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Astron. Astrophys. 343, 990-996 (1999) 1. IntroductionThe idea that helioseismology may be used to test the assumption that the solar age is equal to the age of the oldest meteorites is not new. Gough & Novotny (1990), who considered the problem in great detail, concluded that the accuracy of 0.3 Gy may be achieved once the seismic age indicators are measured to a precision of 0.1 µHz. The precision of current seismic data is now significantly better. However, results of recent studies of the problem yield conflicting conclusions. Before we go to the results of these studies, let us first point
out that we should expect a unique determination of the solar age from
seismic data. Calculated p-mode frequencies depend on the assumed
solar age but they also depend on other input solar parameters and
physical quantities. All these data are subject to uncertainties. We
now have at our disposal nearly 2000 accurate frequency data for solar
p-modes to determine solar age - the only observable in the standard
solar model (SSM) construction which we surrender. It would be indeed
surprising if the answer would not depend on the way we make use of
seismic data. An assessment of the uncertainty of
Guenther & Demarque (1997) concluded their comparison of the
solar frequencies with those for models calculated upon assuming
different age with the following statement: "The best agreement with
the calculated oscillation spectra is achieved for
Weiss & Schlattl (1998), proceeding in a more formal way, used
The main motivation for our work was to explain the large
difference in the conclusions of the two papers regarding the value of
© European Southern Observatory (ESO) 1999 Online publication: March 1, 1999 ![]() |