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Accretion disks that become gravitationally unstable can fragment into stellar or sub-stellar companions. The formation and survival of these fragments depends on the precarious balance between self-gravity, internal pressure, tidal…

Solar and Stellar Astrophysics · Physics 2015-05-28 Kaitlin M. Kratter , Ruth A. Murray-Clay

The observation of pits at the surface of comets offers the opportunity to take a glimpse into the properties and the mechanisms that shape a nucleus through cometary activity. If the origin of these pits is still a matter of debate,…

The evolution of thousands of orbits of Jupiter-family comets and asteroids under the gravitational influence of planets was calculated. Comparison of the results obtained by a symplectic method with those obtained by direct integration…

Astrophysics · Physics 2011-04-12 S. I. Ipatov

Rapid orbital drift of macroscopic dust particles is one of the major obstacles against planetesimal formation in protoplanetary disks. We reexamine this problem by considering porosity evolution of dust aggregates. We apply a porosity…

Earth and Planetary Astrophysics · Physics 2015-06-04 Satoshi Okuzumi , Hidekazu Tanaka , Hiroshi Kobayashi , Koji Wada

Quasiperiodic eruptions (QPEs), the repeated outbursts observed in soft X-ray bands, have attracted broad interest, but their physical origin is under debate. One of the popular models, the star-disk collision model, suggests that QPEs can…

High Energy Astrophysical Phenomena · Physics 2026-01-27 Wenyuan Guo , Rong-Feng Shen

Probabilities of collisions of migrating small bodies and dust particles produced by these bodies with planets were studied. Various Jupiter-family comets, Halley-type comets, long-period comets, trans-Neptunian objects, and asteroids were…

Earth and Planetary Astrophysics · Physics 2011-01-04 S. I. Ipatov

The formation of chondrules is one of the oldest unsolved mysteries in meteoritics and planet formation. Recently an old idea has been revived: the idea that chondrules form as a result of collisions between planetesimals in which the…

Earth and Planetary Astrophysics · Physics 2015-01-26 Cornelis Petrus Dullemond , Sebastian Markus Stammler , Anders Johansen

One of the main aims of the ESA Rosetta mission is to study the origin of the solar system by exploring comet 67P/Churyumov-Gerasimenko at close range. In this paper we discuss the origin and evolution of comet 67P/Churyumov-Gerasimenko in…

We investigate the outcomes of collisions between Mars-sized bodies through smooth particle hydrodynamics (SPH) simulations, focusing on the transitions among ``merging'', ``hit-and-run'', and catastrophic disruption. By systematically…

Earth and Planetary Astrophysics · Physics 2025-12-18 Hiroshi Kobayashi , Hidekazu Tanaka , Yukihiko Hasegawa , Shu-ichiro Inutsuka

Understanding the geological modification processes on asteroids can provide information concerning their surface history. Images of small asteroids from spacecraft show a depletion in terms of smaller craters. Seismic shaking was…

The large scale structure of the Solar System has been shaped by a transient dynamical instability that may have been triggered by the interaction of the giants planets with a massive primordial disk of icy debris. In this work, we…

Earth and Planetary Astrophysics · Physics 2021-08-18 Marvin Morgan , Darryl Seligman , Konstantin Batygin

The origin of close-in giant planets is a key open question in planet formation theory. The two leading models are (i) formation at the outer disk followed by migration and (ii) in situ formation. In this work we determine the atmospheric…

Earth and Planetary Astrophysics · Physics 2022-10-07 Henrik Knierim , Sho Shibata , Ravit Helled

Over the course of the recent decades, $N$-body simulations have become a standard tool for quantifying the gravitational perturbations that ensue in planet-forming disks. Within the context of such simulations, massive non-central bodies…

Earth and Planetary Astrophysics · Physics 2020-08-12 Shirui Peng , Konstantin Batygin

Pebble accretion is a new mechanism to quickly grow the cores of planets. In pebble accretion, gravity and gas drag conspire to yield large collisional cross sections for small particles in protoplanetary disks. However, before pebble…

Earth and Planetary Astrophysics · Physics 2016-02-03 Rico G. Visser , Chris W. Ormel

The scattering of small bodies by planets is an important dynamical process in planetary systems. We present an analytical model to describe this process using the simplifying assumption that each particle's dynamics is dominated by a…

Earth and Planetary Astrophysics · Physics 2015-06-03 A. Bonsor , M. C. Wyatt

Formation of bodies near the deuterium-burning limit is considered by detailed numerical simulations according to the core-nucleated giant planet accretion scenario. The objects, with heavy-element cores in the range 5-30 Mearth, are…

Earth and Planetary Astrophysics · Physics 2013-06-07 Peter Bodenheimer , Gennaro D'Angelo , Jack J. Lissauer , Jonathan J. Fortney , Didier Saumon

Most major planetary bodies in the solar system rotate in the same direction as their orbital motion: their spin is prograde. Theoretical studies to explain the direction as well as the magnitude of the spin vector have had mixed success.…

Earth and Planetary Astrophysics · Physics 2019-09-25 R. G. Visser , C. W. Ormel , C. Dominik , S. Ida

Context: Sticking of colliding dust particles through van der Waals forces is the first stage in the grain growth process in protoplanetary disks, eventually leading to the formation of comets, asteroids and planets. A key aspect of the…

Astrophysics · Physics 2009-11-11 C. W. Ormel , M. Spaans , A. G. G. M. Tielens

Context. The composition of a protoplanetary disk at a given location does not only depend on temperature and pressure but also on the time dependent transport of matter, such as radial drift of solid bodies, which could release water and…

Earth and Planetary Astrophysics · Physics 2019-09-11 Remo Burn , Ulysse Marboeuf , Yann Alibert , Willy Benz

Hot Jupiters receive strong stellar irradiation, producing equilibrium temperatures of $1000 - 2500 \ \mathrm{Kelvin}$. Incoming irradiation directly heats just their thin outer layer, down to pressures of $\sim 0.1 \ \mathrm{bars}$. In…

Earth and Planetary Astrophysics · Physics 2020-05-05 Thaddeus D. Komacek , Andrew N. Youdin