Uranus and Neptune: Origin, Evolution and Internal Structure
arXiv:1909.04891 · doi:10.1007/s11214-020-00660-3
Abstract
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.
arXiv commentAccepted for publication in Space Science Reviews
References in corpus (41)
- Planetary Candidates Observed by Kepler, III: Analysis of the First 16 Months of Data
- Rapid growth of gas-giant cores by pebble accretion
- The Interiors of Giant Planets: Models and Outstanding Questions
- The Interior Structure, Composition, and Evolution of Giant Planets
- A new vision on giant planet interiors: the impact of double diffusive convection
- Growing the gas-giant planets by the gradual accumulation of pebbles
- Interior Models of Uranus and Neptune
- New indication for a dichotomy in the interior structure of Uranus and Neptune from the application of modified shape and rotation data
- Planet formation with envelope enrichment: new insights on planetary diversity
- Herschel measurements of the D/H and 16O/18O ratios in water in the Oort-cloud comet C/2009 P1 (Garradd)
- Self-Consistent Model Atmospheres and the Cooling of the Solar System's Giant Planets
- Layered convection as the origin of Saturn's luminosity anomaly
- Condensation-inhibited convection in hydrogen-rich atmospheres: Stability against double-diffusive processes and thermal profiles for Jupiter, Saturn, Uranus, and Neptune
- Uranus evolution models with simple thermal boundary layers
- The formation of Jupiter by hybrid pebble-planetesimal accretion
- The D/H ratio in the atmospheres of Uranus and Neptune from Herschel PACS observations
- The fuzziness of giant planets' cores
- Uranus and Neptune: Shape and Rotation
- Cassini Ring Seismology as a Probe of Saturn's Interior I: Rigid Rotation
- The Evolution and Internal Structure of Jupiter and Saturn with Compositional Gradients
- Accretion of Uranus and Neptune from inward-migrating planetary embryos blocked by Jupiter and Saturn
- Planetary Ices and the Linear Mixing Approximation
- Consequences of Giant Impacts on Early Uranus for Rotation, Internal Structure, Debris, and Atmospheric Erosion
- The formation of mini-Neptunes
- A collisionless scenario for Uranus tilting
- Saturn's fast spin determined from its gravitational field and oblateness
- Probable detection of hydrogen sulphide (HS) in Neptune's atmosphere
- Models of Saturn's Interior Constructed with Accelerated Concentric Maclaurin Spheroid Method
- Record-breaking Storm Activity on Uranus in 2014
- The Formation of Uranus & Neptune: Challenges and Implications For Intermediate-Mass Exoplanets
- Constraining the Origins of Neptune's Carbon Monoxide Abundance with CARMA Millimeter-wave Observations
- Explaining the low luminosity of Uranus: A self-consistent thermal and structural evolution
- Effect of Non-Adiabatic Thermal Profiles on the Inferred Compositions of Uranus and Neptune
- Bifurcation in the history of Uranus and Neptune: the role of giant impacts
- Thermochemistry and vertical mixing in the tropospheres of Uranus and Neptune: How convection inhibition can affect the derivation of deep oxygen abundances
- The Formation of Uranus and Neptune in Solid-Rich Feeding Zones: Connecting Chemistry and Dynamics
- Thermal evolution of Uranus and Neptune I: adiabatic models
- What do we Really Know about Uranus and Neptune?
- Analysis of Neptune's 2017 Bright Equatorial Storm
- Acceleration of Cooling of Ice Giants by Condensation in Early Atmospheres
- The Exchange of Mass and Angular Momentum in the Impact Event of Ice Giant Planets: Implications for the origin of Uranus
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- New constraints on the planetary system around the young active star AU Mic. Two transiting warm Neptunes near mean-motion resonance
- A High Internal Heat Flux and Large Core in a Warm Neptune Exoplanet
- Predicting the phase behaviors of superionic water at planetary conditions
- Transition in the supercritical state of matter: experimental evidence
- The Interiors of Uranus and Neptune: Current Understanding and Open Questions
- Superionic silica-water and silica-hydrogen compounds under high pressure
- A framework for the architecture of exoplanetary systems. I. Four classes of planetary system architecture
- The Imprint of the Protoplanetary Disk in the Accretion of Super-Earth Envelopes
- The Fundamental Connections Between the Solar System and Exoplanetary Science
- Metallization of Shock-Compressed Liquid Ammonia
- Heat and charge transport in HO at ice-giant conditions from ab initio molecular dynamics simulations
- Early planet formation in embedded protostellar disks: Setting the stage for the first generation of planetesimals
- How planets grow by pebble accretion IV: Envelope opacity trends from sedimenting dust and pebbles
- Tentative Evidence for Water Vapor in the Atmosphere of the Neptune-Size Exoplanet HD 106315 c
- The deep composition of Uranus and Neptune from in situ exploration and thermochemical modeling
- Ice Giant System Exploration in the 2020s: An Introduction
- Ariel Planetary Interiors White Paper
- Convective storms and atmospheric vertical structure in Uranus and Neptune
- Asynchronous accretion can mimic diverse white dwarf pollutants II: water content
- A warm super-Neptune around the G-dwarf star TOI-1710 revealed with TESS, SOPHIE and HARPS-N
- The interior of Uranus: Thermal profile, bulk composition and the distribution of rock, water and hydrogen and helium
- Could Uranus and Neptune form by collisions of planetary embryos?
- H-HO demixing in Uranus and Neptune: Adiabatic structure models
- Partially Diffusive Helium-Silica Compound in the Deep Interiors of Giant Planets
- The deep oxygen abundance in Solar System Giant Planets, with a new derivation for Saturn
- Speed of sound in methane under conditions of planetary interiors
- Random Models for Exploring Planet Compositions I: Uranus as an Example
- Ab Initio Entropy Calculations of Water Predict the Interiors of Uranus and Neptune to be 15-30% Colder than Previous Models
- Very-wide-orbit planets from dynamical instabilities during the stellar birth cluster phase
- Solid Accretion onto Neptune-Mass Planets I: In-Situ Accretion and Constraints from the metallicity of Uranus and Neptune
- An idealized general circulation model for the atmospheric circulation on the ice giants
- Thermal evolution of Uranus and Neptune II -- Deep thermal boundary layer
- Did Uranus' regular moons form via a rocky giant impactor?
- Reassessing planetary composition: Evidence of rock-dominated envelopes in Uranus and Neptune
- Possible in situ formation of Uranus and Neptune via Pebble Accretion
- Chemical diversity of the atmospheres and interiors of sub-Neptunes: a case study of GJ 436 b