first
paper, or above 5 Gy like in the second paper. The discrepancy in the
seismic estimates of the solar age may be eliminated by assuming
higher than the standard metal abundance and/or an upward revision of
the opacities in the solar radiative interior.
We argue that the most accurate and robust seismic measure of the
solar age are the small frequency separations,
, for spherical harmonic degrees
and radial orders
. The seismic age inferred by
minimization of the sum of squared differences between the model and
the solar small separations is Gy, a
number consistent with meteoritic data. Our analysis supports earlier
suggestions of using small frequency separations as stellar age
indicators.
Key words: Sun:
abundances
Sun: evolution
Sun: interior
Sun: oscillations
Send offprint requests to: W.A. Dziembowski
This article contains no SIMBAD objects.
Contents
© European Southern Observatory (ESO) 1999
Online publication: March 1, 1999
helpdesk.link@springer.de  |