Solar System Abundances and Condensation Temperatures of the Elements
© 2003. The American Astronomical Society. All rights reserved. Printed in U.S.A.
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Citation Katharina Lodders 2003 ApJ 591 1220DOI 10.1086/375492
Katharina Lodders
AFFILIATIONS
Planetary Chemistry Laboratory, Department of Earth and Planetary Sciences and McDonnell Center for the Space Sciences, Washington University, Campus Box 1169, St. Louis, MO 63130-4899
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Dates
- Received 2003 January 22
- Accepted 2003 March 21
Abstract
Solar photospheric and meteoritic CI chondrite abundance determinations for all elements are summarized and the best currently available photospheric abundances are selected. The meteoritic and solar abundances of a few elements (e.g., noble gases, beryllium, boron, phosphorous, sulfur) are discussed in detail. The photospheric abundances give mass fractions of hydrogen (X = 0.7491), helium (Y = 0.2377), and heavy elements (Z = 0.0133), leading to Z/X = 0.0177, which is lower than the widely used Z/X = 0.0245 from previous compilations. Recent results from standard solar models considering helium and heavy-element settling imply that photospheric abundances and mass fractions are not equal to protosolar abundances (representative of solar system abundances). Protosolar elemental and isotopic abundances are derived from photospheric abundances by considering settling effects. Derived protosolar mass fractions are X0 = 0.7110, Y0 = 0.2741, and Z0 = 0.0149. The solar system and photospheric abundance tables are used to compute self-consistent sets of condensation temperatures for all elements.
