TY - JOUR
T1 - Fossilized condensation lines in the Solar System protoplanetary disk
AU - Morbidelli, A.
AU - Bitsch, B.
AU - Crida, A.
AU - Gounelle, M.
AU - Guillot, T.
AU - Jacobson, S.
AU - Johansen, A.
AU - Lambrechts, M.
AU - Lega, E.
N1 - Funding Information:
We acknowledge support by the French ANR , project number ANR-13-13-BS05-0003-01 projet MOJO (Modeling the Origin of JOvian planets). A.J. is grateful for the financial support from the European Research Council (ERC Starting Grant 278675-PEBBLE2PLANET ) and the Swedish Research Council (Grant 2014-5775 ). A.J. and B.B. thank the Knut and Alice Wallenberg Foundation for their financial support. S.J. was supported by the European Research Council (ERC) Advanced Grant ACCRETE (contract number 290568 ). We are grateful to C. Dullemond and an anonymous reviewer for their constructive reviews.
Publisher Copyright:
© 2015 The Authors.
PY - 2016/3/15
Y1 - 2016/3/15
N2 - The terrestrial planets and the asteroids dominant in the inner asteroid belt are water poor. However, in the protoplanetary disk the temperature should have decreased below water-condensation level well before the disk was photo-evaporated. Thus, the global water depletion of the inner Solar System is puzzling. We show that, even if the inner disk becomes cold, there cannot be direct condensation of water. This is because the snowline moves towards the Sun more slowly than the gas itself. Thus the gas in the vicinity of the snowline always comes from farther out, where it should have already condensed, and therefore it should be dry. The appearance of ice in a range of heliocentric distances swept by the snowline can only be due to the radial drift of icy particles from the outer disk. However, if a planet with a mass larger than 20 Earth mass is present, the radial drift of particles is interrupted, because such a planet gives the disk a super-Keplerian rotation just outside of its own orbit. From this result, we propose that the precursor of Jupiter achieved this threshold mass when the snowline was still around 3 AU. This effectively fossilized the snowline at that location. In fact, even if it cooled later, the disk inside of Jupiter's orbit remained ice-depleted because the flow of icy particles from the outer system was intercepted by the planet. This scenario predicts that planetary systems without giant planets should be much more rich in water in their inner regions than our system. We also show that the inner edge of the planetesimal disk at 0.7 AU, required in terrestrial planet formation models to explain the small mass of Mercury and the absence of planets inside of its orbit, could be due to the silicate condensation line, fossilized at the end of the phase of streaming instability that generated the planetesimal seeds. Thus, when the disk cooled, silicate particles started to drift inwards of 0.7. AU without being sublimated, but they could not be accreted by any pre-existing planetesimals.
AB - The terrestrial planets and the asteroids dominant in the inner asteroid belt are water poor. However, in the protoplanetary disk the temperature should have decreased below water-condensation level well before the disk was photo-evaporated. Thus, the global water depletion of the inner Solar System is puzzling. We show that, even if the inner disk becomes cold, there cannot be direct condensation of water. This is because the snowline moves towards the Sun more slowly than the gas itself. Thus the gas in the vicinity of the snowline always comes from farther out, where it should have already condensed, and therefore it should be dry. The appearance of ice in a range of heliocentric distances swept by the snowline can only be due to the radial drift of icy particles from the outer disk. However, if a planet with a mass larger than 20 Earth mass is present, the radial drift of particles is interrupted, because such a planet gives the disk a super-Keplerian rotation just outside of its own orbit. From this result, we propose that the precursor of Jupiter achieved this threshold mass when the snowline was still around 3 AU. This effectively fossilized the snowline at that location. In fact, even if it cooled later, the disk inside of Jupiter's orbit remained ice-depleted because the flow of icy particles from the outer system was intercepted by the planet. This scenario predicts that planetary systems without giant planets should be much more rich in water in their inner regions than our system. We also show that the inner edge of the planetesimal disk at 0.7 AU, required in terrestrial planet formation models to explain the small mass of Mercury and the absence of planets inside of its orbit, could be due to the silicate condensation line, fossilized at the end of the phase of streaming instability that generated the planetesimal seeds. Thus, when the disk cooled, silicate particles started to drift inwards of 0.7. AU without being sublimated, but they could not be accreted by any pre-existing planetesimals.
KW - Cosmochemistry
KW - Origin, Solar System
KW - Planetesimals
KW - Solar Nebula
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U2 - 10.1016/j.icarus.2015.11.027
DO - 10.1016/j.icarus.2015.11.027
M3 - Article
AN - SCOPUS:84955092255
SN - 0019-1035
VL - 267
SP - 368
EP - 376
JO - Icarus
JF - Icarus
ER -