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Conditions on Early Earth02:06

Conditions on Early Earth

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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.
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Reduced Mass Coordinates: Isolated Two-body Problem01:12

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In classical mechanics, the two-body problem is one of the fundamental problems describing the motion of two interacting bodies under gravity or any other central force. When considering the motion of two bodies, one of the most important concepts is the reduced mass coordinates, a quantity that allows the two-body problem to be solved like a single-body problem. In these circumstances, it is assumed that a single body with reduced mass revolves around another body fixed in a position with an...
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Kepler's First Law of Planetary Motion01:10

Kepler's First Law of Planetary Motion

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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,...
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Circular Orbits and Critical Velocity for Satellites01:16

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The Moon orbits around the Earth. In turn, the Earth (and other planets) orbit the Sun. The space directly above our atmosphere is filled with artificial satellites in orbit. One can examine the circular orbit, the simplest kind of orbit, to understand the relationship between the speed and the period of planets and satellites with respect to their positions and the bodies that they orbit.
Nicolaus Copernicus (1473-1543) first suggested that the Earth and all other planets orbit the Sun in...
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Atomic Orbitals02:44

Atomic Orbitals

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An atomic orbital represents the three-dimensional regions in an atom where an electron has the highest probability to reside. The radial distribution function indicates the total probability of finding an electron within the thin shell at a distance r from the nucleus. The atomic orbitals have distinct shapes which are determined by l, the angular momentum quantum number. The orbitals are often drawn with a boundary surface, enclosing densest regions of the cloud.
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First Law: Particles in One-dimensional Equilibrium01:10

First Law: Particles in One-dimensional Equilibrium

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Newton's first law of motion states that a body at rest remains at rest, or if in motion, remains in motion at constant velocity, unless acted on by a net external force. It also states that there must be a cause for any change in velocity (a change in either magnitude or direction) to occur. This cause is a net external force. For example, consider what happens to an object sliding along a rough horizontal surface. The object quickly grinds to a halt, due to the net force of friction. If...
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Related Experiment Video

Updated: Feb 22, 2026

Laboratory Drop Towers for the Experimental Simulation of Dust-aggregate Collisions in the Early Solar System
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Laboratory Drop Towers for the Experimental Simulation of Dust-aggregate Collisions in the Early Solar System

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The empty primordial asteroid belt.

Sean N Raymond1, Andre Izidoro1,2

  • 1Laboratoire d'Astrophysique de Bordeaux, Université de Bordeaux, CNRS, B18N, Allée Geoffroy Saint-Hilaire, 33615 Pessac, France.

Science Advances
|September 20, 2017
PubMed
Summary
This summary is machine-generated.

The asteroid belt may have formed empty, with planetesimals later migrating in from terrestrial and giant planet formation. This challenges previous assumptions of a massive, depleted asteroid belt.

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Area of Science:

  • Planetary Science
  • Solar System Formation
  • Asteroid Research

Background:

  • The asteroid belt shows radial segregation of S-type (inner) and C-type (outer) asteroids.
  • Current models assume the asteroid belt initially formed with substantial mass, which was later depleted.

Purpose of the Study:

  • To investigate the formation of the asteroid belt by testing the hypothesis that it formed empty.
  • To determine if planetesimal implantation mechanisms can explain the observed composition and distribution of asteroids.

Main Methods:

  • Simulations modeling planetesimal dynamics and gravitational scattering during planet formation.
  • Analysis of mass distribution and radial segregation patterns within the asteroid belt.

Main Results:

  • The present-day asteroid belt composition and distribution are consistent with an initially empty formation scenario.
  • Terrestrial planet formation scattered planetesimals into the inner belt (S-types).
  • Giant planet formation injected planetesimals into the outer belt (C-types).

Conclusions:

  • The asteroid belt may have formed without planetesimals, acting as a repository for material from across the solar system.
  • Implantation mechanisms are a natural consequence of terrestrial and giant planet formation.
  • This challenges traditional models of asteroid belt formation and evolution.