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Molecular Differentiation in Pre-stellar Cores

This study focuses on the molecular differentiation in pre-stellar cores, exploring the evidence for chemical differentiation and how to use chemical composition to trace core evolution. The physical properties, density structure, temperature gradient, gas temperature, kinematics, and molecular freeze-out are discussed using various observational data. The results provide reliable estimates of the chemical composition and help in understanding the formation and evolution of pre-stellar cores.

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Molecular Differentiation in Pre-stellar Cores

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  1. Molecular Differentiation in Pre-stellar Cores Mario Tafalla Observatorio Astronómico Nacional (Spain) Outline * Basic physical properties of cores * Evidence for chemical differentiation * How to use chemical composition to trace core evolution

  2. Dense cores: simplest star-forming sites L1544-Ward-Thompson et al. (1999) L1498-Tafalla et al. (2002) B68- Alves et al. (2001) • Variety of sizes, shapes • embedded cores, exposed globules • observed in multiple tracers • Simplest laboratories to study ISM chemistry • Need to characterize their physical properties

  3. Pysical properies: core sizes • In Taurus: relatively narrow range • <r0> = 0.03 pc (= 7,000 AU) • Coincides with break point in the distribution of stars • cluster vs. binary regimes 44 Cores in Taurus (Tafalla et al. 2007) • Change in the gas physics • Transition • r > r0: supersonic/turbulent (cloud) • r < r0: subsonic/gravity (core) • How the transition occurs? • turbulence dissipation • magnetic field dissipation binaries 0.04 pc clustering Larson (1995)

  4. Density structure of starless cores & globules • Recent agreement between different techniques • Radial profiles: • central flattening (r0) • central density 105-106 cm-3 • In some cases • fit very close to expectation from isothermal (BE) sphere • center/edge contrast close to maximal (14) Alves et al. (2001) • Caveats • dust properties are not well known: factor of 2 uncertainty • most cores are not spheres (axial ratio close to 2:1). Additional source of stability (magnetic field?)

  5. Temperature: dust and gas • Dust and gas can have different temperatures • temperature set by heating = cooling • for densities > 105 cm-3, dust and gas couple thermally Galli et al. (2001)

  6. Dust temperature gradient • Cloud-wide dust temperature gradient • cloud is warm (15-20 K) • core is cold (10 K) • Consistent with extinction of ISRF Ward-Thompson et al. (2002) IC 5146 core cloud cloud Kramer et al. (1998) • Dust emissivity increases • evidence for grain coagulation: fluffy grains • small grains disappear

  7. Gas temperature • From NH3 observations • (J,K)=(1,1) & (2,2) sensitive to temperature • NH3 survives in gas phase inside core (enhanced abundance) • Low resolution data: constant temperature ≈ 10 K • High resolution observations: central drop in L1544 Crapsi et al. (2007) Tafalla et al. (2004)

  8. Kinematics. Internal motions • Derived from linewidth • N2H+ & NH3 • In contrast with clouds • internal subsonic motions • Thermal pressure support dominates turbulent pressure • Break-down of Larson’s law • velocity coherent cores (Goodman et al 1998) Taurus Tafalla et al. (2007) L1498 Tafalla et al. (2004)

  9. Molecular differentiation • Accurate determination of physical properties provides • reliable estimate of chemical composition • solution of old discrepancies between tracers • Most species do not survive in gas phase if n > few 104 cm-3 L1517B Tafalla et al. (2002)

  10. Molecular freeze out • At low temperatures: molecules stick on grains • Equilibrium situation • molecules on grains if Tgrain < Tfreezeout • molecules in gas phase if Tgrain > Tfreezeout • Time for equilibrium is ≈ 5 109 /n(H2) yr • if n(H2) = 105 cm-3, tfrz ≈ 5 104 yr (<< core lifetime) Leger (1983) Scott Sandford

  11. Why do N2H+ and NH3 stay in the gas phase? • Initial models (e.g., Bergin & Langer 1997) • N2binding energy assumed lower than CO b.e. • CO, etc freezes at low densities, N2 at high densities, N2H+ and NH3 are formed from N2 • Laboratory work (Öberg et al. 2005, Bisschop et al. 2006) • binding energies are almost equal • sticking probability S=1 • New understanding of differential freeze out • both CO and N2 freeze out simultaneously • disappearance of CO from gas phase changes chemistry • CO is highly abundant (X≈10-5) • major destroyer of N2H+ • freeze out of CO dominates chemistry (over N2 freeze out) • N2H+ is enhanced (NH3 is formed from N2H+)

  12. Molecular survey of L1498 and L1517B • Motivation: • study behavior of as many species as possible • determine a set of “well determined” abundances • Sample • L1498 and L1517B: close to round, isolated (simple) • CH3OH, SO, C3H2, H2CO, HC3N, DCO+, HCO+, C2S, CO, CS, N2H+, NH3 • Two or more transitions, optically thin isotopologues, IRAM 30m L1498 L1517B

  13. Sample maps for L1498 Tafalla et al. (2006)

  14. Abundance results (L1498)

  15. Comparison with models • Models reproduce pattern of selective depletion • CO, CS, CCS, etc deplete at center • N2H+ and NH3 survive or are even enhanced Aikawa et al. (2005)

  16. Comparison with Aikawa et al. (2005) • Despite qualitative agreement with models • order of magnitude discrepancies in some abundances (e.g., CH3OH) L1498 andL1517B Tafalla et al. (2006)

  17. Using freeze out to trace core history • Freeze out is a time-dependent process • it can be used as a clock of core contraction • In the simplest form: • old core: CO depleted, N2H+ abundant, high deuteration • young core: CO abundant, N2H+ weak, low deuteration • Define ratio R • Old core: small R • Young core: large R (measured at core center)

  18. L1521E: a core with negligible depletion

  19. Comparison with other cores: depletion-sensitive species • L1521E inner abundances: within factor 2 of outer abundances for L1498 and L1517B • Little chemical evolution except for depletion • cores originate from cloud material of similar composition • Use L1498 and L1517 as “standards”

  20. N2H+ and NH3: unusually rare • N2H+: 8 times lower than average • NH3: 20 times lower than average • Most extreme core in sample

  21. L1521E still a mystery • Chemical composition • consistent with lack of depletion in CO, etc. • unusually young core • Physical composition • central density and concentration typical of mature cores • unusually fast contraction? • We need to identify more cases like L1521E

  22. How to search for chemically young cores? • Compare effect of depletion in models (L1498 & L1517B) • Depletion decreases central intensity by factor ≈ 2 • Some species more sensitive to depletion • combination of excitation and hole size • SO and C2S appear as the most sensitive to depletion L1498 &L1517B constant/depletion

  23. Searching for the youngest cores in L1517 N2H+

  24. Searching for the youngest cores in L1517 DSS2 red and SO(23-12) SO

  25. Summary • Dense cores • first coherent structures that form in clouds • separate from the self-similar, turbulent component • dominated by self-gravity and subsonic motions • Physical structure • flattened density profile (reminiscent BE) • temperature gradient (dust and possibly gas) • Chemical structure • inhomogeneous, differentiated, dominated by freeze out • qualitative but not quantitative agreement with models • new generation of models still needed to extract ages • Using chemistry as timer of core evolution • L1521E is consistent with being chemically young (but physics) • we have tools to search for new candidates: first fruits

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