Published August 2008 | Version v1
Journal article

Rapid formation of gas giants, ice giants and super-Earths

Creators

  • 1. DTM, Carnegie Institution of Washington, 5241 Broad Branch Road, NW, Washington, DC 20015 (United States)

Description

Giant planets might have been formed by either of the two basic mechanisms, top-down (disk instability) or bottom-up (core accretion). The latter mechanism is the most generally accepted mechanism and it begins with the collisional accumulation of solid cores that may then accrete sufficient gas to become gas giants. The former mechanism is more heretical and begins with the gravitational instability of the protoplanetary disk gas, leading to the formation of self-gravitating protoplanets, within which the dust settles to form a solid core. The disk instability mechanism has been thought of primarily as a mechanism for the formation of gas giants, but if it occurs in a disk that is being photoevaporated by the ultraviolet radiation from nearby massive stars, then the outer gaseous protoplanets can be photoevaporated as well and stripped of their gaseous envelopes. The result would then be ice giants (cold super-Earths), such as the objects discovered recently by microlensing orbiting two presumed M dwarf stars. M dwarfs that form in regions of future high-mass star formation would be expected to produce cold super-Earths orbiting at distances of several astronomical units (AU) and beyond, while M dwarfs that form in regions of low-mass star formation would be expected to have gas giants at those distances. Given that most stars are born in the former rather than in the latter regions, M dwarfs should have significantly more super-Earths than gas giants on orbits of several AU or more

Availability note (English)

Available from http://dx.doi.org/10.1088/0031-8949/2008/T130/014020

Additional details

Publishing Information

Journal Title
Physica Scripta (Online)
Journal Volume
2008
Journal Issue
T130
Journal Page Range
[7 p.]
ISSN
1402-4896

Conference

Title
Physics of planetary systems
Acronym
Nobel symposium 135
Dates
18-22 Jun 2007
Place
Stockholm (Sweden)

INIS

Country of Publication
United Kingdom
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
40018982
Subject category
S71: CLASSICAL AND QUANTUM MECHANICS, GENERAL PHYSICS;
Resource subtype / Literary indicator
Conference
Descriptors DEI
DISTANCE; DUSTS; DWARF STARS; GRAVITATIONAL INSTABILITY; ICE; MASS; ORBITS; PLANETS; PROTOPLANETS; ULTRAVIOLET RADIATION
Descriptors DEC
ELECTROMAGNETIC RADIATION; INSTABILITY; PLASMA INSTABILITY; RADIATIONS; STARS