Bejad
0
Gas Giant
Magnetic FieldExtreme Activity
Why is this a Gas Giant?Your planet has 62.5% hydrogen and helium, combined with a mass of 23.0x Earth, which exceeds the gas giant threshold.
Gas giants form when massive cores capture enormous atmospheres of light gases. They typically form beyond the 'frost line' where volatiles can condense.
Classification Criteria:
✓ Hydrogen + Helium: 62.5% (>60% required)✓ Mass: 23.0x Earth (>10x required)
Habitability ScoreExtremely Harsh
Contributing Factors
water15
No solid surface — any water is locked in a supercritical mantle and hot ice, not oceans
geology50
Extreme volcanic activity may be hazardous (tidal flexing sustains geologic activity)
rotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only
Organic Chemistry20
Limited organic chemistry potential
atmosphere12
Hydrogen-rich atmosphere typical of gas giants (partially stripped by slow rotation)
temperature75
Challenging but potentially habitable temperature (large moon stabilizes the axial tilt - steady seasons)
magnetic Field100
Magnetic field provides radiation protection (a large close moon may help stir the core dynamo (speculative)) — but the pulsar's beams bathe this orbit in hard X-rays
Physical Properties
Mass
23.00x Earth (1.37e+26 kg)Radius
2.84x Earth (18,118 km)Surface Gravity
2.84x Earth (27.9 m/s²)Surface Temperature
254 K (-19 °C / -3 °F)Rotation Period
50.0 hours/day (slower than Earth)Orbital Environment
Star Type
NS-type (Neutron Star)Distance from Star
0.12 AU (18 million km)Orbital Period
13 daysTime Dilation
Clocks run 5.5 seconds per year slower than deep space — about 7 minutes over a lifetimeAtmosphere
Hydrogen and helium dominated with trace methane and ammonia
Elemental Composition
H - Hydrogen
50.0%
N - Nitrogen
12.5%
O - Oxygen
12.5%
Surface Characteristics
No solid surface - thick gaseous envelope with possible rocky core deep withinClosest Real Exoplanet
Kepler-712 c92% similar
Orbiting Kepler-712| Yours | Kepler-712 c | |
|---|---|---|
| Mass | 23.0 × Earth | 21.0 × Earth |
| Radius | 4.60 × Earth | 4.85 × Earth |
| Density (composition) | 1.30 g/cm³ | 1.01 g/cm³ |
| Temperature | 253.8 K | 236.0 K |
| Starlight received | 0.69 × Earth | 0.66 × Earth |
| Star temperature | — | 5,148 K |
MoonsLife may exist on a moon
Moon 1rings0.025% - 5.0 radii
Inside the synchronous orbit: it spiraled inward and was torn apart at the Roche limit (Phobos's fate).
Moon 2recedingOcean world - life3.5% - 13.6 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
Tidal heat sustains a subsurface ocean over a rock seafloor: a strong candidate for life (Europa-like, 87/100).