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Superbubbles, Wolf-Rayet Stars, and the Origin of Galactic Cosmic Rays W.R. Binns, M.H. Israel, L.M. Scott: Washington University M.E. Wiedenbeck: Jet Propulsion Laboratory A.C. Cummings, J.S. George, R.A. Leske, R.A. Mewaldt, E.C. Stone: Caltech T.T. von Rosenvinge: Goddard Space Flight Center M. Arnould, S. Goriely: Institut d’Astronomie et d’Astrophysique, Bruxelles
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Outline Introduction—Cosmic Ray Source models »Superbubbles formed from OB associations as possible source of galactic cosmic rays »Wolf-Rayet (WR) Stars as source of enhancement of certain isotopic ratios: e.g. 22 Ne/ 20 Ne, 58 Fe/ 56 Fe The CRIS experiment »Instrument »Isotopic measurements WR component as tracer of galactic cosmic ray source »Comparison of data with WR model calculations Suggested scenario for cosmic ray origin Conclusions
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Cosmic Ray Source? Stellar atmosphere injection (e.g. Meyer, Shapiro) »Low-FIP elements enhanced (as in the solar corona). Interstellar grain source (Most recently Meyer et al.) »Refractory elements enhanced »Mass dependence for volatile elements Acceleration of material in superbubbles by SN shocks Higdon et al. ApJ To be pub., Aug. 2005; ApJ 590 (2003) 822; ApJ 509 (1998) L33; Lingenfelter et al. ApJL 500 (1998) L153. Streitmatter et al. A&A 143 (1985) 249. »Supernova material »Wind material from massive stars
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Superbubbles & Supernovae Superbubbles blown by stellar winds & SN in OB associations Superbubble size: ~100-1000 pc The majority of core-collapse SN (80-90%) in our galaxy occur in superbubbles (Higdon & Lingenfelter). Mean time between SN within OB assoc.~10 6 y SN shocks accelerate ambient superbubble material Superbubble in Perseus Arm Superbubble (N 70) in the Large Magellanic Cloud (ESO-VLT image) ~100 pc diameter
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Wolf-Rayet Stars Evolutionary phase of massive O & B type stars exist primarily in OB associations WR Mass—15-45 M ⊙ High velocity surface winds (~1,000-4,000 km/s) eject material into the ISM Often are dusty and ~>60% are binaries—puzzle how dust can exist in such a hot environment Two phases—WN and WC »WN--CNO processed material is ejected with production of high 13 C/ 12 C and 14 N/ 16 O ratios »WC--Wind enrichment of He- burning products: esp. C, O, and 22 Ne through reaction 14 N( , ) 18 F(e + ) 18 O( , ) 22 Ne WR-124 in Sagittarius—Hubble Image WR-104 in Sagittarius—Keck Telescope Image Diam~0.2pc Diam~200au
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Evolution of surface abundances (mass fraction) with stellar mass for 60M ⊙ star (Meynet & Maeder, 2003) Time evolution of WR abundances Non- rotating star Rotating Star 300 km/s at equator Top curve—total mass; Bottom curve—convective core mass 2D models—van Marle Time evolution of mass Non-rotating Star Rotating star
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Cosmic Ray Isotope Spectrometer (CRIS) Large geometrical factor of CRIS (~50 x previous instruments) Excellent mass resolution enables precise identification of abundances. Statistical sample is large enough so that the energy spectra of the Neon isotopic ratios (important ratios as will be seen later) have been obtained
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CRIS GCR Isotopic Measurements
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Source Abundances & Tracer Isotopes To obtain source abundances from measured abundances, use “tracer” method (Wiedenbeck & Stone) Use secondary isotopes to “subtract” the secondary component of isotopes that are predominantly primary
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Two component models Wolf-Rayet winds from stars with various initial masses, with and without rotation. Adjust the WR fraction mixed with ISM to match CR 22 Ne/ 20 Ne. (Goriely, Arnould & Meynet Modeling) “Combined” data points (red) are mean values of ratios from Ulysses, Voyager, ISEE-3 and HEAO-3-C2
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ModelWR Fraction M60-no rot0.20 M85-no rot0.12 M120-no rot0.16 M40-rot0.22 M60-rot0.16 M85-rot0.41 M120-rot0.35 Fraction of WR material mixed with ISM with solar system composition to normalize to 22 Ne/ 20 Ne ratio 300 km/s But what about the 14 N/ 16 O and N/Ne ratios???
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Volatility & mass fractionated GCR source abundances Meyer et al., 1997 model—Refractory elements are enriched in GCRs since they sputter off accelerated dust grains » preferential acceleration (~factor of 13 enhancement) »Additionally, even for volatile elements, there appears to be a mass bias for which they estimate a mass dependency of A 0.8 0.2 Ratios need to be corrected for these effects. Oxygen »Volatile in elemental or molecular form »But 23% is estimated to reside in refractory compounds in the ISM (e.g. silicates) (K. Lodders, 2003) Nitrogen »Exists primarily as a gas in space Carbon »Refractory in elemental form »But a poorly known fraction exists in volatile molecules (e.g. CO) in space. Neon »Entirely volatile
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GCR source abundances compared with WR model corrected for volatility and mass fractionation (open symbols)
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Suggested Scenario WR star ejecta, enriched in 22 Ne and other neutron- rich isotopes, mixes within the superbubble (Higdon & Lingenfelter) with » Ejecta from core-collapse SN »Average ISM (represented by solar-system abundances) Refractory elements must exist mostly as grains and volatile elements mostly as gas. SN shocks accelerate mix of material in SB to cosmic ray energies »Grains are preferentially accelerated (Ellison et al.) Mean time between SN events in SB is ~3-35 x 10 5 y (Schaller et al. 1992) »Sufficient time for 59 Ni to decay to 59 Co
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Summary CRIS measurements have led to an improved value 22 Ne/ 20 Ne, 58 Fe/ 56 Fe, and other isotope ratios useful for identifying a WR component in GCRs. Comparison of CRIS and other data show »the three isotope ratios predicted to be most enhanced in WR models, 12 C/ 16 O, 22 Ne/ 20 Ne, and 58 Fe/ 56 Fe, are indeed enhanced in the cosmic rays. »Those for which enhancement is not predicted are consistent with solar system abundances, provided volatility and mass fractionation corrections are applied
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Summary (cont) We take agreement as evidence that WR star ejecta is likely an important component of cosmic-ray source material. Since most WR stars & core-collapse SN reside in SBs, then SBs must be the predominant site of injection of WR material and SN ejecta into the GCR source material. Picture that emerges is that SBs appear to be the site of origin and acceleration of at least a substantial fraction of GCRs.
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