Magnetic Field Extreme Activity
Why is this a Gas Giant? Your planet has 82.7% hydrogen and helium, combined with a mass of 132.0x 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.
✓ Hydrogen + Helium: 82.7% (>60% required) ✓ Mass: 132.0x Earth (>10x required)
Habitability Score Uninhabitable
Contributing Factors water 15
No solid surface — any water is locked in a supercritical mantle and hot ice, not oceans geology 40
Extreme volcanic activity may be hazardous rotation 30
Very slow rotation - severe temperature swings between eternal day and night sides Organic Chemistry 84
Core organic elements (CHNO) present (tidal pools cycle wet and dry - a boost for prebiotic chemistry) atmosphere 18
Hydrogen-rich atmosphere typical of gas giants (partially stripped by slow rotation) temperature 5
Near absolute zero - all molecular activity ceases, impossible for life (large moon stabilizes the axial tilt - steady seasons) magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
132.00x Earth (7.88e+26 kg) Radius
5.09x Earth (32,439 km) This planet: 5.09× Earth radius Earth: 1× (baseline)
Surface Gravity
5.09x Earth (49.9 m/s²) Surface Temperature
45 K (-228 °C / -379 °F) Rotation Period
26.0 hours/day (slower than Earth) This planet: 26 h/day Earth: 24 h/day Orbital Environment Distance from Star
24.40 AU (3.65 billion km) Orbital Period
144.1 years Atmosphere Hydrogen and helium dominated with trace methane and ammonia
Surface Characteristics No solid surface - thick gaseous envelope with possible rocky core deep within Moons
Moon 1 stable 0.0071% - 7.6 radii
Small and distant: a quiet, stable companion.
Moon 2 stable 0.016% - 13.6 radii
Small and distant: a quiet, stable companion.
Moon 3 receding 0.071% - 23.0 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Moon 4 receding 0.56% - 48.0 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Moon 5 receding 0.063% - 100.0 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Moon 6 rings 0.025% - 1.8 radii
Inside the Roche limit (1.79 planet radii): torn apart into a ring system.
Moon 7 rings 0.089% - 3.0 radii
Inside the synchronous orbit: it spiraled inward and was torn apart at the Roche limit (Phobos's fate).
+5 temperature: large moon stabilizes the axial tilt - steady seasons +4 chemistry: tidal pools cycle wet and dry - a boost for prebiotic chemistry