No life — too hot for liquid waterMagnetic FieldExtreme Activity
Why is this a Carbon World?Your planet's carbon (47.7%) outweighs its oxygen (12.6%), so the mineralogy flips from silicate rock to carbide - a graphite crust over a diamond mantle.
Carbon worlds form in carbon-rich disks where there isn't enough oxygen to bind it all into silicates. Instead carbon condenses directly into graphite, carbides, and - under pressure at depth - diamond. They form water-poor, so no life takes hold.
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only
Organic Chemistry79
All CHNOPS elements present - building blocks of life - chlorine-laced environment attacks organic molecules (tidal pools cycle wet and dry - a boost for prebiotic chemistry)
atmosphere16
Atmosphere present but composition not ideal for life (partially stripped by slow rotation)
temperature15
Extremely hot - hostile to known life forms
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
7.60x Earth (4.54e+25 kg)
Radius
1.97x Earth (12,526 km)
Surface Gravity
1.97x Earth (19.3 m/s²)
Surface Temperature
437 K (164 °C / 327 °F)
Rotation Period
50.0 hours/day (slower than Earth)
Orbital Environment
Star Type
K-type (Orange)
Distance from Star
0.85 AU (127 million km)
Orbital Period
342 days
Atmosphere
Carbon monoxide and methane haze over a graphite surface
Elemental Composition
C - Carbon
47.7%
O - Oxygen
12.6%
H - Hydrogen
10.8%
Surface Characteristics
Graphite plains and carbide ridges over a diamond mantle - a glittering coal-black world