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Uranus and Neptune: Origin, Evolution and Internal Structure
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There are still many open questions regarding the nature of Uranus and Neptune, the outermost planets in the Solar System. In this review we summarize the current-knowledge about Uranus and Neptune with a focus on their composition and internal structure, formation including potential subsequent giant impacts, and thermal evolution. We present key open questions and discuss the uncertainty in the internal structures of the planets due to the possibility of non-adiabatic and inhomogeneous interiors. We also provide the reasoning for improved observational constraints on their fundamental physical parameters such as their gravitational and magnetic fields, rotation rates, and deep atmospheric composition and temperature. Only this way will we be able to improve our understating of these planetary objects, and the many similar-sized objects orbiting other stars.
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Accretion of Uranus and Neptune: confronting different giant impact scenarios
Both the equal-mass-embryo scenario and the high-mass-ratio impact scenario form Uranus and Neptune analogues with comparable low probability (~0.1-1%), so neither is dynamically preferred.
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