Jump to content
Main menu
Main menu
move to sidebar
hide
Navigation
Main page
Recent changes
Random page
Help about MediaWiki
Special pages
Niidae Wiki
Search
Search
Appearance
Create account
Log in
Personal tools
Create account
Log in
Pages for logged out editors
learn more
Contributions
Talk
Editing
Uranus
(section)
Page
Discussion
English
Read
Edit
View history
Tools
Tools
move to sidebar
hide
Actions
Read
Edit
View history
General
What links here
Related changes
Page information
Appearance
move to sidebar
hide
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
== Formation == {{main|Formation and evolution of the Solar System}} {{For|details of the evolution of Uranus's orbit|Nice model}} It is argued that the differences between the ice giants and the gas giants arise from their formation history.<ref name="Thommes1999" /><ref name="Brunini1999" /><ref name="dangelo2021">{{Cite journal |last1=D'Angelo |first1=Gennaro |last2=Weidenschilling |first2=Stuart J. |last3=Lissauer |first3=Jack J. |last4=Bodenheimer |first4=Peter |date=February 2021 |title=Growth of Jupiter: Formation in disks of gas and solids and evolution to the present epoch |journal=[[Icarus (journal)|Icarus]] |volume=355 |pages=114087 |arxiv=2009.05575 |bibcode=2021Icar..35514087D |doi=10.1016/j.icarus.2020.114087 |s2cid=221654962}}</ref> The Solar System is hypothesised to have formed from a rotating disk of gas and dust known as the [[presolar nebula]]. Much of the nebula's gas, primarily hydrogen and helium, formed the Sun, and the dust grains collected together to form the first protoplanets. As the planets grew, some of them eventually accreted enough matter for their gravity to hold on to the nebula's leftover gas.<ref name="Thommes1999" /><ref name="Brunini1999" /><ref name="dangelo_bodenheimer_2013">{{Cite journal |last1=D'Angelo |first1=Gennaro |last2=Bodenheimer |first2=Peter |date=6 November 2013 |title=Three-dimensional Radiation-hydrodynamics Calculations of the Envelopes of Young Planets Embedded in Protoplanetary Disks |journal=[[The Astrophysical Journal]] |volume=778 |issue=1 |pages=77 |arxiv=1310.2211 |bibcode=2013ApJ...778...77D |doi=10.1088/0004-637X/778/1/77 |issn=0004-637X |s2cid=118522228}}</ref> The more gas they held onto, the larger they became; the larger they became, the more gas they held onto until a critical point was reached, and their size began to increase exponentially.<ref name="dl2018">{{Cite book |last1=D'Angelo |first1=G. |title=Handbook of Exoplanets |last2=Lissauer |first2=J. J. |date=2018 |publisher=[[Springer International Publishing AG]] |isbn=978-3-319-55332-0 |editor-last=Deeg |editor-first=H. |pages=2319β2343 |chapter=Formation of Giant Planets |bibcode=2018haex.bookE.140D |doi=10.1007/978-3-319-55333-7_140 |editor-last2=Belmonte |editor-first2=J. |arxiv=1806.05649 |s2cid=116913980}}</ref> The ice giants, with only a few [[Earth mass]]es of nebular gas, never reached that critical point.<ref name="Thommes1999" /><ref name="Brunini1999" /><ref name="Sheppard Jewitt Kleyna 2006" /> Recent simulations of [[planetary migration]] have suggested that both ice giants formed closer to the Sun than their present positions, and moved outwards after formation (the [[Nice model]]).<ref name="Thommes1999" />
Summary:
Please note that all contributions to Niidae Wiki may be edited, altered, or removed by other contributors. If you do not want your writing to be edited mercilessly, then do not submit it here.
You are also promising us that you wrote this yourself, or copied it from a public domain or similar free resource (see
Encyclopedia:Copyrights
for details).
Do not submit copyrighted work without permission!
Cancel
Editing help
(opens in new window)
Search
Search
Editing
Uranus
(section)
Add topic