Giant planet migration during the disc dispersal phase

نویسندگان

چکیده

Context. Transition discs are expected to be a natural outcome of the interplay between photoevaporation and giant planet formation. Massive planets reduce inflow material from outer inner disc, therefore triggering an earlier onset disc dispersal due through process known as Planet-Induced PhotoEvaporation. In this case, cavity is formed inside planetary orbit removed by photoevaporation, leaving only drive migration planet. Aims. We investigate impact on focus specifically case transition with evacuated location. This important for determining under what circumstances efficient at halting planets, thus affecting final orbital distribution population planets. Methods. For purpose, we use 2D FARGO simulations model in range primordial subject photoevaporation. The results then compared standard prescriptions used calculate tracks 1D synthesis models. Results. show that once location depleted gas, ceases. contradicts obtained impulse approximation, which predicts accelerated inward have been cleared orbit. Conclusions. These suggest approximation may not suitable embedded discs. A better could models would involve gas surface density 3:2 mean motion resonance reaches threshold value 0.01 g cm ‒2 .

برای دانلود رایگان متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Overcoming Migration during Giant Planet Formation

In the core accretion model, gas giant formation is a race between growth and migration; for a core to become a jovian planet, it must accrete its envelope before it spirals into the host star. We use a multizone numerical model to extend our previous investigation of the “window of opportunity” for gas giant formation within a disk. When the collision cross-section enhancement due to core atmo...

متن کامل

Migration and giant planet formation

X iv :a st ro -p h/ 04 03 57 4v 1 2 4 M ar 2 00 4 We extend the core-accretion model of giant gaseous planets by Pollack et al. ([1996]) to include migration, disc evolution and gap formation. Starting with a core of a fraction of an Earth’s mass located at 8 AU, we end our simulation with the onset of runaway gas accretion when the planet is at 5.5 AU 1 Myr later. This timescale is about a fac...

متن کامل

Cavity Opening by a Giant Planet in a Protoplanetary Disc and Effects on Planetary Migration

We study the effect of a Jovian planet on the gas distribution of a protoplanetary disc, using a new numerical scheme that allows us to take into consideration the global evolution of the disc, down to an arbitrarily small inner physical radius. We find that Jovian planets do not open cavities in the inner part of the disc (i.e. interior to their orbits) unless (a) the inner physical edge of th...

متن کامل

Giant Planet Migration through the Action of Disk Torques and Planet-planet Scattering

This paper presents a parametric study of giant planet migration through the combined action of disk torques and planet-planet scattering. The torques exerted on planets during Type II migration in circumstellar disks readily decrease the semi-major axes a, whereas scattering between planets increases the orbital eccentricities ǫ. This paper presents a parametric exploration of the possible par...

متن کامل

Giant Planet Accretion and Migration: Surviving the Type I Regime

In the standard model of gas giant planet formation, a large solid core (∼ 10 times the Earth’s mass) forms first, then accretes its massive envelope (100 or more Earth masses) of gas. However, inward planet migration due to gravitational interaction with the proto-stellar gas disk poses a difficulty in this model. Core-sized bodies undergo rapid “Type I” migration; for typical parameters their...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

ژورنال

عنوان ژورنال: Astronomy and Astrophysics

سال: 2021

ISSN: ['0004-6361', '1432-0746']

DOI: https://doi.org/10.1051/0004-6361/202039658