The GENESIS Mission: Solar Wind Isotopic and Elemental Compositions and Their Implications

R C Wiens, D S Burnett, K D McKeegan, A P Kallio, P H Mao, V S Heber, R Wieler, A Meshik, C M Hohenberg, J C Mabry, J Gilmour, S A Crowther, D B Reisenfeld, A Jurewicz, B Marty, R O Pepin, B L Barraclough, J E Nordholt, C T Olinger, J T Steinberg

Research output: Chapter in Book/Report/Conference proceedingConference contribution

Abstract

The GENESIS mission was a novel NASA experiment to collect solar wind at the Earth's L1 point for two years and return it for analysis. The capsule crashed upon re-entry in 2004, but many of the solar-wind collectors were recovered, including separate samples of coronal hole, interstream, and CME material. Laboratory analyses of these materials have allowed higher isotopic precision than possible with current in-situ detectors. To date GENESIS results have been obtained on isotopes of O, He, Ne, Ar, Kr, and Xe on the order of 1% accuracy and precision, with poorer uncertainty on Xe isotopes and significantly better uncertainties on the lighter noble gases. Elemental abundances are available for the above elements as well as Mg, Si, and Fe. When elemental abundances are compared with other in situ solar wind measurements, agreement is generally quite good. One exception is the Ne elemental abundance, which agrees with Ulysses and Apollo SWC results, but not with ACE. Neon is of particular interest because of the uncertainty in the solar Ne abundance, which has significant implications for the standard solar model. Helium isotopic results of material from the different solar wind regimes collected by GENESIS is consistent with isotopic fractionation predictions of the Coulomb drag model, suggesting that isotopic fractionation corrections need to be applied to heavier elements as well when extrapolating solar wind to solar compositions. Noble gas isotopic compositions from GENESIS are consistent with those obtained for solar wind trapped in lunar grains, but have for the first time yielded a very precise Ar isotopic result. Most interesting for cosmochemistry is a preliminary oxygen isotopic result from GENESIS which indicates a solar enrichment of ~4% in 16O relative to the planets, consistent with a photolytic self-shielding phenomenon during solar system formation. Analyses of solar wind N and C isotopes may further elucidate this phenomenon. Preliminary results from GENESIS have been reported for N, and results are still pending for C.
Original languageEnglish
Title of host publicationAGU 2008 Fall Meeting. San Francisco, USA. 15th – 19th December 2008.
PagesAbstract SH21A-1569
Publication statusPublished - 2008
EventAGU 2008 Fall Meeting - San Francisco, United States
Duration: 15 Dec 200819 Dec 2008

Conference

ConferenceAGU 2008 Fall Meeting
Country/TerritoryUnited States
CitySan Francisco
Period15/12/0819/12/08

Keywords

  • 1027 Composition of the planets
  • 2169 Solar wind sources
  • 5205 Formation of stars and planets
  • 7529 Photosphere

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