Laythe: Difference between revisions
mNo edit summary |
mNo edit summary |
||
| (3 intermediate revisions by the same user not shown) | |||
| Line 17: | Line 17: | ||
| mass= 2.93973×10<sup>22</sup>kg |
| mass= 2.93973×10<sup>22</sup>kg |
||
| mean_density=56,144.728kg/m<sup>3</sup> |
| mean_density=56,144.728kg/m<sup>3</sup> |
||
| − | | surface_gravity=7.85m/s< |
+ | | surface_gravity=7.85m/s<sup>2</sup> (0.8g) |
| escape_velocity=2.801km/s |
| escape_velocity=2.801km/s |
||
| sidereal_rotation_period=52,980.879s 2d,2h,43m,0.9s) |
| sidereal_rotation_period=52,980.879s 2d,2h,43m,0.9s) |
||
| Line 34: | Line 34: | ||
A large circular archipelago covering over a third of the moon's surface area suggests that in the past Laythe was involved in a massive collision with another body, likely during the period of events that formed the Joolian system as it is today. |
A large circular archipelago covering over a third of the moon's surface area suggests that in the past Laythe was involved in a massive collision with another body, likely during the period of events that formed the Joolian system as it is today. |
||
| + | |||
| + | ==Atmosphere== |
||
| + | {| class="wikitable" |
||
| + | |- |
||
| + | ! Altitude (m) !! Pressure (Pa) !! Pressure (atm) |
||
| + | |- |
||
| + | | 0 || 60,795 || 0.6 |
||
| + | |- |
||
| + | | 2,500 || 47,153 || 0.465 |
||
| + | |- |
||
| + | | 5,000 || 34,495 || 0.34 |
||
| + | |- |
||
| + | | 7,500 || 24,914 || 0.246 |
||
| + | |- |
||
| + | | 10,000 || 17,786 || 0.176 |
||
| + | |- |
||
| + | | 15,000 || 9,351 || 0.092 |
||
| + | |- |
||
| + | | 20,000 || 4,782 || 0.047 |
||
| + | |- |
||
| + | | 25,000 || 2,671 || 0.026 |
||
| + | |- |
||
| + | | 30,000 || 1,507 || 0.015 |
||
| + | |- |
||
| + | | 40,000 || 363.5 || 0.004 |
||
| + | |- |
||
| + | | 50,000 || 0 || 0 |
||
| + | |} |
||
| + | |||
[[Category:Celestial Bodies]][[Category:Celestial Bodies of the Kerbol System]] |
[[Category:Celestial Bodies]][[Category:Celestial Bodies of the Kerbol System]] |
||
Latest revision as of 01:10, 12 July 2023
|
Laythe
Moon of Jool
|
|||||
|---|---|---|---|---|---|
 |
|||||
| A photograph of Laythe taken by the crew of the JFDF reconnaissance picket Serina on December 7th, 2133 while departing the moon's SOI. | |||||
| Orbital Parameters | |||||
| Apoapsis | 27,184,000m | ||||
| Periapsis | 27,184,000m | ||||
| Semi-major axis | 27,184,000m | ||||
| Orbital eccentricity | 0 | ||||
| Orbital period (sidereal) | 2.4528224 days | ||||
| Average orbital speed | 3.224km/s | ||||
| Mean anomaly | 179.909° | ||||
| Inclination | 0° | ||||
| Satellites | None | ||||
| Physical Characteristics | |||||
| Equatorial radius | 500,000m | ||||
| Circumference | 3,141,593m | ||||
| Surface area | 3.1415927×1012m2 | ||||
| Mass | 2.93973×1022kg | ||||
| Mean density | 56,144.728kg/m3 | ||||
| Surface gravity | 7.85m/s2 (0.8g) | ||||
| Escape velocity | 2.801km/s | ||||
| Sidereal rotation period | 52,980.879s 2d,2h,43m,0.9s) | ||||
| Solar day | 21,600s (6h,0m,0s) | ||||
| Axial tilt | 0° | ||||
| Surface equivalent dose rate | 0.359μSv/h | ||||
| Surface atmospheric pressure | 60.7950kPa (0.6 atm) | ||||
| Sphere of influence | 3,723,645m | ||||
| History | |||||
| Discovered | March 29th, 1754, Ezhrack Coralde Kerman | ||||
| Landed upon | April 22, 2054 | ||||
Laythe is the first moon of Jool and one of only two bodies in the Kerbol System to sustain liquid surface water. Aside from Kerbin, it is the only celestial body known to possess an oxygen rich breathable atmosphere. Approximately 87% of the moon's surface is covered by oceans. Laythe is locked an orbital resonance with the two other largest Joolian moons, Vall and Tylo.
While fossil records of large indigenous aquatic organisms have been found, when the moon was first landed on in 2054 by Grestian settlers it was found to be devoid of all life. Since falling under the jurisdiction of the Joolian Federation, several ecosystem seeding projects have been carried out, and Laythe now supports small patches of free growing vegetation and animal species.
A large circular archipelago covering over a third of the moon's surface area suggests that in the past Laythe was involved in a massive collision with another body, likely during the period of events that formed the Joolian system as it is today.
Atmosphere
| Altitude (m) | Pressure (Pa) | Pressure (atm) |
|---|---|---|
| 0 | 60,795 | 0.6 |
| 2,500 | 47,153 | 0.465 |
| 5,000 | 34,495 | 0.34 |
| 7,500 | 24,914 | 0.246 |
| 10,000 | 17,786 | 0.176 |
| 15,000 | 9,351 | 0.092 |
| 20,000 | 4,782 | 0.047 |
| 25,000 | 2,671 | 0.026 |
| 30,000 | 1,507 | 0.015 |
| 40,000 | 363.5 | 0.004 |
| 50,000 | 0 | 0 |