Minimum Mass Solar Nebulae

Minimum Mass Solar Nebulae

Minimum Mass Solar Nebulae, Nice model, & Planetary Migration. Aurélien CRIDA 1) MMSN : definition, recipe Minimum Mass Solar Nebula Little reminder : It is not a nebula, but a protoplanetary disc. Solar : from which the Solar System is born. Minimum Mass : just enough solid material to build the 8 planets. Importance : Density used in basically all processes of planet formation. A. Crida Tübingen, 5/3/2009 1) MMSN : definition, recipe Recipe of the Minimum Mass Solar Nebula Ingredients for 8 planets : ~ 60 Earth masses of solids (chondritic composition). ~ 0.01 solar mass of the famous mixture H (75%), He (25%). Preparation : Spread the appropriate mass of solids around the orbit of each planet. Multiply the obtained density by 100 (add gas). Cover with a power law profile. Dispose around the Sun for 10 million years. You get the Solar System. Enjoy ! A. Crida Tübingen, 5/3/2009 1) MMSN : definition, recipe Weidenschilling (1977), Hayashi (1981) : − 1.5 r -2 Σ ( r ) = 1700 g.cm 1AU Main assumptions : The planets accreted all the solids (therefore «minimum»). They formed where they presently orbit. ... did they ? A. Crida Tübingen, 5/3/2009 2) The Nice model After the protoplanetary disc dispersal, the giant planets were on circular orbits, in a compact configuration, surrounded by a disc of planetesimals. (Gomes et al. 2005 ; Tsiganis et al, 2005) Planetesimal scattering perturbs the orbits of the planets. When Jupiter and Saturn reach their 2:1 resonance, the system is destabilized : → Late Heavy Bombardement. → The planets reach their present orbits. A. Crida Tübingen, 5/3/2009 2) The Nice model The Nice model explains : The eccentricities of the giants the Late Heavy Bombardement. Time [years] A. Crida Tübingen, 5/3/2009 2) The Nice model The Nice model explains : And also : The eccentricities of the giants ✔ The capture of Jupiter's the Late Heavy Bombardement. Trojans on inclined orbits (Morbidelli et al, 2005). ✔ The Hildas and D-type asteroids (Bottke et al, 08). ✔ The capture of the irregular satellites by the giants (Nesvorny et al, 2007). ✔ The Kuiper Belt architec- ture (Levison et al, 2007). A. Crida Tübingen, 5/3/2009 3) Return of the MMSN If the Nice model holds, the giant planets didn't form where they now orbit. After the gas disc phase, they were located at : Jupiter : 5,45 AU ; Saturn : ~8,2 AU ; Neptune: 11-12 AU ; Uranus: 14-17 AU. Then, the Hayashi density profile is out of date. Desch applied the recipe with these positions (and improved the cooking). A. Crida Tübingen, 5/3/2009 3) Return of the MMSN Desch (2007) : a MMSN based on the Nice model - Compact configuration, - Uranus ↔ Neptune, - Disc of planetesimals, → Excellent fit with : r − 2.168 Σ(r) = 50500 g.cm-2 1AU 10 times more dense at 5 AU than Hayashi's MMSN. Much steeper slope. A. Crida Tübingen, 5/3/2009 Migration, did you say migration ? The orbital radius may change through 3 different processes : ● Small size bodies (<km) : radial drift (or type 0) through gas drag. ● Planets in a gaseous disc : migration (type I, II, III) through tidal interaction (this session). ● Planets after the gas disc : discontinuous change through scattering (ex: in the Nice model). None is taken into account in the Hayashi (1981) MMSN. Only the 3rd one is considered in the Desch (2007) MMSN. How about migration inside the MMSN ? A. Crida Tübingen, 5/3/2009 4) Migration strikes back Jupiter, Saturn, Neptune & Uranus in Desch (2007) disc. 100 Jupiter orbits on a fixed orbit, then released. Jupiter: runaway, Uranus type III migration, lost. Neptune Saturn : type I, then type III Saturn migration, lost. Jupiter Neptune : type I, lost. Uranus : type I, lost. A. Crida Tübingen, 5/3/2009 4) Migration strikes back Jupiter, Saturn, Neptune & Uranus in Desch (2007) disc. Non localy isothermal EOS: viscous heating, radiative cooling. Jupiter: runaway, 14 Uranus type III migration, 12 Neptune lost. 10 Saturn, Neptune, Saturn This is the case Uranus, lost. 8 for any disc, 6 Jupiter insn't it ? The planets can't survive more 4 than 20 000 yrs. semi major [AU]axis 2 ( Crida, 2009, 0 0 2000 16000 ApJ, submitted) time [years] A. Crida Tübingen, 5/3/2009 4) Migration strikes back Jupiter & Saturn in Hayashi (1981) density profile, with same H/r, α as in Desch (2007), localy isothermal EOS. 10 Saturn 9 Sa No type III, no runaway. 8 7 Jupiter, Saturn enter in 3:2 6 mean motion resonance, 5 Jupiter semi major [AU]axis and stop ! 4 0 104 3.5x104 time [years] A. Crida Tübingen, 5/3/2009 4) Migration strikes back Jupiter, Saturn, Neptune & Uranus in Hayashi (1981) disc. On longer term, with other disc parameters : Jupiter-Saturn: 30 Neptune in resonance, Masset & Snellgrove (2001) stop. 25 Morbidelli & Crida (2007) Neptune,Uranus, 20 Uranus also caught in resonance, after 15 Saturn type I migration. 10 5 ( Crida, 2009, semi major [AU]axis Jupiter ApJ, submitted) 0 0 104 time [years] 105 A. Crida Tübingen, 5/3/2009 5) A new hope Morbidelli et al. (2007) : 6 possible resonant confi- gurations in the gas disc. 2 are stable over 108-9 yrs without gas disc. With a planetesimals disc, a (late) global instability can take place. This is the « Nice model II ». A. Crida Tübingen, 5/3/2009 CONCLUSION Neither the standard MMSN (Hayashi, 1981), nor the newer one (Desch, 2007), are consistent with planetary migration. In a very dense disc, the giants can't survive (runaway migration of Jupiter and Saturn, no resonance). Formation of the giant planets over a wide radial range, in a low density disc, then, migration, approach, and resonances, then, Nice model II. Radial drift and migration make the recipe of the MMSN irrelevant. A. Crida Tübingen, 5/3/2009 .

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