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On the Influence of the Treatment of Heavy Elements in the Equation of State on the Resulting Values of the Adiabatic Exponent Γ1

Published online by Cambridge University Press:  12 April 2016

W. Däppen ,
D.O. Gough ,
A.G. Kosovichev  and
E.J. Rhodes Jr
W. Däppen
Affiliation:
Department of Physics and Astronomy, University of Southern California, Los Angeles, USA Institut für Astronomie, Universität Wien, Austria
D.O. Gough
Affiliation:
Institute of Astronomy, University of Cambridge, UK Department of Applied Mathematics and Theoretical Physics, University of Cambridge, UK
A.G. Kosovichev
Affiliation:
Institute of Astronomy, University of Cambridge, UK Crimean Astrophysical Observatory, Crimea
E.J. Rhodes Jr
Affiliation:
Department of Physics and Astronomy, University of Southern California, Los Angeles, USA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, USA

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Helioseismology and asteroseismology put high demands on the accuracy and consistent numerical realization of the equation of state (for a review see Däppen, these proceedings). This is explicitly illustrated by the helioseismic determination of the helium abundance of the solar convection zone in a recent investigation by Kosovichev et al. (1992). In that work it was observed that details of the treatment of the heavy elements matter more than is intuitively expected. Naively, one would expect an uncertainty of less than 10−4 in the key thermodynamic quantity, the adiabatic gradient Γ1. This is because in material of solar composition the heavy-element abundance is less than about 1.5 × 10−3 by number, and under solar conditions the dominant nontrivial contributions to the seismically relevant thermodynamic quantities predicted by modern equations of state agree to a few per cent, even for the much more abundant hydrogen and helium. However, Kosovichev et al. (1992) found that uncertainties in the treatment of the heavy elements translate into discrepancies in Γ1 of the order of 10−3, which is enough to disturb the helioseismic helium-abundance determination significantly. We briefly present the reason below. A forthcoming paper will show more detailed results, though some further information can already be found in papers by Kosovichev et al. (1992) and Christensen–Dalsgaard & Däppen (1992).

Type
III. Input physics for stellar structure
Information
International Astronomical Union Colloquium , Volume 137: Inside the Stars , 1993 , pp. 304 - 306
Copyright
Copyright © Astronomical Society of the Pacific 1993

References

Christensen-Dalsgaard, J. & Däppen, W.: 1992, Astron. Astrophys. Review submittedGoogle Scholar
Däppen, W.: 1992, in Astrophysical Opacities, eds. Mendoza, C. & Zeippen, C. (Revista Mexicana de Astronomía y Astrofísica) 141 – 149 Google Scholar
Däppen, W., Mihalas, D., Hummer, D.G. & Mihalas, B.W.: 1988, Astrophys. J. 332, 261 – 270 Google Scholar
Hummer, D.G. & Mihalas, D.: 1988, Astrophys. J. 331, 794 – 814 Google Scholar
Kosovichev, A.G., Christensen-Dalsgaard, J., Däppen, W., Dziembowski, W.A., Gough, D.O., & Thompson, M.J.: 1992, Mon. Not. R. astr. Soc., in the pressGoogle Scholar
Mihalas, D., Däppen, W. & Hummer, D.G.: 1988, Astrophys. J. 331, 815 – 825 Google Scholar