The simulation assigns points to represent units of Planck mass rotating around each other. All points orbit each other forming n-body orbital pairs. To reproduce 2-body orbits we can clump a set of points in near vicnity (the orbited mass) and assign 1 point at a distance, the orbiting mass. For example we could do a simple earth-moon orbit by setting 81 points in near vicinity and 1 point at greater distance given that the earth-moon mass ratio is 81:1. This would then be mapped as a 2-body orbit although the simulation itself is still rotating all 82 points around each other (i.e.: for the simulation this is still an 82-body orbit).
The files are in this directory: nbody orbitals.
For a discussion of the theory see Article 3 or the wiki mirror site #Orbital_formulas_(2-D_plane)
The elliptical orbit version simulation is the same program as for 2-body orbits but with an extra function, orbitals can travel either clock-wise or anti-clockwise. By choosing the ratio of clock-wise:anti-clockwise orbitals the degree of eccentricity can be controlled. The ratio 108:1 (kcurve = 108) gives an eccentricity close to Mercury.
The files are in this directory: elliptical orbits.
For a discussion of the theory see Article 3 or the wiki mirror site #Orbital_alignment
We can compare this simulation with a standard Newtonian simulation (note. still under development).
The files are in this directory: Newtonian orbits.
For a discussion of the theory see Article 3 or the wiki mirror site #Orbital_vs_Newton
By changing the 2-body gravitational orbital simulation angle of rotation from a reduced mass component to a fixed alpha component, atomic orbital transitions can be mapped as specifc gravitation orbits. The proton is represented by a clump of of points in near vicnity and the electron is assigned as 1 point at a distance defined by alpha and the proton-electron wavelength. In the default given, the proton is represented by 65 points, as the program is still simulating a 66-point orbit, a larger central mass requires proportinately more computation time and so this number was choosen as a comprise. users can select as they wish, although n-body orbits are not always stable and some expermentation with initial positions may be helpful. The simulation can also be divided into a 4-body orbit (3-quarks + 1 electron), again simply by modifying the start positions.
The files are in this directory: Atomic orbital transitions.
For a discussion of the theory see Article 3 or the wiki mirror site #Atomic_orbitals
By testing both alpha and Omega as free parameters we can investigate optimal values and compare with theorectical. Also the base-15 conjecture is studied.
The files are in this directory: Physical constant anomalies.
For a discussion of the theory see Article 6.
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