A new study has shed light on the age of Saturn’s rings which was thought to be of younger origin until now.
About the Study
Published In: The new findings were published in the journal Nature Geoscience.
Conducted By: The research is conducted by scientists at the Institute of Science Tokyo and the Paris Institute of Planetary Physics
Objective: To test the hypothesis that Saturn’s Rings are relatively of younger origin ie (between 100-400 million years ago) based on a popular interpretation of the Cassini data
Method: A 3D computer model has been developed to simulate crashes between micrometeoroids and Saturn’s rings at speeds of about 67,100 mph (108,000 km/h).
Finding:
Age of Saturn Rings: Saturn’s rings are likely to be of ancient origin ie. (about 4.5 billion to 4 billion years old) during the era called the Late Heavy Bombardment
Vapourisation: The speedy collisions between micrometeoroids and saturn’s rings generates temperatures of more than 9,725oC leading the micrometeoroids to vaporize and produce electrically charged ions and microscopic particles.
Clean Rings: These charged particles mostly either collide with Saturn, escape its gravitational pull, or get dragged into the planet’s atmosphere.
Therefore, very little of this material appeared to pollute the rings, leaving them relatively clean.
Importance:
Other Planetary Rings: To study and explain the diverse ring systems of our solar system’s four gas giants
To Study the Evolution of Enceladus: To investigate how icy grains from the plumes of Enceladus affect the ring’s composition playing a major role in determining the ring’s age.
Enceladus: It is the geologically active moon of Saturn and is a top-priority target to study habitability and astrobiology due to active plume activity from its subsurface ocean
NASA’s Cassini Spacecraft
Conducted By: Cassini probe is a joint endeavor of NASA, ESA (the European Space Agency), and the Italian space agency (ASI)
A Mission to Saturn: Cassini was a sophisticated robotic spacecraft sent to study Saturn in 2004 and its complex system of rings and moons.
ESA’s Huygens probe parachuted to Titan, making the first landing on a moon in the outer solar system
Objectives:
Saturn: To study cloud properties and atmospheric composition, winds and temperatures, internal structure and rotation, ionosphere, origin, and evolution
Rings: To observe their structure and composition, dynamical processes, interrelation of rings and satellites, dust and micrometeoroid environment
Titan: To study abundances of atmospheric constituents, distribution of trace gases and aerosols, winds and temperatures, composition and state of the surface, and upper atmosphere
Icy Satellite: To determine their characteristics and geological histories; study mechanisms of surface modification, surface composition and distribution, overall composition and internal structure, and their interactions with Saturn’s magnetosphere
Saturn’s Magnetosphere: To study its structure and electric currents; composition, sources, and sinks of particles within it; dynamics; interaction with the solar wind, satellites, and rings.
Key Findings:
Clean Rings: Saturn’s rings appeared relatively bright and clean with minimal accumulation of space dust particles
Enceladus Moon: Enceladus possesses a global ocean of liquid water, likely with hydrothermal activity on the seafloor
Icy plumes: They were found to be abundant in water molecules leaking from Enceladus’s southern hemisphere.
Saturn’s rings were found to be active and dynamic
Titan Moon: It has rain, rivers, lakes, and seas; it is shrouded in a thick, nitrogen-rich atmosphere that might be similar to what Earth’s was like long ago
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