Saturn, which is the second largest planet in our solar system, is known to have multiple rings and satellites.
In 1979, Pioneer 11 discovered the F ring located just outside the main ring system that extends tens of thousands of kilometres.
The F ring is very narrow with a width of only a few hundred kilometres, and has two shepherd satellites called Prometheus and Pandora, which orbit inside and outside the ring, respectively.
Although the Voyager and Cassini spacecraft later made detailed observations of the F ring and its shepherd satellites, their origin has not been clarified.
During the final stage of satellite formation, multiple small satellites tend to form near the outer edge of the ring.
On the other hand, observations by Cassini indicate that the small satellites orbiting near the outer edge of the main ring system have a dense core.
In their simulations using in part computer systems at the National Astronomical Observatory of Japan, Hyodo Ryuki, a second-year student in the doctoral programme, and Ohtsuki Keiji, professor at the Graduate School of Science at Kobe University showed that the F ring and its shepherd satellites formed as these small satellites with a dense core collided and partially disintegrated.
This new finding is expected to help elucidate the formation of satellite systems both within and outside our solar system.
For example, the above formation mechanism can also be applied to the rings and shepherd satellites of Uranus, which are similar to those of Saturn.
"Through this study, we were able to show that the current rings of Saturn reflect the formation and evolution processes of the planet's satellite system," said Ryuki.
"We will continue to unravel the origin of satellite systems, which is key to understanding the formation process of planetary systems," said Keiji.
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