scholarly journals On the Importance of Wave–Planet Interactions for the Migration of Two Super-Earths Embedded in a Protoplanetary Disk

2021 ◽  
Vol 921 (2) ◽  
pp. 142
Author(s):  
Zijia Cui ◽  
John C. B. Papaloizou ◽  
Ewa Szuszkiewicz
Keyword(s):  
2018 ◽  
Vol 14 (S345) ◽  
pp. 351-352
Author(s):  
Ernst A. Dorfi ◽  
Florian Ragossnig

AbstractDuring the early stages of planet formation accretion of small bodies add mass to the planet and deposit their energy kinetic energy. Caused by frictional heating and/or large stagnation pressures within the dense and extended atmospheres most of the in-falling bodies get destroyed by melting or break-up before they impact on the planet’s surface. The energy is added to the atmospheric layers rather than heating the planet directly. These processes can significantly alter the physical properties of protoplanets before they are exposed with their primordial atmospheres to the early stellar source when the protoplanetary disk becomes evaporated.


Science ◽  
2007 ◽  
Vol 316 (5828) ◽  
pp. 1178-1181 ◽  
Author(s):  
M. Bizzarro ◽  
D. Ulfbeck ◽  
A. Trinquier ◽  
K. Thrane ◽  
J. N. Connelly ◽  
...  
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2017 ◽  
Vol 52 (9) ◽  
pp. 1797-1821 ◽  
Author(s):  
Conel M. O'D. Alexander ◽  
Larry R. Nittler ◽  
Jemma Davidson ◽  
Fred J. Ciesla
Keyword(s):  

2014 ◽  
Vol 9 (S310) ◽  
pp. 194-203 ◽  
Author(s):  
Sean N. Raymond ◽  
Alessandro Morbidelli

AbstractThe “Grand Tack” model proposes that the inner Solar System was sculpted by the giant planets' orbital migration in the gaseous protoplanetary disk. Jupiter first migrated inward then Jupiter and Saturn migrated back outward together. If Jupiter's turnaround or “tack” point was at ~ 1.5 AU the inner disk of terrestrial building blocks would have been truncated at ~ 1 AU, naturally producing the terrestrial planets' masses and spacing. During the gas giants' migration the asteroid belt is severely depleted but repopulated by distinct planetesimal reservoirs that can be associated with the present-day S and C types. The giant planets' orbits are consistent with the later evolution of the outer Solar System.Here we confront common criticisms of the Grand Tack model. We show that some uncertainties remain regarding the Tack mechanism itself; the most critical unknown is the timing and rate of gas accretion onto Saturn and Jupiter. Current isotopic and compositional measurements of Solar System bodies – including the D/H ratios of Saturn's satellites – do not refute the model. We discuss how alternate models for the formation of the terrestrial planets each suffer from an internal inconsistency and/or place a strong and very specific requirement on the properties of the protoplanetary disk.We conclude that the Grand Tack model remains viable and consistent with our current understanding of planet formation. Nonetheless, we encourage additional tests of the Grand Tack as well as the construction of alternate models.


2008 ◽  
Vol 680 (2) ◽  
pp. L141-L144 ◽  
Author(s):  
Kristine Thrane ◽  
Kazuhide Nagashima ◽  
Alexander N. Krot ◽  
Martin Bizzarro

2018 ◽  
Vol 860 (1) ◽  
pp. 82 ◽  
Author(s):  
Charles L. H. Hull ◽  
Haifeng Yang ◽  
Zhi-Yun Li ◽  
Akimasa Kataoka ◽  
Ian W. Stephens ◽  
...  
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2015 ◽  
Vol 809 (2) ◽  
pp. L26 ◽  
Author(s):  
Jane Huang ◽  
Karin I. Öberg
Keyword(s):  

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