K2-137b


K2-137b is a hot, iron-rich, rocky exoplanet around the red dwarf K2-137 in the constellation Virgo about from Earth. It orbits the star very rapidly, with an orbital period of, at a distance of just. It has received the Guinness [World Record] for the shortest orbital period for a confirmed planet, though the planetary candidate KOI-1843.03 has a period four minutes shorter.

Physical properties

K2-137b is a sub-Earth in terms of radius. The discovery paper gives an estimate of , similar to Venus, whereas Adams et al. provides a smaller value of , slightly larger than Mars. If the latter is true, this would be one of the smallest exoplanets discovered so far. Despite the small size, it is somewhere between 1.01 and 2.80 times as massive as Earth, comparable to some super-Earths. Because it has yet to be disrupted by tidal forces from the host star, it can be inferred that iron makes up at least % of its mass. Still, the planet is tidally stretched to an aspect ratio of between 1.21 and 1.66. Its equilibrium temperature is approximately, hot enough to melt silicate minerals.
While K2-137b itself displays no signs of evaporation, such iron-rich USP planets may be higher-mass counterparts to disintegrating planets e.g., Kepler-1520b.

Host star

The planet orbits a red dwarf star, K2-137, with the spectral type M3V. Smith et al. gives it a mass of, a radius of, and an effective temperature of, while Adams et al. presents a substantially smaller mass of but a slightly hotter temperature of.

Formation

Several hypotheses exist as to how K2-137b became such an iron-rich, short-period planet. It could have been stripped of its outer silicate layers through high-velocity giant impacts, much like how Mercury came to have a high iron content according to several theories. Such collisions are projected to be common among USP planets due to high orbital speeds, reaching 270 km/s for K2-137b compared to the 29.8 km/s of Earth. On the other hand, it may have formed out of iron-rich material. Matter near the inner edge of the protoplanetary disk could be enriched in iron due to iron condensing at higher temperatures than enstatite and photophoresis separating iron grains from silicate grains by the difference in thermal conductivity. Finally, it is possible that the planet is situated at the Roche limit and has been slowly losing the silicate crust and mantle to Roche lobe overflow as its orbit slowly decays.