K2-141b (also designated EPIC 246393474.01) is a massive rocky exoplanet orbiting extremely close to a K Type orange main-sequence star K2-141. The planet was first discovered by the Kepler space telescope during its K2 “Second Light” mission and later observed by the HARPS-N spectrograph. It is classified as an ultra-short period planet (USP) and is confirmed to be terrestrial in nature. Its high density implies a massive iron core taking up between 30% and 50% of the planet's total mass.[3]
| Discovery | |
|---|---|
| Discovery site | Kepler Space Observatory |
| Discovery date | 2018 |
| Transit | |
| Orbital characteristics | |
| 0.00716 +0.00055 −0.00065 AU[1] (1,071,000 +82,000 −97,000 km) | |
| Eccentricity | 0[1] |
| 0.2803244 ± 0.0000015 d (24,220.03 ± 0.13 s; 6.727786 ± 3.6×10−5 h)[1] | |
| Inclination | 86.3 +2.7 −3.6[1] |
| Star | K2-141 |
| Physical characteristics | |
| 1.51±0.05[1] R🜨 | |
| Mass | 5.08±0.41[1] ME |
Mean density | 8.2 ± 1.1 g/cm3 (4.74 ± 0.64 oz/cu in) [1] |
| 2.23 +0.35 −0.31 g | |
| Albedo | ~0.28±0.07 |
| Temperature | 2,039 K (1,766 °C) (equilibrium)[1] 3,270 K (3,000 °C) (day side) 73 K (−200.2 °C) (night side)[2] |
Characteristics
editMass and radius
editLike the majority of known exoplanets, K2-141b was detected using the transit method, where a planet blocks a tiny fraction of its star's light as it passed between our line of the sight and its host. This method is only able to determine the radius of the planet, not its mass. However, K2-141b was also detected by the radial velocity method using the HARPS-N spectrograph. Therefore, its mass could also be determined along with its radius. The planet is classified as a Super-Earth, being significantly larger and more massive than Earth but not as large as the ice giants Uranus and Neptune. K2-141b has a radius of 1.51 R🜨, below the 1.6 R🜨 threshold where most planets are expected to accumulate thick hydrogen and helium atmospheres, transforming them into mini-Neptunes. The planet's mass confirms that it is rocky. It has a mass of 5.08 ME, which gives K2-141b a high density of 8.2 g/cm3, about 1.48 times the density of Earth. This high density implies a composition with a large iron core taking up about 30% to 50% of the planet's total mass.[3]
Orbit
editK2-141b has one of the shortest known orbital periods of any confirmed exoplanet. With an orbital period of only 6.7 hours, it is the shortest-period planet known to date with a precisely determined mass.[4] Only a few planets, including those around Kepler-70, have shorter orbital periods. At this proximity, K2-141b is most likely tidally locked with its host star, meaning that the same side of the planet always faces the star. It has a semi-major axis of 0.00716 +0.00055
−0.00065 AU. For a comparison, Mercury's perihelion is 0.307499 AU, more than 41 times farther away from the Sun.
Atmosphere and climate
editDespite its terrestrial nature, K2-141b is far from habitable. Its extremely close proximity to its host star has resulted in an equilibrium temperature of about 2,039 K (1,766 °C; 3,211 °F).[3] However, the actual temperature is probably much higher. About two-thirds of K2-141b faces perpetual daylight. The night side experiences frigid temperatures of below −200 °C (73.1 K; −328.0 °F). The day side of the exoplanet, at an estimated 3,000 °C (3,270 K; 5,430 °F), is hot enough to not only melt rocks but vaporize them as well.[5] A low albedo of around 0.3 means most light which hits the planet is absorbed, adding to the heat of the dayside.[6]
K2-141b is believed to have both an atmosphere and oceans, which are magma and likely tens of kilometers deep. The makeup of the atmosphere is unknown but likely consists of vaporized metals which are common in solid form on Earth. The atmosphere is believed to have extreme wind speeds of over 1.75 kilometers per second. Temperatures are high enough that the magma in the oceans can vaporize into the atmosphere. The mineral vapor formed by evaporated rock is swept to the frigid night side by supersonic winds and rocks "rain" back down into a magma ocean. The resulting currents flow back to the hot day side of the exoplanet, where rock evaporates once more.[5] If the planet's atmosphere has high levels of sodium, then solid sodium might slowly slide towards the planet's oceans, similarly to how glaciers move on Earth.[2]
Host star
editK2-141 is an K5 main-sequence star about 61 parsecs (202 light years) away, in the direction of the constellation Pisces. Based on the spectral type (K5/6 D) of the star, the star's colour is orange.[7] It has a radius of 0.681 ±0.018 R☉ and a mass of 0.708 ±0.028 M☉. It has a temperature of 4,599 ±79 K and is between 1.6 and 12.9 billion years old.[3] For comparison, the Sun has a temperature of 5778 K and is 4.5 billion years old.
See also
editReferences
edit- ^ a b c d e f g h "K2-141 b CONFIRMED PLANET OVERVIEW PAGE". NASA Exoplanet Archive. Retrieved 2018-03-05.
- ^ a b Nguyen, T Giang; Cowan, Nicolas B.; Banerjee, Agnibha; Moores, John E. (4 November 2020). "Modelling the atmosphere of lava planet K2-141b: implications for low- and high-resolution spectroscopy". Monthly Notices of the Royal Astronomical Society. 499 (4): 4605–4612. arXiv:2010.14101. doi:10.1093/mnras/staa2487. Retrieved 22 June 2021.
- ^ a b c d Malavolta, Luca; et al. (2018). "An Ultra-short Period Rocky Super-Earth with a Secondary Eclipse and a Neptune-like Companion around K2-141". The Astronomical Journal. 155 (3). 107. arXiv:1801.03502. Bibcode:2018AJ....155..107M. doi:10.3847/1538-3881/aaa5b5. S2CID 54869937.
- ^ Barragán, O.; Gandolfi, D.; Dai, F. (April 2018). "K2-141 b A 5-M🜨 super-Earth transiting a K7 V star every 6.7 h". Astronomy & Astrophysics. 612. A95. arXiv:1711.02097. doi:10.1051/0004-6361/201732217. S2CID 119473627.
- ^ a b "Supersonic winds, rocky rains forecasted on lava planet News". McGill University Newsroom. McGill University. Retrieved 22 June 2021.
- ^ Zieba, S.; Zilinskas, M.; Kreidberg, L.; Nguyen, T. G.; Miguel, Y.; Cowan, N. B.; Pierrehumbert, R.; Carone, L.; Dang, L.; Hammond, M.; Louden, T.; Lupu, R.; Malavolta, L.; Stevenson, K. B. (2022-08-01). "K2 and Spitzer phase curves of the rocky ultra-short-period planet K2-141 b hint at a tenuous rock vapor atmosphere". Astronomy & Astrophysics. 664: A79. arXiv:2203.00370. Bibcode:2022A&A...664A..79Z. doi:10.1051/0004-6361/202142912. ISSN 0004-6361. S2CID 247187527.
- ^ "K2-141 - Universe Guide". Guide to Space, Planets and the Rest of the Universe. Retrieved 22 June 2021.
