Exoplanets’ complex orbital structure points to planetary migration in solar systems


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The four planets of the Kepler-223 star system seem to have little in common with the planets of Earth’s own solar system. And yet a new study shows that the Kepler-223 system is trapped in an orbital configuration that Jupiter, Saturn, Uranus, and Neptune may have broken from in the early history of the solar system.

Exoplanets' complex orbital structure points to planetary migration in solar systems
This animation illustrates the Kepler-223 planetary system, which has long-term stability because its four planets interact gravitationally to keep the beat of a carefully choreographed dance as they orbit their host star. For example, each time the innermost planet (Kepler-223b) orbits the system’s star 3 times, the second-closest planet (Kepler-223c) orbits precisely 4 times, and these two planets return to the same positions relative to each other and their host star. The orbital periods of the four planets of the Kepler-233 system have ratios of exactly 3 to 4, 4 to 6, and 6 to 8. The ratio of these orbits is so precise that they provide a stabilizing influence
 for the planetary system [Credit: W. Rebel]

“Exactly how and where planets form is an outstanding question in planetary science,” said the study’s lead author, Sean Mills, a graduate student in astronomy & astrophysics at the University of Chicago. “Our work essentially tests a model for planet formation for a type of planet we don’t have in our solar system.”

These puffy, gaseous planets, far more massive than Earth, orbit close to their stars. “That’s why there’s a big debate about how they form, how they got there, and why don’t we have one,” Mills said.

Mills and his collaborators used brightness data from NASA’s Kepler telescope to analyze how the four planets block the starlight and change each other’s orbits, thus inferring the planets’ sizes and masses. The team performed numerical simulations of planetary migration that generate this system’s current architecture, similar to the migration suspected for the solar system’s gas giants. These calculations are described in Nature.

The orbital configuration of the solar system seems to have evolved since its birth 4.6 billion years ago. The four known planets of the much older Kepler-223 system, however, have maintained one orbital configuration for far longer.

The planets of Kepler-223 are much larger than Earth, likely consisting of a solid core and an envelope of gas, and they orbit their star in periods ranging from only seven to 19 days. Astronomers call these planets sub-Neptunes. They are the most common type of planets known in the galaxy.

Kepler-223’s planets also are in resonance. Planets are in resonance when, for example, every time one of them orbits its sun once, the next one goes around twice. Jupiter’s moons, where the phenomenon was discovered, display resonance.

Kepler-223’s two innermost planets are in a 4:3 resonance. The second and third are in a 3:2 resonance. And the third and fourth are in a 4:3 resonance. Astronomers had seen extrasolar systems containing two or three planets in resonance, but not four.

“This is the most extreme example of this phenomenon,” said study co-author Daniel Fabrycky, an assistant professor of astronomy & astrophysics at UChicago.

Exoplanets' complex orbital structure points to planetary migration in solar systems
The arrangement and relative sizes of the four planets around Kepler-223, though not to scale. One AU (astronomical unit) is 93 million miles, the distance between Earth and sun in our solar system [Credit: University of Chicago]

Formation scenarios

The Kepler-223 system provides alternative scenarios for how planets form and migrate in a planetary system that is different from our own, said study co-author Howard Isaacson, a research astronomer at the University of California, Berkeley, and member of the California Planet Search Team.

“Data from Kepler and the Keck Telescope were absolutely critical in this regard,” Isaacson said. Thanks to observations of Kepler-223 and other exoplanetary systems, “We now know of systems that are unlike the sun’s solar system, with hot Jupiters, planets closer than Mercury or in between the size of Earth and Neptune, none of which we see in our solar system. Other types of planets are very common.”

Some stages of planet formation can involve violent processes, but during other stages, planets can evolve from gaseous disks in a smooth, gentle way, which is probably what the sub-Neptune planets of Kepler-223 did, Mills said.

“We think that two planets migrate through this disk, get stuck and then keep migrating together; find a third planet, get stuck, migrate together; find a fourth planet and get stuck,” Mills explained.

That process differs completely from the one that scientists believe led to the formation of Earth, Mercury, Venus, and Mars, which likely formed in their current orbital locations.

Earth formed from Mars- or moon-sized bodies smacking together, Mills said, a violent and chaotic process. When planets form this way their final orbital periods are not near a resonance.

Substantial movement

But scientists suspect that the solar system’s larger, more distant planets of today–Jupiter, Saturn, Uranus, and Neptune–moved around substantially during their formation. They may have been knocked out of resonances that once resembled those of Kepler-223, possibly after interacting with numerous asteroids and small planets (planetesimals).

These animations show approximately 200,000 years of orbital evolution
in the Kepler-223 planetary system. The planets’ interactions with the
disk of gas and dust in which they formed caused their orbits to shrink
toward their star over time at differing rates. Once two planets reach a
resonant state (for example, one planet orbits its star three times
every time the next planet orbits two times), the planets strongly
interact with each other. The interactions become apparent in the
animations as the orbits shrink (left and top right) when the orbital
period ratios of neighboring planets (bottom right) get stuck at
constant values. Even as the planets continue moving inwards (upper
right) they do so in concert, migrating together locked in this
configuration. They also cause each other’s orbits to change from nearly
circular to elliptical. This is represented by the varying orbits on
the left panel and the spread of the orbital distances for each
individual planet in the upper right [Credit: Daniel Fabrycky and
Cezary Migazewski]

“These resonances are extremely fragile,” Fabrycky said. “If bodies were flying around and hitting each other, then they would have dislodged the planets from the resonance.” But Kepler-223’s planets somehow managed to dodge this scattering of cosmic bodies.

Other processes, including tidal forces that flex the planets, might also cause resonance separation.

“Many of the multi-planet systems may start out in a chain of resonances like this, fragile as it is, meaning that those chains usually break on long timescales similar to those inferred for the solar system,” Fabrycky said.

Mills and Fabrycky’s UC Berkeley collaborators were able to determine the size and mass of the star by making precise measurements of its light using the high resolution Echelle spectrometer on the 10-meter Keck I telescope atop Mauna Kea in Hawaii.

“The spectrum revealed a star very similar in size and mass to the sun but much older–more than six billion years old,” UC Berkeley’s Isaacson said. “You need to know the precise size of the star so you can do the dynamical and stability analysis, which involve estimates of the masses of the planets.”

Source: University of Chicago [May 12, 2016]



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