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Astronomers Discover Two New Giant Exoplanets

TOI-6303b and TOI-6330b expand our understanding of giant planets around M-dwarfs.

Andrew Hotnisky, Shubham Kanodia, Jessica Libby-Roberts, Suvrath Mahadevan, Caleb I. Canas, Arvind F. Gupta, Te Han, Henry A. Kobulnicky, Alexander Larsen, Paul Robertson, Michael Rodruck, Gudmundur Stefansson, William D. Cochran, Megan Delamer, Scott A. Diddams, Rachel B. Fernandes, Samuel Halverson, Leslie Hebb, Andrea S. J. Lin, Andrew Monson, Joe P. Ninan, Arpita Roy, Christian Schwab

― 4 min read


Giant Planets Discovered Giant Planets Discovered Around M-Dwarfs planetary systems. New findings challenge our views on
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In a quest to find new worlds, astronomers have made an exciting discovery. They found two giant planets, TOI-6303b and TOI-6330b. Both are larger than Jupiter and orbit M-dwarfs, which are the most common type of stars in our galaxy. These planets were discovered using a mission called TESS, which stands for Transiting Exoplanet Survey Satellite. TESS is like a cosmic detective, looking for tiny dips in starlight that suggest a planet is passing in front of a star.

Meet the Giants: TOI-6303b and TOI-6330b

TOI-6303b is a hefty 7.84 times the mass of Jupiter and has a radius about the same as Jupiter's. It takes about 9.5 days to complete one orbit around its star. On the other hand, TOI-6330b weighs in at 10 times the mass of Jupiter and has a radius slightly smaller than Jupiter's. It zips around its star in just 6.85 days.

Why M-Dwarfs?

M-dwarfs are a popular focus for astronomers. They're smaller and dimmer than our Sun, but they have a special charm that makes them appealing for discovering planets. The habitable zones, where conditions might be right for life, are much closer to these stars. This closeness makes it easier to spot planets passing in front of them.

One might wonder: can giant planets and smaller, Earth-like planets coexist? So far, we haven't seen both types together in the same system around M-dwarfs. It’s a bit like searching for unicorns in a field of horses. The more we observe, the better we can understand how these planetary buddies interact.

How Did We Find Them?

Both TOI-6303b and TOI-6330b were confirmed through a series of observations. Using different telescopes, scientists gathered enough evidence to say, "Aha! This planet is definitely there!" Ground-based observations followed, allowing astronomers to nail down their characteristics.

The Debate: Core-Accretion vs. Gravitational Instability

When it comes to how these giant planets formed, there are two main theories: core-accretion and gravitational instability.

  1. Core-Accretion: This is the idea that a solid core forms first. Once that core gets big enough, it starts pulling in gas to create a massive planet. Think of it as making a snowman: you start with a small snowball and roll it until it becomes huge.

  2. Gravitational Instability: This theory takes a different route. Instead of building a solid core, it suggests that the gas in a protoplanetary disk becomes so dense that it collapses into clumps, which then become planets. Picture a really thick soup that just can't hold all its ingredients.

The masses of TOI-6303b and TOI-6330b suggest they could have formed through either method, leading to interesting discussions among scientists. This is where it gets tricky; we need more observations to figure out which method is likely the winner.

The Importance of Heavy Elements

One interesting finding is about the heavy elements in these planets. These elements could help reveal how they formed and evolved. Our giant planets probably formed with lots of these heavy elements, possibly due to collisions among smaller bodies in their early solar systems. It's like gathering a bunch of friends to build a really impressive Lego tower!

What About the Eccentricity?

Eccentricity is a fancy term used to describe how "stretched out" or round an orbit is. The more circular an orbit, the lower the eccentricity. TOI-6303b is pretty chill with a low eccentricity, suggesting it has a more stable orbit. TOI-6330b, on the other hand, has a higher eccentricity, indicating it might have experienced some dramatic interactions in its past.

What’s Next?

As scientists continue to search for more GEMS (which stands for Giant Exoplanets around M-dwarfs), they hope to gather more data about these strange worlds. The goal is to understand how they form and what their presence means for smaller, Earth-like planets. Think of it as trying to decipher the recipe for a complicated dish; every new ingredient brings us closer to understanding the final product.

Conclusion: The Cosmic Mystery Continues

The discovery of TOI-6303b and TOI-6330b adds to the growing list of intriguing planets beyond our solar system. The more we learn, the more questions arise. Are these giant planets friends or foes to smaller worlds? What can their formation tell us about our own planet? As astronomers continue their observations, the mysteries of the universe remain tantalizingly out of reach, like a star just beyond the grasp of a telescope's lens.

The quest for knowledge in the cosmos is ever-changing, and who knows what other surprises await us in the vastness of space? Maybe one day we'll have an answer to all the questions swirling around in our heads, but for now, we'll just keep looking up!

Original Source

Title: Searching for GEMS: Two Super-Jupiters around M-dwarfs -- Signatures of Instability or Accretion?

Abstract: We present the discovery of TOI-6303b and TOI-6330b, two massive transiting super-Jupiters orbiting a M0 and a M2 star respectively, as part of the Searching for GEMS survey. These were detected by TESS and then confirmed via ground-based photometry and radial velocity observations with the Habitable-zone Planet Finder (HPF). TOI-6303b has a mass of 7.84 +/- 0.31 MJ, a radius of 1.03 +/- 0.06 RJ , and an orbital period of 9.485 days. TOI-6330b has a mass of 10.00 +/- 0.31 MJ , a radius of 0.97 +/- 0.03 RJ , and an orbital period of 6.850 days. We put these planets in context of super-Jupiters around M-dwarfs discovered from radial-velocity surveys, as well as recent discoveries from astrometry. These planets have masses that can be attributed to two dominant planet formation mechanisms - gravitational instability and core-accretion. Their masses necessitate massive protoplanetary disks that should either be gravitationally unstable, i.e. forming through gravitational instability, or be amongst some of the most massive protoplanetary disks to form objects through core-accretion. We also discuss the eccentricity distribution of these objects, as a potential indicator of their formation and evolutionary mechanisms.

Authors: Andrew Hotnisky, Shubham Kanodia, Jessica Libby-Roberts, Suvrath Mahadevan, Caleb I. Canas, Arvind F. Gupta, Te Han, Henry A. Kobulnicky, Alexander Larsen, Paul Robertson, Michael Rodruck, Gudmundur Stefansson, William D. Cochran, Megan Delamer, Scott A. Diddams, Rachel B. Fernandes, Samuel Halverson, Leslie Hebb, Andrea S. J. Lin, Andrew Monson, Joe P. Ninan, Arpita Roy, Christian Schwab

Last Update: 2024-11-12 00:00:00

Language: English

Source URL: https://arxiv.org/abs/2411.08159

Source PDF: https://arxiv.org/pdf/2411.08159

Licence: https://creativecommons.org/licenses/by/4.0/

Changes: This summary was created with assistance from AI and may have inaccuracies. For accurate information, please refer to the original source documents linked here.

Thank you to arxiv for use of its open access interoperability.

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