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Sökning: WFRF:(Milam S.) > (2010-2014)

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1.
  • Meech, K. J., et al. (författare)
  • EPOXI: Comet 103P/Hartley 2 Observations from a Worldwide Campaign
  • 2011
  • Ingår i: Astrophysical Journal Letters. - London : IOP. - 2041-8213 .- 2041-8205. ; 734:L1, s. 1-9
  • Tidskriftsartikel (refereegranskat)abstract
    • Earth- and space-based observations provide synergistic information for space mission encounters by providing data over longer timescales, at different wavelengths and using techniques that are impossible with an in situ flyby. We report here such observations in support of the EPOXI spacecraft flyby of comet 103P/Hartley 2. The nucleus is small and dark, and exhibited a very rapidly changing rotation period. Prior to the onset of activity, the period was ~16.4?hr. Starting in 2010 August the period changed from 16.6?hr to near 19?hr in December. With respect to dust composition, most volatiles and carbon and nitrogen isotope ratios, the comet is similar to other Jupiter-family comets. What is unusual is the dominance of CO 2 -driven activity near perihelion, which likely persists out to aphelion. Near perihelion the comet nucleus was surrounded by a large halo of water-ice grains that contributed significantly to the total water production.
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2.
  • Wirström, Eva, 1977, et al. (författare)
  • ISOTOPIC ANOMALIES IN PRIMITIVE SOLAR SYSTEM MATTER: SPIN-STATE-DEPENDENT FRACTIONATION OF NITROGEN AND DEUTERIUM IN INTERSTELLAR CLOUDS
  • 2012
  • Ingår i: Astrophysical Journal. - 1538-4357 .- 0004-637X. ; 757:1, s. L11-
  • Tidskriftsartikel (refereegranskat)abstract
    • Organic material found in meteorites and interplanetary dust particles is enriched in D and 15N. This is consistentwith the idea that the functional groups carrying these isotopic anomalies, nitriles and amines, were formed byion–molecule chemistry in the protosolar nebula. Theoretical models of interstellar fractionation at lowtemperaturespredict large enrichments in both D and 15N and can account for the largest isotopic enrichments measured incarbonaceous meteorites. However, more recent measurements have shown that, in some primitive samples, a large15N enrichment does not correlate with one in D, and that some D-enriched primitive material displays little, ifany, 15N enrichment. By considering the spin-state dependence in ion–molecule reactions involving the ortho andpara forms of H2, we show that ammonia and related molecules can exhibit such a wide range of fractionation forboth 15N and D in dense cloud cores.We also show that while the nitriles, HCN and HNC, contain the greatest 15Nenrichment, this is not expected to correlate with extreme D enrichment. These calculations therefore support theview that solar system 15N and D isotopic anomalies have an interstellar heritage. We also compare our results toexisting astronomical observations and briefly discuss future tests of this model.
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