AST3020. Lecture 07 Migration type I, II, III Talk by Sherry on migration Ups And and the need for disk-planet interaction during the formation of multiplanetary systems Torques and migration type I Numerical calculations of gap opening
01 / 97AST3020. Lecture 07 Migration type I, II, III Talk by Sherry on migration
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AST3020. Lecture 07 Migration type I, II, III Talk by Sherry on migration
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AST3020. Lecture 07 Migration type I, II, III Talk by Sherry on migration Ups And and the need for disk-planet interaction during the formationof multiplanetary systems Torques and migration type I Numerical calculations of gap opening and type II situation, as well as fast migration Test problem and difference between codes Last Mohican scenario and the viability of Earths
Classical celestial mechanics In the secular pertubation theory, semi-major axes (energies) are constant (as a result of averaging over time). Eccentricities and orbit misalignment vary, such as to conserve the angular momentum and energy of the system. We will show sets of thin theoretical curves for (e2, dw). [There are corresponding (e3, dw) curves, as well.] Thick lines are numerically computed full N-body trajectories.
N-body (planet-planet) or disk-planet interaction? Conclusions from modeling Ups And 1. Secular perturbation theory and numerical calculations spanning 2 Gyr in agreement. 2. The apsidal “resonance” (co-evolution) is expected and observed to be strong, and stabilizes the system of two nearby, massive planets 3. There are no mean motion resonances 4. The present state lasted since formation period 5. Eccentricities in inverse relation to masses, contrary to normal N-body trend tendency for equipartition. Alternative: a lost most massive planet - very unlikely 6. Origin still studied, Lin et al. Developed first models involving time-dependent axisymmetric disk potential
Diversity of exoplanetary systems likely a result of: cores? disk-planet interaction a m e (only medium) yes planet-planet interaction a m? e yes star-planet interaction a m e? yes disk breakup (fragmentation into GGP) a m e? Metallicity no X X X X X X X X
. . . SPH (Smoothed Particle Hydrodynamics) Jupiter in a solar nebula (z/r=0.02) launches waves at LRs. The two views are (left) Cartesian, and (right) polar coordinates.
A gap-opening body in a disk: Saturn rings, Keeler gap region (width =35 km) This new 7-km satellite of Saturn was announced 11 May 2005. To Saturn
Migration Type I : embedded in fluid Migration Type II : more in the open (gap)
Illustration of nominal positions of Lindblad resonances (obtained by WKB approximation. The nominal positions coincide with the mean motion resonances of the type m:(m+-1) in celestial mechanics, which doesn’t include pressure.) Nominal radii converge toward the planet’s semi-major axis at high azimuthal numbers m, causing problems with torque calculation (infinities!). On the other hand, the pressure-shifted positions are the effective LR positions, shown by the green arrows. They yield finite total LR torque.
Wave excitation at Lindblad resonances (roughly speaking, places in disk in mean motion resonance, or commensurability of periods, with the perturbing planet) is the basis of the calculation of torques (and energy transfer) between the perturber and the disk. Finding precise locations of LRs is thus a prerequisite for computing the orbital evolution of a satellite or planet interacting with a disk. LR locations can be found by setting radial wave number k_r = 0 in dispersion relation of small-amplitude, m-armed, waves in a disk. [Wave vector has radial component k_r and azimuthal component k_theta = m/r] This location corresponds to a boundary between the wavy and the evanescent regions of a disk. Radial wavelength, 2*pi/k_r, becomes formally infinite at LR.
Eccentricity in type-I situation is always strongly damped. Eccentricity pumping --> m(z/r)
Migration Type I : embedded in fluid Migration Type II : in the open (gap) Migration Type III partially open (gap)
Migration Type I, II, and III Underlying fig. from: “Protostars and Planets IV (2000)”; cf. “Protostars and Planets V (2006)” & this talk for type III data ? type III Time-scale (years)