Inga Kamp The role of the central star for the structure of protoplanetary disks
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Transcript of Inga Kamp The role of the central star for the structure of protoplanetary disks
Inga KampInga Kamp
The role of the central star for The role of the central star for the structure of the structure of
protoplanetary disksprotoplanetary disks
Peter Woitke, Wing-Fai Thi, Ian Tilling (all Edinburgh)Peter Woitke, Wing-Fai Thi, Ian Tilling (all Edinburgh)
Protoplanetary Disks and Planet Protoplanetary Disks and Planet FormationFormation
Dust dynamics are controlled by gas, even at late times !• dust substructure• dust coagulation• dust settling
[HR4796: NICMOS 1.6 mSchneider et al. 1999] 8 Myr
Jy/pixel
[Reverse ∂p/∂r at 70 AU Klahr & Lin 2001]
[Barge & Sommeria 1995, Johansen et al. 2006, 2007]
OutlineOutline
• Various planet forming environments (BD - T Tauri - Herbig)
• Second generation disk structure modeling
• How do observations inform us about the star-disk interaction ?
OutlineOutline
• Various planet forming environments (BD - T Tauri - Herbig)
• Second generation disk structure modeling
• How do observations inform us about the star-disk interaction ?
OutlineOutline
• Various planet forming environments (BD - T Tauri - Herbig)
• Second generation disk structure modeling
• How do observations inform us about the star-disk interaction ?
Protoplanetary Disk ModelsProtoplanetary Disk Models
Key astrophysical questions:
• What is the environment in which planets form ? disk structure - boundary conditions for planet formation
• Can planets form around stars different from our Sun ? star-disk interaction - impact on disk structure and dispersal
OutlineOutline
• Various planet forming environments (BD - T Tauri - Herbig)
• Second generation disk structure modeling
• How do observations inform us about the star-disk interaction ?
Disk propertiesDisk properties
[2 BDs @ 2 and 10 Myr: Sterzik et al. 2004]
[8m excess @ 5 Myr: Carpenter et al. 2006]
[Pascucci et al. 2003, Allers et al. 2006, Bouy et al. 2008]
Dust in BD disks evolves on same time scale as T Tauri disks
Inner disk clearing occurs much faster in T Tauri disks
Dust models fit BD, T Tauri and Herbig SEDs in the same wayindicating the first steps of planetesimal formation in all cases
some BD SEDs require flaring disks, others flat… low # statistics
Disk propertiesDisk properties
[Pascucci et al. 2009]
[Kessler-Silacci et al. 2007]
lower HCN/H2C2 ratios in the disks around brown dwarfsweaker and more processed silicate features
OutlineOutline
• Various planet forming environments (BD - T Tauri - Herbig)
• Second generation disk structure modeling
• How do observations inform us about the star-disk interaction ?
comparisonwith observation
radiativetransfer
Protoplanetary Disk ModelsProtoplanetary Disk Models
physical structure
chemical composition
comparisonwith observation
radiativetransfer
Protoplanetary Disk ModelsProtoplanetary Disk Models
physical structure
chemical composition
surface density = 0 (r/r0)-p
dust temperature T = T0 (r/r0)-q
disk scale height H = H0 (r/r0)-e
[e.g. Menard et al.; Pinte et al. 2006]
comparisonwith observation
radiativetransfer
Protoplanetary Disk ModelsProtoplanetary Disk Models
physical structure
chemical composition
surface density = 0 (r/r0)-p
dust temperature 2D continuum RTdisk scale height H = (cs
2 r3/GM*)0.5
[e.g. D’Alessio et al. 1998, Dullemond et al. 2002]
Gas chemical modeling on top of fixed density structure
[e.g. Aikawa et al. 2002, Semenov et al. 2008]
comparisonwith observation
line radiativetransfer
chemical composition
physical structure
Protoplanetary Disk ModelsProtoplanetary Disk Models
atomic/ionizedrich molecular chemistry
molecule freeze-out
hot flaring surface
cold midplane
[e.g. Aikawa et al. 2002, Kamp & Dullemond 2004][PPV chapters: Dullemond et al. 2007, Bergin et al. 2007]
comparisonwith observation
Protoplanetary Disk ModelsProtoplanetary Disk Models
radiativetransfer
physical structure
chemical composition
[Woitke, Kamp, Thi 2009]
ProDiMo
Similar approaches have been followed by other groups[Nomura & Millar 2005, Gorti & Hollenbach 2004, 2008]
ChemistryChemistry
nnnnknnkdtdn
ijijj
ijkijk
jikkjjk
ijki
stationary solution with modifiedNewton-Raphson algorithm (switch to time-dependant)65 species: H, H+, H-, H2, H2
+, H3+
He, He+
C, C+, CO, CO+, CO2, CO2+, HCO, HCO+, H2CO
CH, CH+, CH2, CH2+, CH3, CH3
+, CH4, CH4+, CH5
+
O, O+, O2, O2+, OH, OH+
H2O, H2O+, H3O+
N, N+, NH, NH+, NH2, NH2+, NH3, NH3
+, N2, HN2+
CN, CN+, HCN, HCN+, NO, NO+ Si, Si+, SiH, SiH+, SiO, SiO+, SiH2
+, SiOH+
S, S+, Mg, Mg+, Fe, Fe+ --> plus CO, H2O, CO2, CH4, NH3 ice
Heating and coolingHeating and cooling
photo-electric heating, PAH heating, viscous (α) heating, cosmic ray, C photo-ionisation, coll. de-excitation of H⋆
2 , H2 on grains, H2 photodissociation, IR background line heatingthermal accomodation on grains, OI, CII, CI fine-structure cooling, CO ro-vibrational (110 levels, 243 lines), o/p H2O rotational (45/45 levels, 258/257 lines), o/p H2 quadrupole (80/80 levels, 803/736 lines), SiII, SII, FeII semi-forbidden (80 levels, 477 lines), Ly α, MgII h&k, OI 6300Å
Heating
Cooling
kk (Tgas,ni) k
k (Tgas,ni)
Heating and coolingHeating and cooling
photo-electric heating, PAH heating, viscous (α) heating, cosmic ray, C photo-ionisation, coll. de-excitation of H⋆
2 , H2 on grains, H2 photodissociation, IR background line heating, (X-ray heating)thermal accomodation on grains, OI, CII, CI fine-structure cooling, CO ro-vibrational (110 levels, 243 lines), o/p H2O rotational (45/45 levels, 258/257 lines), o/p H2 quadrupole (80/80 levels, 803/736 lines), SiII, SII, FeII semi-forbidden (80 levels, 477 lines), Ly α, MgII h&k, OI 6300Å
Heating
Cooling
kk (Tgas,ni) k
k (Tgas,ni)
Protoplanetary Disk ModelsProtoplanetary Disk Models
soft inner and outer edges [Hartmann et al. 1989, Hughes et al. 2008, Woitke, Kamp & Thi 2009]
stellar UV
interstellar UV
stellar X rays
The Thermal BalanceThe Thermal Balance
stellar photonse-
e-e-
e-
small grains: a << (e.g. PAHs)yield ~ ??
large grains: a >> (micron sized)yield ??
Photoelectric heating of the gas
The Thermal BalanceThe Thermal Balance
stellar photonse-
e-e-
e-
small grains: a << (e.g. PAHs)yield ~ ??
large grains: a >> (micron sized)yield ??
Photoelectric heating of the gas
[Abbas et al. 2006]
Impact of UV IrradiationImpact of UV Irradiation
FUSE: Apr 2000 STIS: Oct 2001 May 2001 GHRS: Nov 1994
OVI
H2
HD104237
H2, CO photodissociation C ionization
Impact of UV IrradiationImpact of UV Irradiation
time
UV
exc
ess
5000 K50010 50 80
Impact of UV IrradiationImpact of UV Irradiation
time
UV
exc
ess
0 log n(OH)/n(tot)-5-14 -10
Protoplanetary Disk ModelsProtoplanetary Disk Models
soft inner and outer edges [Hartmann et al. 1989, Hughes et al. 2008, Woitke, Kamp & Thi 2009]
stellar UV
interstellar UV
stellar X rays
The Thermal BalanceThe Thermal Balance
stellar X-rays e-
e-
X-ray heating of the gas
[Glassgold et al. 2004, Meijerink et al. 2008]
TW HyaLX ~ 1030 erg/s
[Kastner et al. 1997][Nomura et al. 2007]
e-
*
Auger electrons
Secondary ionization
Primary ionization
124.0 Å 1.24 Å
*
Protoplanetary Disk ModelsProtoplanetary Disk Models
Flaring disk structure “early Sun”
M* = 1 M
L* = 1 L
Teff = 5800 KMdisk = 10-2 M
0.5-500 AU
dust:
90% Mg2SiO410% Fe0.1-10 m (2.5)
[Woitke, Kamp, Thi 2009]
X-ray source @ 20 R toirradiate disk midplane
Protoplanetary Disk ModelsProtoplanetary Disk Models
Flaring disk structure “Herbig star”
M* = 2.2 M
L* = 32 L
Teff = 8500 KMdisk = 10-2 M
0.5-500 AU
dust:
90% Mg2SiO410% Fe0.1-10 m (2.5)
T Tauri Herbig Ae
Protoplanetary Disk ModelsProtoplanetary Disk Models
Flaring disk structure “Herbig star”
M* = 2.2 M dust: L* = 32 L 90% Mg2SiO4Teff = 8500 K 10% FeMdisk = 10-2, 10-3, 10-4 M 0.05-200 m (3.5)0.5-700 AU
self-similarity
decreasing disk mass
Herbig Ae T Tauri
OutlineOutline
• Various planet forming environments (BD - T Tauri - Herbig)
• Second generation disk structure modeling
• How do observations inform us about the star-disk interaction ?
Probes of UV Irradiation: [OI], OHProbes of UV Irradiation: [OI], OH
[Bally et al. 2000, Störzer & Hollenbach 1998, Acke et al. 2005]
WFPC2
OH photodissociation layer: OH + O* + HO* denotes the 1D2 excited level (decay emits a 6300 Å photon)
460 AU
[Mandell et al. 2008, Salyk et al. 2008]
Probes of UV Irradiation: [OI], OHProbes of UV Irradiation: [OI], OH
[Bally et al. 2000, Störzer & Hollenbach 1998, Acke et al. 2005]
OH photodissociation layer: OH + O* + HO* denotes the 1D2 excited level (decay emits a 6300 Å photon)
[Mandell et al. 2008, Salyk et al. 2008]
norm
aliz
ed fl
ux
velocity [km/s]
VLT/UVES: HD97048
Probes of UV, X-ray Irradiation: CO, HProbes of UV, X-ray Irradiation: CO, H22
[Brittain et al. 2007]
Fluorescence excitation vs. thermal emission:CO UV pumping of electronic states => cascade into high v levelsH2 UV (Lyman & Werner bands) or X-rays (collisions with fast e-)
[v=1-0 S(1), S(0), v=2-1 S(1) NIR: Carmona et al. 2008]see talk by Gerrit van der Plas
Probes of UV, X-ray Irradiation: CO, HProbes of UV, X-ray Irradiation: CO, H22
[Brittain et al. 2007]
Fluorescence excitation vs. thermal emission:CO UV pumping of electronic states => cascade into high v levelsH2 UV (Lyman & Werner bands) or X-rays (collisions with fast e-)
[S(1), S(2), S(4) pure rotational MIR lines: Bitner et al. 2008]see talk by Gerrit van der Plas
Probes of X-ray Irradiation: NeIIProbes of X-ray Irradiation: NeII
[Glassgold et a. 2007, Pascucci et al. 2007, Lahuis et al. 2007, Meijerink et al. 2008]
see talk by Richard Alexander
0 50 100 150 200R (AU)
D: 13CO 3-2E: 13CO 1-0
C: 12CO 2-1H: HCO+ 4-5
H
[van Zadelhoff et al. 2001]
Probes of gas-dust decouplingProbes of gas-dust decoupling[Pietu et al. 2007]
temperatures derived from gas lines at the surface are higher than dust temperatures => support for decoupling of gas and dust in the surface layers
C
ED
[Fedele et al. 2008]
Probes of gas-dust decouplingProbes of gas-dust decoupling
dust is flat (self-shadowed) and gas is flaring=> support for decoupling of gas and dust in the surface layers
MIR dust emission
[OI] emission
GASPS: A Herschel Key programGASPS: A Herschel Key programGAS evolution in Protoplanetary Systems (PI: Dent)
~200 disks distributed over spectral type, age, and disk mass
[CII], [OI], CO and H2O lines
Aim: probe the gas mass evolution throughout the planet forming phase
line radiativetransfer
physical structure
chemical composition
comparisonwith observation
GASPS: A Herschel Key programGASPS: A Herschel Key program
Monte Carlo line radiative transfer
understand where the line originatesand then put resolution there !!
Kamp, Tilling, Woitke, Thi, Hogerheijde
[Hogerheijde, van der Tak 2000]
Key points to take homeKey points to take home
• Models predict that stellar UV and X-ray radiation shape the disk structure and chemistry and we actually observe that !
• Individual gas lines DO NOT probe total disk mass ! but we keep trying with multiple tracers …
• Gas lines DO probe the physical and chemical conditions in the region where they arise (interplay between radiative transfer and chemical structure)
and we try hard with GASPS to find the desperately wanted 10-4 M disks…
Thank You !Thank You !