Proc. of 2002 SOHO 12 /GONG + 2002, Local and Global Helioseismology: The Present and Future, Big Bear Lake, CA USA (Ed: Huguette Lacoste, ESA SP-517, Feb 2003) pp. 345-348 COMPOSITION OF THE SOLAR INTERIOR: INFORMATION FROM ISOTOPE RATIOS O. Manuel(1) and Stig Friberg(2) 1University of Missouri, Nuclear Chemistry, Rolla, MO 65409 U.S.A. tel: +1 573-341-4420 / fax: +1 573-341-6033 / e-mail:
[email protected] 2Clarkson University, Physical Chemistry, 641 Spring Hill Estate, Eminence, KY 13699-5814 U.S.A. ABSTRACT confirmed in diverse types of meteorites [10,11]. The amount of Xe-2 in the early solar system was Measurements are reviewed showing that the interior sufficient to shift the composition of bulk xenon in of the Sun, the inner planets, and ordinary meteorites meteorites (Point AVCC in Fig. 1) away from Xe-1. consist mostly of the same elements: Iron, oxygen, nickel, silicon, magnesium, sulfur and calcium [1]. These results do not support the standard solar model. INTRODUCTION Reynolds found the decay product of extinct 129I and an unusual abundance pattern of the other xenon isotopes in meteorites in 1960 [2,3]. Since 129I exceeded that expected if the solar system formed from an interstellar cloud, Fowler et al. [4] suggested that D, Li, Be, B and extinct 129I and 107Pd might have been produced locally in the early solar system. Figure 2: The link of primordial helium with xenon In 1965 the decay product of extinct 244Pu [5], a isotopes in the Allende meteorite [9]. nuclide that could only be made by rapid neutron- capture in a supernova (SN), was found in meteorites.