Sub-Neptunes: The Most Common Planets in the Galaxy

Sub-Neptunes are a class of planets that are smaller than Neptune, but larger than Earth. They are also known as mini-Neptunes or super-Earths, depending on their mass and composition. Sub-Neptunes are the most frequently observed type of planet in our galaxy, and they exhibit a wide range of properties and characteristics. In this article, we will explore what sub-Neptunes are, how they form, and what they can tell us about the diversity and evolution of planetary systems.

What are sub-Neptunes?

The term sub-Neptune can refer to a planet with a smaller radius than Neptune, even though it may have a larger mass, or to a planet with a smaller mass than Neptune, even though it may have a larger radius like a super-puff. Both meanings can be used in the same publication. Sub-Neptunes have radii between that of Earth and Neptune, which corresponds to about 1.25 to 3.9 times the radius of Earth.

Sub-Neptunes can have different compositions, depending on their formation history and environment. Some sub-Neptunes may be rocky worlds with thick atmospheres of hydrogen and helium gas, or perhaps composed of rock and ice with warm, water-rich atmospheres. Others may be more similar to Neptune, with a large fraction of dense gas and a smaller core of rock and ice. The density and temperature of sub-Neptunes can vary significantly, as well as their orbital properties and interactions with their host stars and other planets.

One of the ways to classify sub-Neptunes is by their bulk density, which is the ratio of their mass to their volume. Bulk density can indicate the relative amount of gas, rock, and ice in a planet's interior. For example, a sub-Neptune with a low bulk density (less than 1 g/cm$^3$) may have a large gas envelope, while a sub-Neptune with a high bulk density (more than 5 g/cm$^3$) may have a small or negligible gas envelope. However, bulk density alone is not enough to determine the exact composition of a sub-Neptune, as other factors such as temperature, pressure, and chemical reactions can affect the state and distribution of the materials inside the planet.

Another way to classify sub-Neptunes is by their atmospheric temperature, which is influenced by the distance from their host star, the albedo (reflectivity) of their surface, and the greenhouse effect of their atmosphere. Atmospheric temperature can affect the stability and escape of the gas envelope, as well as the chemistry and dynamics of the atmosphere. For example, a sub-Neptune with a high atmospheric temperature (more than 1000 K) may have a thin or evaporated gas envelope, while a sub-Neptune with a low atmospheric temperature (less than 300 K) may have a thick or accreted gas envelope. However, atmospheric temperature alone is not enough to determine the exact structure and evolution of a sub-Neptune, as other factors such as stellar activity, orbital eccentricity, and tidal heating can affect the energy balance and heat transport of the planet.

Some examples of sub-Neptunes that have been discovered and characterized by various methods are:
  • Kepler-11b, c, d, e, f, and g: A system of six sub-Neptunes orbiting a Sun-like star, with radii ranging from 1.8 to 4.2 times that of Earth and masses ranging from 2 to 25 times that of Earth. They have low densities (0.7 to 1.5 g/cm$^3$) and high temperatures (600 to 900 K), suggesting that they have large gas envelopes that are being eroded by stellar radiation.
  • GJ 1214b: A sub-Neptune orbiting a red dwarf star, with a radius of 2.7 times that of Earth and a mass of 6.5 times that of Earth. It has a moderate density (1.9 g/cm$^3$) and a low temperature (550 K), suggesting that it has a thick atmosphere of water or hydrogen-rich gas.
  • K2-18b: A sub-Neptune orbiting a red dwarf star, with a radius of 2.6 times that of Earth and a mass of 8.6 times that of Earth. It has a high density (3.3 g/cm$^3$) and a moderate temperature (280 K), suggesting that it has a small gas envelope and a large rocky core. It is also the first sub-Neptune to have water vapor detected in its atmosphere.

How do sub-Neptunes form?

The formation of sub-Neptunes is still a matter of debate among astronomers and planetary scientists. One possible scenario is that sub-Neptunes form in the outer regions of protoplanetary disks, where there is more gas and ice available, and then migrate inward due to gravitational interactions with the disk or other planets. This would explain why sub-Neptunes are often found close to their stars, in contrast to Neptune, which is far from the Sun. Another possibility is that sub-Neptunes form in situ, or in their current locations, by accreting gas and dust from the disk until they reach a critical mass that allows them to capture more gas from the disk. This would require a high enough gas-to-dust ratio and a low enough disk temperature to prevent the gas from escaping the planet's gravity.

The formation of sub-Neptunes is also influenced by the evolution of their atmospheres, which can change over time due to various processes. For example, sub-Neptunes that are close to their stars may lose some of their atmospheres due to stellar radiation and winds, which can strip away the lighter elements and leave behind a denser core. This process is known as atmospheric escape or photoevaporation, and it can explain why some sub-Neptunes have higher densities than others. On the other hand, sub-Neptunes that are farther from their stars may retain their atmospheres, or even gain more gas from the disk or from cometary impacts. This process is known as atmospheric accretion, and it can explain why some sub-Neptunes have lower densities than others.

Some of the factors that affect the formation and evolution of sub-Neptunes are:
  • The mass and luminosity of the host star: The mass and luminosity of the host star determine the amount and type of radiation and wind that the planet receives, as well as the location and width of the habitable zone. The radiation and wind can affect the atmospheric escape and heating of the planet, while the habitable zone can affect the availability of liquid water and organic molecules on the planet.
  • The distance and eccentricity of the planet's orbit: The distance and eccentricity of the planet's orbit determine the orbital period and the variation of the stellar flux that the planet receives. The orbital period can affect the tidal forces and the rotation rate of the planet, while the variation of the stellar flux can affect the atmospheric temperature and circulation of the planet.
  • The mass and radius of the planet: The mass and radius of the planet determine the surface gravity and the escape velocity of the planet, as well as the amount of gas and dust that the planet can accrete and retain. The surface gravity and the escape velocity can affect the atmospheric escape and pressure of the planet, while the amount of gas and dust can affect the composition and structure of the planet.
  • The composition and structure of the planet: The composition and structure of the planet determine the density and temperature of the planet, as well as the chemical and physical properties of the materials inside the planet. The density and temperature can affect the state and distribution of the gas, rock, and ice in the planet, while the chemical and physical properties can affect the reactions and interactions of the gas, rock, and ice in the planet.

What can sub-Neptunes tell us?

Sub-Neptunes are important for understanding the diversity and evolution of planetary systems, as they represent a large fraction of the exoplanet population and a class of planets that is absent in our solar system. By studying sub-Neptunes, we can learn more about the physical and chemical processes that shape planets, as well as the environmental factors that affect their formation and survival. Sub-Neptunes can also provide clues about the habitability and potential for life on other worlds, as some of them may have suitable conditions for liquid water and organic molecules to exist.

One of the main challenges in studying sub-Neptunes is to determine their true nature and composition, which requires precise measurements of their masses, radii, temperatures, and atmospheres. These measurements can be obtained by using various techniques, such as transit photometry, radial velocity, transit spectroscopy, and direct imaging. However, these techniques are often limited by the faintness of the planets and the brightness of their stars, as well as by the degeneracy and uncertainty of the models and parameters used to interpret the data. Therefore, more observations and better models are needed to improve our knowledge and understanding of sub-Neptunes.

Some of the questions that sub-Neptunes can help us answer are:
  • How common are sub-Neptunes in the galaxy, and how do they compare to other types of planets? According to a statistical analysis of the Kepler data, sub-Neptunes are the most abundant type of planet in the galaxy, accounting for about 50% of the planets with radii between 0.5 and 4 times that of Earth. Sub-Neptunes are also more diverse than other types of planets, as they span a wide range of masses, radii, densities, temperatures, and compositions. Sub-Neptunes are distinct from gas giants, which are much larger and more massive, and from terrestrial planets, which are much smaller and denser.
  • How do sub-Neptunes form and evolve in different types of planetary systems, and what are the implications for their habitability and potential for life? Sub-Neptunes can form and evolve in various ways, depending on the properties of their host stars, their orbital distances, their initial masses and compositions, and their interactions with other planets and the disk. Sub-Neptunes can also have different implications for their habitability and potential for life, depending on their atmospheric conditions, their surface features, and their availability of liquid water and organic molecules. Some sub-Neptunes may be too hot, too cold, or too volatile to support life, while others may have more favorable environments for life to emerge and thrive.
  • How can we improve our observations and models of sub-Neptunes, and what are the current and future challenges and opportunities in this field? Sub-Neptunes are challenging to observe and model, as they are often faint and obscured by their bright host stars, and as they have complex and uncertain structures and atmospheres. Sub-Neptunes require more data and better models to constrain their properties and compositions, and to understand their formation and evolution. Sub-Neptunes also offer many opportunities for scientific discovery and exploration, as they are the most common and diverse type of planet in the galaxy, and as they can provide insights into the origin and nature of life in the universe.
Sub-Neptunes are a fascinating and diverse class of planets that are smaller than Neptune, but larger than Earth. They are the most common type of planet in our galaxy, and they can have different compositions, densities, temperatures, and orbits. Sub-Neptunes are important for studying the formation and evolution of planetary systems, as well as the habitability and potential for life on other worlds. However, sub-Neptunes are also challenging to characterize and understand, as they require more data and better models to reveal their true nature and properties.

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