Supercomputer Simulation Explains the Origins of Mars’ Moons

Supercomputer Simulation Explains the Origins of Mars’ Moons

Mars’ moons, Deimos and Phobos, have long been mysterious. While various theories have existed about their origins, new supercomputer simulations are providing fresh insights. These simulations suggest that the moons were not simply captured asteroids, nor the result of a traditional collision. Instead, a near miss by a large asteroid may have created a debris ring from which the moons formed.

This discovery brings us closer to understanding these enigmatic companions of Mars. With future missions like the Mars Moons eXploration (MMX) mission set for 2026, we may finally answer the question of how Mars’ moons came to be.

Summary

• Mars is one of only two rocky planets in the solar system with moons.
• The two Martian moons, Deimos and Phobos, resemble small asteroids.
• There are two main models explaining their origins: capture or collision.
• The capture model struggles due to Mars’ weak gravity.
• The collision model suggests an asteroid impact, forming debris that became the moons.
• A new model proposes a “near miss” by an asteroid that caused tidal forces to break it apart.
• The fragments from the near miss formed elliptical orbits around Mars, eventually becoming circular.
• The new model explains the orbital characteristics of both moons.
• The upcoming MMX mission in 2026 may provide rock samples to confirm the origin.

Introduction to the Mystery of Mars’ Moons

Mars’ moons, Deimos and Phobos, have fascinated scientists for centuries. Unlike Earth’s Moon, which has a well-understood origin tied to the collision between Earth and a protoplanet, Mars’ moons have remained enigmatic. While these moons are small, irregularly shaped objects, they hold critical clues about the early history of our solar system and the planet Mars itself. Researchers have proposed several theories about how these moons were formed, but new advancements in supercomputer simulations are helping to clarify their true origin.

The Current Models

Two main theories have dominated discussions about the origins of Deimos and Phobos.

Capture Theory:

This theory suggests that the moons are captured asteroids. This would explain why they resemble asteroids in size and composition. However, this model faces significant challenges because Mars is much smaller than Earth and Venus, and its gravitational pull is weaker. Capturing one asteroid, let alone two, would be a rare event, especially for a planet like Mars. In addition, captured moons generally have elliptical orbits, which does not match the nearly circular orbits of Phobos and Deimos.

Collision Theory:

The collision theory posits that an asteroid or comet collided with Mars early in its history. This impact would have created a debris ring, and from this ring, the moons would have formed. This theory accounts for the circular orbits of Phobos, which is close to Mars. However, Deimos, the smaller moon, has a more distant orbit, which is difficult to explain using this theory.

The Supercomputer Simulation Breakthrough

New supercomputer simulations are challenging these traditional models by proposing a compromise theory that blends both ideas. According to this new model, a large asteroid passed close to Mars and was torn apart by the tidal forces of the planet’s gravity. Instead of being captured outright or colliding with Mars, the asteroid’s fragments were captured into elliptical orbits around Mars. Over time, these orbits shifted due to the small gravitational influences of the Sun and other planets in the solar system.

The small gravitational tugs from other bodies, including the Sun, caused the orbits of the fragments to shift, eventually leading some of them to collide and form a debris ring around Mars. This process allowed the moons to form at a greater distance than the collision model had suggested, better explaining both the orbits of Phobos and Deimos.

This breakthrough offers a better explanation for the current positions and orbits of the Martian moons. It accounts for the proximity of Phobos to Mars and the more distant orbit of Deimos.

The Importance of the MMX Mission

While these simulations offer an intriguing explanation, they are still hypotheses. The real test will come in 2026, when the Mars Moons eXploration (MMX) mission is set to launch. MMX will explore both Deimos and Phobos, gathering important samples, particularly from Phobos, to help confirm or challenge these theories. This mission could be the key to unlocking the mystery of how Mars’ moons came to be.

Facts About Mars’ Moons

• Phobos is gradually getting closer to Mars and will eventually crash into the planet in about 50 million years.
• Deimos is moving away from Mars at a rate of about 1.8 centimeters per year.
• The origin of Mars’ moons has been debated for centuries, but we are now closer to solving the mystery.
• Both moons are irregularly shaped and are considered to be captured asteroids or remnants from a past collision.
• The name Phobos comes from the Greek word for “fear,” while Deimos comes from the Greek word for “panic.” These names were chosen because of the moons’ association with Mars, the god of war.

The origins of Mars’ moons have long been a topic of great scientific interest. Through new supercomputer simulations, researchers are offering a compelling new theory that might finally explain the mysteries of Deimos and Phobos. Whether these moons were captured from the asteroid belt or the result of a near-miss asteroid collision, the answers will likely come in the near future with the MMX mission. Until then, the mystery of Mars’ moons remains an exciting puzzle for scientists and space enthusiasts alike.

References

1. Origin of Mars’s moons by disruptive partial capture of an asteroid – Kegerreis, Jacob A., et al.
2. Rings of an Ancient Sky – Brian Koberlein.
3. Broken World – Brian Koberlein.
4. JAXA MMX Mission – Japan Aerospace Exploration Agency.
5. Mars and its Moons – NASA Solar System Exploration.

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