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Showing posts with the label TRAPPIST-1c

The Bare Carbonate Plains and Airless Crust of TRAPPIST-1c

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Deep within the constellation of Aquarius, approximately 40 light-years from Earth, lies one of the most intensively studied planetary systems in modern astrophysics: the TRAPPIST-1 system . At the heart of this compact stellar family is an ultra-cool red dwarf star , orbited by seven rocky, Earth-sized worlds. Among these, TRAPPIST-1c stands out as a critical laboratory for understanding the limits of planetary atmosphere retention, crustal geology, and the intense physical forces that shape terrestrial worlds orbiting low-mass stars. Discovered via the transit method , this exoplanet offers researchers an unprecedented look at a dry, highly irradiated rocky surface stripped of its primary volatile envelope. TRAPPIST-1c orbits its host star at a distance of just 0.0158 astronomical units (AU), completing a full revolution in a mere 2.42 Earth days. Because of its extreme proximity to the stellar primary, the planet is subjected to immense gravitational forces and high-energ...

The Scorched Basaltic Surface and Bare Crust of Exoplanet TRAPPIST-1c

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TRAPPIST-1c , cataloged designated as 2MASS J23062928-0502285 c , is a confirmed terrestrial exoplanet orbiting an ultra-cool M-dwarf star located approximately 39.6 light-years from Earth in the constellation Aquarius. Discovered in 2016 through ground-based transit photometry by the Transiting Planets and Planetesimals Small Telescope (TRAPPIST) project , TRAPPIST-1c has become a foundational object in comparative planetology . With a radius approximately 1.097 times that of Earth and a mass measured at 1.308 Earth masses, the planet possesses a mean bulk density of roughly 5.49 grams per cubic centimeter. This density closely aligns with a terrestrial mantle-to-core mass ratio, confirming that TRAPPIST-1c is a solid, iron-rich rocky planet rather than a volatile-rich sub-Neptune. Orbital Mechanics and Tidal Synchronization Positioned at a semi-major axis of ju...

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