Related Experiment Video
Updated: Apr 15, 2026

06:04
Simulation of the Planetary Interior Differentiation Processes in the Laboratory
Published on: November 15, 2013
12.2K
Jupiter's decisive role in the inner Solar System's early evolution.
Konstantin Batygin1, Greg Laughlin2
1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125; and kbatygin@gps.caltech.edu.
Summary
The Solar System
Area of Science:
- Planetary Science
- Computational Astrophysics
- Solar System Formation
Background:
- Extrasolar planetary systems typically form planets with short orbital periods (<100 days) and high masses.
- The Solar System's architecture, with its low-mass terrestrial planets and lack of short-period planets, is anomalous compared to exoplanetary systems.
- A common formation scenario involves Jupiter migrating inward from beyond 5 AU to 1.5 AU before outward migration.
Purpose of the Study:
- To investigate whether Jupiter's inward migration can explain the unique characteristics of the Solar System's terrestrial planets.
- To understand the dynamical processes that shaped the inner Solar System and led to its low terrestrial planet mass and absence of close-in planets.
Main Methods:
- Computational simulations of planet formation and dynamical evolution.
- Modeling Jupiter's inward migration and its gravitational influence on planetesimals.
- Analysis of orbital resonances, collisional cascades, and gas drag effects on early planetary bodies.
Main Results:
- Jupiter's inward migration to ~1.5 AU can account for the low mass of terrestrial planets.
- This migration process explains the absence of planets within 0.4 AU.
- Migrating Jupiter's gravity excited planetesimals into resonances, triggering a cascade that depleted material and removed inner planets.
Conclusions:
- The inward migration of Jupiter is a key factor in shaping the terrestrial planet region of the Solar System.
- The terrestrial planets likely formed from a depleted debris disk after significant dynamical evolution.
- This scenario reconciles the Solar System's unusual architecture with general planet formation theories.
Related Concept Videos
Kepler's First Law of Planetary Motion
6.2K
In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. He formulated his first two laws based on the observations of his forebears, Nikolaus Copernicus and Tycho Brahe.
Polish astronomer Nikolaus Copernicus put forth a theory that stated a heliocentric model for the solar system. According to this heliocentric theory, all the planets, including Earth, orbit the Sun in circular orbits.
On the other hand,...
Polish astronomer Nikolaus Copernicus put forth a theory that stated a heliocentric model for the solar system. According to this heliocentric theory, all the planets, including Earth, orbit the Sun in circular orbits.
On the other hand,...
6.2K
Kepler's Third Law of Planetary Motion
4.7K
In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. In 1909, he formulated his first two laws based on the observations of his forebears, Nikolaus Copernicus and Tycho Brahe. However, in 1918, he published his third law of planetary motion, which gives a precise mathematical relationship between a planet's average distance from the Sun and the amount of time it takes to revolve around the Sun. It...
4.7K
Kepler's Second Law of Planetary Motion
5.9K
In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. His first law states that all planets orbit the Sun in an elliptical orbit, with the Sun at one of the ellipse's foci. Therefore, the distance of a planet from the Sun varies throughout its revolution around the Sun.
While in an elliptical orbit, the total energy of the planet is conserved. Therefore, the planet slows down when it is at apogee and...
While in an elliptical orbit, the total energy of the planet is conserved. Therefore, the planet slows down when it is at apogee and...
5.9K
Conditions on Early Earth
103.6K
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
103.6K
Conditions on Early Earth
3.0K
3.0K
Acceleration due to Gravity on Other Planets
5.2K
The gravitational acceleration of an object near the Earth's surface is called the acceleration due to gravity. It can be measured by conducting simple experiments on Earth. However, such an experiment is impossible to conduct on the surface of other planets.
Astronomical observations are thus used to measure the acceleration due to gravity on other planets. This can be determined by observing the effect of a planet's gravity on objects close to it. The crucial factor that helps in this...
Astronomical observations are thus used to measure the acceleration due to gravity on other planets. This can be determined by observing the effect of a planet's gravity on objects close to it. The crucial factor that helps in this...
5.2K

