top of page

MOON FORMATION

June 2019 - May 2022

This project involved research into how moons form from circumplanetary disks of moonetesimals. More specifically, it looked into how they form around earth-like planets and when multi-moon systems occur. Through the use of SyMBA, which is a numerical integrator, and a variety of sub-programs that I co-wrote in Fortran and MATLAB, this project simulated the physics of moon formation.

DIVISION OF PLANETARY SCIENCES PRESENTATION

(presented at the 2020 annual conference)

SKILLS

Programming

Fortran, MATLAB, bash, command line, debugging, compiling

Simulations

Numerical integrators, setting parameters, submitting batch jobs

Data Analysis

Analyzing matrix data, trend identification

Data Visualization

3D models in MATLAB, time lapses, scatter plots, multi-plot figures

Astronomy

Moon formation, Lindblad resonances, tidal forces, orbits

Physics

Gravitational forces, collisions, fluid-like disks

CONTEXT

01.

Collision

Growing protoplanets collide in giant impacts.

02.

Disk formation

Giant impacts make circumplanetary disks with an inner fluidlike section and an outer section of moonlets (moonetesimals).

03.

Disk accretion

Circumplanetary disks contain moonetesimals that collide to make moons.

04.

Formation parameters

We want to investigate how disk size, surface density distribution, and mass may affect the final moon system.

05.

Multi-moon systems

We want to identify which parameter values yield final systems with more than one moon.

circumplanetary disk forms moon

Credit: Ida et. al.

Circumplanetary disk

Credit: Salmon & Canup

METHODS

disk mass plots for moon formation research
disk outer bound plots for moon formation research
surface density plots for moon formation research

Simulator

We are using a numerical integrator called SyMBA to run n-body simulations of disk evolution under different parameter values.

Simulator changes

We added subroutines within our copy of SyMBA to increase the simulator's complexity. Based on the work of Salmon & Canup, we added a viscously spreading fluidlike inner disk, mass transfer between the inner and outer disks, tidal dissipation, and first-order Lindblad resonances.

Parameter values

We selected high and low values for each of our three disk parameters: initial disk mass, surface density distribution, and disk size.

Analysis

We used MATLAB to analyze the simulation results, by plotting final moon system results such as the number of moons, the final mass, and the final semi-major axis/axes.

bottom of page