Kepler-248 b: A Dense Super-Earth in a Six-Day Orbit

Kepler-248 b is a massive, compact exoplanet orbiting its host star every 6.3 days, representing a distinct class of worlds.

Orbital Dynamics and Stellar Proximity

The planet maintains a tight semi-major axis of 0.06600 AU. At this distance, the stellar insolation flux reaches 79.31 times that of Earth. With an equilibrium temperature of 819 K, the surface environment remains perpetually scorched by its host star, a G-type star with a mass of 0.838 solar masses. The orbit is perfectly circular, with an eccentricity of 0.0000, which keeps the thermal input constant throughout the brief 151.40-hour orbital period.

Compositional Constraints and Density

With a radius of 3.020 Earth radii, Kepler-248 b occupies a space between terrestrial worlds and gas giants. The bulk density of 1.870 g/cm^3 is the primary indicator of its internal structure. Unlike the dense, iron-rich cores of inner solar system planets, this density suggests a significant volatile-rich mantle or a thick, high-pressure atmosphere. The planet likely possesses a massive rocky core surrounded by a deep, compressed shell of volatiles that remain in a supercritical state due to the intense heat from the host star.

Atmospheric Physics in a High-Flux Environment

At 819 K, the atmosphere of Kepler-248 b is subject to extreme thermal forcing. Atmospheric models for planets in this temperature regime predict rapid circulation patterns that redistribute heat from the dayside to the nightside. The high mass of 9.380 Earth masses provides a strong gravitational well, which helps retain the gaseous envelope against the intense stellar wind. The lack of orbital eccentricity ensures that the planet does not experience seasonal temperature swings, leading to a stable, albeit extremely hot, global climate.

Physical Takeaways

The Kepler-248 system, containing two confirmed planets, serves as a laboratory for studying the migration of massive bodies toward their host stars. The 89.90-degree orbital inclination allows for precise transit observations, which provided the data necessary to calculate these parameters. Future observations focusing on the transit depth and timing variations will continue to refine our understanding of the mass-radius relationship for planets in this specific density range.

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