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Observational Constraints on the Formation and Properties of Giant Planets Jeff Valenti. Road Map for the Talk. Orbital Properties of Planets Observed Planet-Metallicity Relationship Two competing planet formation theories We measured lots of stellar abundances
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Observational Constraints on the Formation and Properties of Giant PlanetsJeff Valenti
Road Map for the Talk • Orbital Properties of Planets • Observed Planet-Metallicity Relationship • Two competing planet formation theories • We measured lots of stellar abundances • Higher metallicity stars have more detected planets! • Not caused by accretion of rocky debris • Timescale for Building Gas Giant Planets • Our HST detection of hot H2 • Characterizing Transiting Planets • My HST program to observe an evaporating exosphere • JWST spectra of atmospheric absorption and emission
Planet Discovery N2K, Ge PLANET consortium SWEEPS, XO
Planets Migrate! “Snow Line” Pile-up at P=3 days http://exoplanets.org/a_hist.gif
Disk is Truncated by Stellar Magnetosphere Milky Way & Cookies Monday, April 3 Shu et al. (1994)
Two Theories of Planet Formation Metals: 0.1 nm Core-Accretion Dust: 1 nm – 1 mm Planetesimals: 1 mm – 1 km Cores: 1 km – 1 Mm Do Metals Matter ? crit nH Planets : 1 Mm – 0.1 Gm Gravitational Instability
Spectroscopic Analysis Tool • SME - “Spectroscopy Made Easy” • Valenti & Piskunov (1996, A&AS, 118, 595) • Publicly available • Radiative transfer code [with Nikolai Piskunov] • LTE, Feautrier solver, Adaptive λ grid, C++ • Chemical equilibrium for over 150 molecules (NextGen EOS) • Fit observed spectrum with synthetic spectrum • Use precise atomic data from solar spectrum fit • Interpolate Kurucz atmospheres in Teff, logg, and [M/H] • Calculate synthetic intensities across the stellar surface • Integrate over stellar surface: rotation and RT macroturbulence • Non-linear least squares solver (Levenberg-Marquardt) • Free parameters: log(gf), Teff, logg, [M/H], etc.
Determining Spectroscopic Properties Segment #1 Segment #2 Valenti & Fischer (2005)
Stellar Macroturbulence Valenti & Fischer (2005)
Isochrone Analysis 1040 Stars T, L, Fe, M, R, age
Spectroscopic Properties of Cool Stars • Valenti & Fischer (2005, ApJS, 159, 141) • 1807 observed spectra (6 CPU months) • 1040 nearby dwarfs and subgiants • N2K: 410 Keck + 400 Subaru + 270 Magellan spectra analyzed • Properties based on fitting spectra • Effective temperature (1%) • Surface gravity (15%) • Rotational velocity (0.5 km/s) • Abundances: Na, Si, Ti, Fe, Ni (5-10%) • Properties based on matching evolutionary models • Stellar mass (15%) • Radius (3%) • Age constraints
p = (10[Fe/H]) = (N(Fe) M) = (4.5 ± 0.8)% = (1.8 ± 0.3) N(Fe) M Quadratic Dependence on Stellar Metals Increasing metals by 40% doubles the number of stars with planets Fischer & Valenti (2005)
Dependence on Stellar Mass? Fischer & Valenti (2005) Cooler Stars Metallicity bias…
0.6 0.4 0.2 [M/H] 0.0 -0.2 -0.4 -0.6 6500 6000 5500 5000 TEFF (K) Does Accretion Cause Planet-Metallicity Relationship? Pinsonneault, De Poy, & Coffee (2001) 1 M Stars with Planets
0.0 2.0 Mbol 4.0 6.0 8.0 6500 6000 5500 5000 TEFF (K) Subgiants with and without Planets Subgiants Planets
0.6 0.2 [Fe/H] -0.2 -0.6 6500 6000 5500 5000 4500 TEFF (K) Subgiant Test – No Diluted Enrichment Subgiants with planets are still metal rich [Fe/H]=0.15
Line Depths NOT Proportional to Abundance Strong Lines are Saturated
Stars with Distant Planets Seem To Be Metal Rich Statistics are improving where giant planets form. 3% of Keck sample has long period planets
Next Step: Detection Limits for Each Star Adapted from Cumming (2004, MNRAS, 354, 1165) P < 4 yr FV05 N=15 N=30 K > 30 m/s 30 m/s p=99% p=50%
Classical Core-Accretion Model Is Slow Pollack et al. (1996) Phase I Core formation via rapid accretion of planetesimals in “feeding zone” Phase III Giant planet formation via rapid gas accretion Phase II Envelope formation via gradual gas accretion Core + Envelope Core Only Isolation Mass
Dust Near a Star Dissipates Quickly Warm dust only lasts “a few Myr” How long does the gas last? Haisch, Lada, & Lada (2001)
Hot Inner Edge(s) of Disks SU Aur RY Tau Akeson et al. (2006)
Molecular Hydrogen in Accretion Disks Herczeg et al. (2002; 2004; 2005)
Ly- Pumped Fluorescence of Hot H2 Herczeg et al. (2004)
Ly- Pumped Fluorescence of Hot H2 Herczeg et al. (2004)
Comparative Planetology • Find planets that transit bright (V<12) stars • Absorption by planetary atmosphere during transit • Thermal emission in and out of secondary eclipse • 1)HD209458b, 2) TrES-1, 3) HD189733b, 4)HD149026b • N2K Survey • Fischer (SFSU), Laughlin (UCSC), Valenti (STScI), … • Surveying the “next 2000” stars, V<10.5 (14,000 candidates) • Constructed metal-rich sample using photometric indexes • “Three strikes and you’re out!” - focus on short periods • So far: 410 Keck + 400 Subaru + 270 Magellan stars • So far: 7 planets announced + 3 in press + 36 candidates • So far: 1 new transiting planet!
HD 149026 40 Velocity (m/s) 0 –40 Subaru&Keck –0.5 0.0 0.5 Orbital Phase “N2K” Discovers Its First Transiting Planet! Sato et al. (2006)
Diversity of Planets - Formation vs. Evolution Evaporating Exosphere Program 10718 Bouchy et al. (2005)
Evaporating Exospheres Vidal Madjar et al. (2003)
Planetary Transits with JWST/NIRSpec R=3000 Brown (1991)
Planetary Eclipses with JWST/NIRSpec R=3000 Spitzer
Key Results • Spectroscopic Properties of Cool Stars (SPOCS) • 1040 solar-type stars in Keck, Lick, AAT planet search programs • Analyzing another 2000 stars in N2K program • Quantified Planet-Metallicity Relationship • Increasing metals by 40% doubles the number of stars with planets • Not due to preferential accretion of metals onto star • Inconsistent with gravitational instability (migration?) • Fundamental constraint on all formation models • HST andJWST will characterize disks and atmospheres • Use fluoresced H2 to study gas in protoplanetary disks • Measure extent of planetary exosphere during transit • Obtain atmospheric absorption spectra during transit • Measure thermal emission spectra in/out of secondary eclipse