Two Planetary Systems

Two Planetary Systems

Time for a quick taste of how the new Architect of Worlds version is turning out.

Long-time followers of this project will remember the two running examples in the draft: planetary systems named Arcadia and Beta Nine that are intended to demonstrate how the system works in practice. I’m in the process of re-working all of the examples, which should be the last step before I share the current draft with my patrons and my readers here.

Here are a couple of tables to suggest some of the results of the revised system.

Arcadia Planetary System
Orbital RadiusPlanet TypePlanet MassDensityRadiusSurface Gravity
0.254 AUTerrestrial Planet0.260.754470 km0.53 g
0.380 AUTerrestrial Planet1.751.097460 km1.28 g
0.580 AUTerrestrial Planet1.341.106800 km1.17 g
1.00 AUTerrestrial Planet0.220.744250 km0.49 g
2.12 AUPlanetoid BeltN/AN/AN/AN/A
4.08 AULarge Gas Giant4600.2084100 km2.64 g
8.12 AUMedium Gas Giant1800.07585300 km1.00 g
12.0 AUSmall Gas Giant52.00.1445800 km1.00 g
17.6 AUFailed Core2.801.138620 km1.53 g

Not too many surprises here – this resembles the previous version’s Arcadia system fairly strongly. For some context, the primary star here is a singleton K2V, with about four-fifths the mass and one-third the luminosity of Sol. The third planet (at 0.58 AU) is the Earthlike candidate that I intend to use as an example for the last portion of the design sequence.

Beta Nine Planetary System
Orbital RadiusPlanet TypePlanet MassDensityRadiusSurface Gravity
0.027 AUTerrestrial Planet1.221.096610 km1.13 g
0.038 AUTerrestrial Planet0.941.016220 km0.99 g
0.062 AUPlanetoid BeltN/AN/AN/AN/A
0.135 AUSmall Gas Giant12.00.2922000 km1.00 g
0.390 AUFailed Core2.801.168540 km1.56 g

The Beta Nine primary is an M4V red dwarf, with about 0.18 solar masses and less than 1% of Sol’s luminosity. It also has a brown-dwarf companion that cuts off planetary formation too far away from the primary. This planetary system is actually quite a bit different from the previous draft’s Beta Nine. The new model I’m using provides enough planetesimal mass for at least a small gas giant world, and it also allows for the possibility that some of that planetesimal mass “migrates” into the inner system to help form rocky worlds. So we end up with more planets this time, and the terrestrial worlds are considerably bigger.

One inspiration here is the TRAPPIST-1 planetary system. My old model didn’t have much trouble generating a planetary system like that for a small red dwarf, but it needed a pretty massive protoplanetary disk to do it. Under the new model, a red dwarf star doesn’t need an improbably big disk mass to have a chance at Earth-sized worlds. Given how many red dwarfs we’ve found with planets of significant size, I suspect the new model fits the facts better.

I’m hoping to have the new draft out as a free update for my patrons, and as an update to the version posted on this site, within a few days.

Leave a Reply

Your email address will not be published. Required fields are marked *

This site uses Akismet to reduce spam. Learn how your comment data is processed.