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This symposium summary covers various aspects of the disk accretion phase, including its ubiquity among stars, lifetimes, mass estimates, sizes, accretion rates, presence of larger bodies, and its role in diagnosing forming planets. The summary also discusses the debris disk phase and explores imaging techniques, radial distribution of dust, and spectroscopic searches for disk gas.
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GILLETT SYMPOSIUM SUMMARY 11- 13 April, 2002 Stephen E. Strom
Disk Accretion Phase: Ubiquity • 100% for stars with M < 1 MO (observed) • 100% for higher mass stars (inferred) • Collimated jets • Evidence for ‘funnel flows’ • Rotational properties • J/M vs M is continuous • Accretion through disks enables assembly • Radiation pressure would otherwise reverse accretion
Disk Accretion Phase: Lifetimes • 0.1 < t < 10 Myr for solar-type stars • Upper limit not well established • Environment may affect lifetimes • Photoevaporation; tidal interactions • 0.1 <t < ? Myr for higher mass stars • Disk lifetimes are shorter than for 1 MO stars • Stellar rotation provides additional clues • N(vsini) for a Per requires disk lifetimes up to ~5 Myr • Rotation rates higher in high density regions • Shorter disk lifetimes? Higher accretion rates? • Caveat: PMS ages are highly uncertain for t < 3 Myr • Tracks • Birthline • Uncertainties in L, Teff
Disk Accretion Phase: Masses • Total mass estimates based on dust mass • mm continuum emission • Range: Mdust ~ 10-3 to 10-5 MO • These are lower limits • Mass int > 1 regions underestimated • Large bodies not detected • Mass estimates depend on (uncertain) grain properties • No reliable estimates of gas content • The total mass available for planet building may well exceed the “minimum mass nebula” • Mass comprising star passes through a disk • Instantaneous disk mass is a lower limit
Disk Accretion Phase: Sizes • Largest centrifugally supported disks: ~ 300 AU • Larger, structures found, but no evidence of rotational support • Orion silhouette disks provide direct measurement • 20 < r < 200 AU (~ 50 disks) • Photo-evaporation and tidal encounters may truncate disks in rich, dense environments • Correlation between disk size and proximity to q Ori • Kuiper belt cutoff may reflect photo-evaporation (Hollenbach)
Disk Accretion Phase: Accretion Rates • Estimated from ultraviolet excess emission • Measures inner disk accretion rate • dM/dt increases with increasing mass • dM/dt ~ 10-7.5 for 0.5 MO; may increase ~ linearly with M • Instantaneous rates are lower than time-averaged rates • Accretion rates ~103 higher during FU Ori phase • Recall that total mass passing through the disk is large • Wide dispersion (> 10x) in dM/dt at fixed age and mass • Q: might this dispersion reflect the effects of planets? • Binarity and tidal encounters may affect dM/dt
Disk Accretion Phase: Larger Bodies • Growth of grains (to 1 cm) estimated from SEDs • Presence of larger bodies inferred from • FEBs (but cf Grady: now suggests accretion origin in HAeS) • Cyrstalline silicate emission in cold disk regions (?) • Evidence favors planet formation during accretion phase • N(a) for extrasolar planets suggests accretion-driven migration • Best (only?) time to form gas giants • Large O/IR telescopes and later, ALMA, should enable detection of ‘gaps’ diagnostic of forming giant planets • Establish the fraction of stars that form giant planets initially • Establish the N(a) during the accretion phase • Is there an (interesting) upper limit to a ?
GSMT AURA-NIO Point Design
ALMA Star at 10pc
Debris Disk Phase • Sparsely-sampled photometry and SEDs • Statistics: <t>, s (t) vs age • Radial distribution t (r) , (if SED is well sampled) • mineralogical probes • Statistical studies suggest • Decrease of t with age (Ldust/ L* ~ t -1.75) • Possible rapid decline of t for stars with ages t > 400 Myr • Radial distributions: low t inner zones • Mineralogy • Solid state features can in principle be matched to source bodies
Debris Disk Phase • Caveat regarding ages • Transformation to L,Teff a problem for t < 200 Myr • Large starspots + photosphere = composite spectral type • Cluster ages (t < 200 Myr) are uncertain at 0.3 dex level • Li-depletion ages • Systematic difference with upper MS turnoff • Rotation affects surface Li • Efficacious for selected spectral type ranges only • Activity-age estimates (e.g. Ca II) • Large dispersion • Conclude (Stauffer): • Relative age uncertainties for field stars up to 0.6 dex
Debris Disk Phase • Imaging: scattered light; thermal IR; mm • Radial distribution of dust • Selected cases reveal (cf Alycia Weinberger) • Low density inner zones • Warps • Rings • Non-axisymetric features • Q: do these provide evidence of planets? • Modeling suggests yes • Analysis of solar system zodi strongly supportive
Debris Disk Phase • Spectroscopic searches for disk gas (steady state) • CO emission (mm-wave measurements) • H2 infrared features (ISO; ground) • H2; CO ultraviolet absorption features • Results • Significant differences between (uv; ground) and ISO • Concensus: [gas/dust] << ISM value • Not enough to build giant planets • Could mitigate dust migration; quantitative study needed • Suggestion that gas is ‘secondary’: evaporated volatiles • High priority for future work • SIRTF observations of H2 spanning wide age range • Knowledge of gas content key to modeling dust evolution • Key Focus: young (5 – 20 Myr) debris disk stars • Do post-accretion phase disks have gas sufficient to build giant planets?
Debris Disk Phase • Spectroscopic monitoring (time variable) • Episodic red-shifted absorption features from metals • Suggest presence of ‘falling, evaporating bodies’ • Limited results suggest origin in refractory bodies
Debris Disk Phase: The Future • SEDs from SIRTF • Well sampled from 3m – 160m • Diagnose t ( r ); infer presence of gaps • Mineralogical features: probe parent body composition • observe transition from ISM to debris-dominated disks • High angular resolution imaging from the ground • Map solid and gaseous components at sub-AU scales
Debris Disk Phase: Solar System Clues • Sources of dust: collisions • Outer solar system: Kuiper Belt objects • Inner solar system: Asteroid Belt objects • In both cases, orbits are ‘stirred’ by planets • Observed disk properties; evolution depend on • Planetesimal/cometesimal distribution; initial density • Planetary architecture • Effects of gravitational and drag forces • Warps; rings; offsets in zodi dust linked to planets • Density enhancements caused by resonant trapping
Debris Disk Phase: Solar System Clues • Dust injection into zodiacal cloud stochastic • Expect large variations in t • Large collisions may give rise to ‘dust waves’ • Timescales ~ 104.5 to 106 yrs • Possible significant climatic consequences • Kuiper belt primordial mass: > 10-4 MO • KB extends S ( r ) from inner solar system to > 100? AU • Slow Collisions produce 100-1000km bodies in ~ 100Myr • Fast Collisions erode initial KBOs • Produce dust (observed by Pioneer?); comets • Total KB mass has likely decreased 1000-fold over 5 Gyr • KB probably similar to outer regions of extrasolar disks
Extrasolar Planetary Systems • (Jovian) planet detection rate ~ 10% • Of these, multiple planet systems common (> 50%) • Unexpected distribution of a for giant planets • N(a) distribution suggests migration • What stops migration (cf Artymowicz)? • Favors formation during accretion phase • Stars with inner Jupiters may have higher Z • Caveats • N(a) suffers from strong observational bias • High M sini favored by Doppler techniques • Consistent analysis of metallicities is critical (underway) • Focus on F stars (thinner convection zones)
GSMT: www.aura-nio.noao.edu AURA-NIO Concept Direct detection with ExAO GSMT enables direct detection and analysis of planets
Debris Disks and the Formation of Planets A true celebration of Fred Gillett whose Insight Imagination Persistence Care Integrity Decency Generosity of spirit Sense of community are a continuing inspiration to us all