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Five-Planet Nice Model Representation

A representation of the Five-planet Nice Model if it occurred 4.48 billion years ago.

The Five-planet Nice model is a theoretical framework that describes the early dynamical evolution of the Solar System, building on the original Nice model. This version incorporates the hypothesis of an additional ice giant planet, which would have coexisted with Jupiter, Saturn, Uranus, and Neptune before being ejected from the Solar System. The model is named after the city of Nice, France, where it was first developed by a group of planetary scientists in the early 21st century.

Background[]

The Nice model was first proposed in 2005 to explain several key features of the Solar System, including the formation of the Kuiper belt, the Late Heavy Bombardment, and the current orbital architecture of the giant planets. The original model depicted a scenario where the gas giants formed in a more compact configuration before gravitational interactions scattered them into their current orbits.

The Five-planet version of the model was introduced as a refinement to address unresolved issues in the original theory. Notably, it seeks to explain the observed orbital eccentricities and inclinations of the outer planets while providing a more comprehensive explanation for the depletion of the primordial Kuiper belt.

Key Features of the Model[]

  1. Initial Configuration:
  2. Planetary Instability:
    • Over time, interactions between the planets and the surrounding planetesimal disk led to an orbital instability.
    • This instability caused the planets to migrate outward, with the fifth ice giant being ejected from the system due to gravitational encounters with Jupiter or Saturn.
  3. Ejection of the Fifth Planet:
    • The ejection of the additional ice giant is a critical component of the model. Numerical simulations suggest that such an event would help stabilize the orbits of the remaining planets while reproducing key features of the modern Solar System.
  4. Implications for the Kuiper Belt:
    • The model explains the observed distribution of objects in the Kuiper belt, including its outer edge and "cold classical" population, as a result of the gravitational perturbations during the instability.

Supporting Evidence[]

  • Orbital Dynamics: Simulations incorporating a fifth ice giant produce results that align more closely with the current orbital parameters of the outer planets compared to four-planet models.
  • Exoplanetary Analogues: Observations of exoplanetary systems often reveal configurations with multiple ice giant-like planets, supporting the idea that such systems are not uncommon.
  • Solar System Debris: The scattering of planetesimals during the instability phase can explain the populations of certain distant small bodies, such as detached trans-Neptunian objects and scattered disc objects.

Criticisms and Challenges[]

While the Five-planet Nice model has gained support, it is not without its critics. Some argue that the ejection of an additional giant planet requires specific initial conditions that may not have been present in the early Solar System. Furthermore, direct evidence for the existence of a fifth ice giant is lacking, and alternative explanations for the Solar System's current configuration remain viable.

Legacy and Influence[]

The Five-planet Nice model has advanced the understanding of planetary dynamics and the early evolution of the Solar System. By expanding on the original Nice model, it provides a richer framework for explaining the formation and evolution of planetary systems, both within and beyond the Solar System.

See Also[]

References[]

  1. Tsiganis, K., et al. (2005). "Origin of the orbital architecture of the giant planets of the Solar System." Nature.
  2. Nesvorný, D. (2011). "Young Solar System's Fifth Giant Planet?" The Astrophysical Journal Letters.
  3. Gomes, R., et al. (2005). "Origin of the cataclysmic Late Heavy Bombardment period of the terrestrial planets." Nature.
Models of the Solar System
Solar Formation Nebular hypothesis
Dynamical Evolution
Origin of the Moon
Early Development Grand tack hypothesisFission theoryCo-formation theoryCapture theoryMigration of NeptuneJumping-Jupiter scenario
Later Development Nice model (Nice 2 modelFive-planet Nice model)
Planetary Formation Giant-impact hypothesis
Placement Heliocentric modelGeocentric model