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Meteoritic Constraints on Astrophysical Models of Star and Planet Formation

Meteoritic Constraints on Astrophysical Models of Star and Planet Formation. Steve Desch, Arizona State University. Star Formation. Chondrites : Leftover crumbs from solar system formation. Cross section of Carraweena (L3.9). MATRIX GRAINS. CHONDRULES. CAIs.

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Meteoritic Constraints on Astrophysical Models of Star and Planet Formation

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  1. Meteoritic Constraints on Astrophysical Models of Star and Planet Formation Steve Desch, Arizona State University

  2. Star Formation

  3. Chondrites: Leftover crumbs from solar system formation Cross section of Carraweena (L3.9) MATRIX GRAINS CHONDRULES CAIs

  4. CAIs: The first minerals formed in the solar system • CAIs contain many minerals that are the first to condense out of a solar nebula gas (Grossman 1972): • melilite: Ca(Al,Mg)(Si,Al)2O7, • hibonite: Ca2(AlTi)24O35, • anorthite: CaAl2Si2O8, • pyroxene: (FeMg)SiO3 McSween 1999

  5. CAIs • Fluffy Type A: • Not as large as other CAIs (< 1 mm) • Most abundant (about 1% of all CCs and OCs, 2% of Allende) • aggregations of small, zoned spheroids with spinel at their cores and mantles of melilite (Wark & Lovering 1977) • Group II Rare Earth Element patterns show ultrarefractory component depleted (Tanaka & Masuda 1973); that component apparently concentrated in nuggets like those recently found (Hiyagon et al 2003) • Formed (condensed?) in hot environment: 1400 K < T < 1800 K • Compact Type A: • Same compositions as fluffy type A, but were melted

  6. Types B and C: • Larger(up to cm-size) • Very abundant in CVs (6-10% of volume), nonexistent in others • Clearly melted after formation • Type B CAI cooling rates constrained from chemical zoning in melilite: 0.5 - 50 K/hr (Stolper & Paque 1986; Jones et al 2000) • At one time contained 26Al, 41Ca, 10Be, etc. CAIs

  7. CAIs • FUN inclusions: • “Fractionation and Unknown Nuclear effects” • Very rare (only 6) • Large mass-dependent fractionations in O, Mg, Si: apparently were severely heated and evaporated • Are anomalous in certain neutron-rich nuclei: 48Ca, 50Ti • Contain evidence they once contained 10Be • Contain no evidence they ever contained 26Al, 41Ca, etc.

  8. Short-Lived Radionuclides • CAIs contained live short-lived radionuclides: 41Ca (t1/2 = 0.1 Myr) (Srinivasan et al. 1994) 36Cl (t1/2 = 0.3 Myr) (Murty et al. 1997) 26Al (t1/2 = 0.7 Myr) (Lee et al. 1976) 60Fe (t1/2 = 1.5 Myr) (Tachibana & Huss 2003) 10Be (t1/2 = 1.5 Myr) (McKeegan et al. 2000) 53Mn (t1/2 = 3.7 Myr) (Birck & Allegre 1985) • These half-lives are so short, the radionuclides must have been created shortly before, or during, solar system formation • CAIs with evidence for 26Al all have remarkably uniform ratio 26Al/27Al = 5 x 10-5: they all formed within ~105 years of each other

  9. 10Be/9Be Ratios CAIs formed with 10Be/9Be = 9 x 10-4 Excess10B correlates with amount of Be: this 10B is from the decay of 10Be 10Be decays to 10B with t1/2=1.5 Myr Natural 10B/11B level Slope gives initial 10Be/9Be ratio McKeeganet al. (2000)

  10. 10Be/9Be Ratios • 10Be has been found in every CAI looked at, at levels consistent with 10Be/9Be = 9 x 10-4 • 10Be is present even if other radionuclides such as 26Al, 41Ca are not, in FUN inclusions and hibonites (Marhas et al. 2002; MacPherson et al. 2003) Table from Desch et al. (2004) 10Be has a different origin than 26Al, 41Ca, etc.(Marhas et al. 2002): Could it be Galactic Cosmic Rays?

  11. Collapse of Cloud Cores: Observations • Stars form in parts of molecular clouds that have gravitationally collapsed, dragged in magnetic field lines • Even the Orion Nebula must have gone through this stage (Schleuning 1998) • 10Be GCRs follow magnetic field lines, are trapped when column densities first exceed ~ 10-2 g cm-2 (before first stars) 1.3 pc Side view: Schleuning (1998)

  12. Collapse of Cloud Cores: Calculations • Numerical simulations show how magnetic fields and gas densities vary with time in collapsing molecular cloud core (Desch & Mouschovias 2001) • We calculate rates at which 10Be GCRs are trapped, and 10Be is produced by spallation • First stars form << 1 Myr after t=0 1.5 pc Desch & Mouschovias (2001)

  13. 10Be in a Collapsing Cloud Core Trapped 10Be GCRs Total • 10Be/9Be ratio = CAI ratio as first stars form! • All of the 10Be in CAIs is attributable to GCRs: 80% from 10Be GCRs trapped in cloud core 20% produced by spallation reactions • 10Be/9Be ratio does indeed peak when column densities exceed ~ 10-2 g cm-2 CAI ratio 9.5 x 10-4 10Be produced by GCR protons spalling CNO nuclei in gas

  14. Supernova Injection of Radionuclides • We attribute10Be to trapped 10Be Galactic cosmic rays • A type II supernova is the most likely source of all the other radionuclides: 41Ca, 36Cl, 26Al, 60Fe produced in proportions seen in meteorites (Meyer & Clayton 2000; Meyer et al. 2003) • We do not claim that a supernova triggered the collapse of the solar system’s cloud core • We claim the solar nebula already existed and CAIs were forming when the supernova ejecta entered the solar system (Sahijpal & Goswami 1998): “Late injection” • FUN inclusions are CAIs that formed before 26Al, 41Ca, 60Fe, and anomalous 48Ca and 50Ti were injected by supernova

  15. The Sun’s Star-Formation Environment • Ionization fronts probably triggered star formation in Eagle Nebula • 80% of Sunlike stars form near a star massive enough to supernova (Adams & Laughlin 2001) • Before massive star goes supernova it ionizes, heats, and “photoevaporates” surrounding gas Evaporating gaseous globules: new solar systems Hester et al (1996)

  16. The Sun’s Star-Formation Environment • After EGG stage, solar system emerges into H II region as a “proplyd” • Disk resides in H II region for ~105 yr until O star(s) supernova • Disk intercepts supernova ejecta with radionuclides • Proplyds in Orion will acquire 26Al/27Al ~ 5 x 10-5 when 1 Ori C supernovas

  17. Protoplanetary Disks HH30: Watson, Stapelfeldt, Krist & Burrows (2000)

  18. Protoplanetary disks are accretion disks • Angular momentum is transported outward, mass moves inward • Angular momentum transport probably due to magnetohydrodynamic turbulence (Desch 2004) PPDs: outflow Mass accretes onto star through disk

  19. As mass moves inward, gravitational energy is released, mostly at midplane • Temperatures highest at midplane, lowest at surfaces • Heat flux drives convection (Bell et al 1997) • Gas rises, cools in convection cells, rocks condense PPDs:

  20. Evidence for Condensation T = 1270 K Metallic Fe condenses FeMg silicates T = 1370 K Refractory minerals condense as rising gas cools T = 1770 K Simon et al (2002) All vapor Z

  21. More Evidence for Condensation • FeNi metal condenses as gas moves from T=1370 K to 1270 K • Ni zoning reproduced if condensation takes a few weeks, as in a convection cell model (Meibom, Desch et al 2000) Meibom et al (1999, 2000)

  22. Convection repeatedly moves material through hot midplane, evaporates most silicates • Only most refractory minerals grow (CAIs) • Convection and turbulence disperse CAIs widely (Cuzzi et al 2003a,b, 2004) • This stage requires dM/dt > 10-6 Msol/yr, ends after ~105 yr (Bell et al 2000) PPDs:

  23. PPDs: • After few x 105 years, magnetohydrodynamic turbulence occurs only in surface layers • Temperatures are everywhere much cooler, FeMg silicates form at midplane (chondrules) • Accretion is unsteady with time, leads to shocks • Shocks melt CAIs and chondrules, cool at rates ~ 50 K/hr (Desch & Connolly 2002)

  24. Conclusions CAI radionuclides constrain setting of solar system formation: • 10Be attributable to trapped 10Be Galactic cosmic rays • Other radionuclides (26Al, 41Ca, esp. 60Fe) injected by supernova • Injection occurred after first CAIs (FUN inclusions) formed • Implicates formation in H II region like Orion or Eagle Nebula CAIs constrain disk temperatures, dynamics, timescales… • CAI mineralogy implicates hot (> 1400 K) protoplanetary disk • Condensates implicate convection • Requires high mass accretion rates through disk > 10-6 Msol/yr, attainable only for ~ 105 yr • Convection, turbulence will then widely disperse CAIs

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