Key Validation
Proton
Kepler's Third Law applied to
Established Parameters from Validation 1.1
Scaling Constants
- Bohr radius: \(r_{\text{Bohr}} = 5.29 \times 10^{-11}\) m
- Optimal Oort radius: \(r_{\text{Oort}} = 77{,}852\) AU \(= 1.165 \times 10^{16}\) m
- Distance
scaling factor : \(k = r_{\text{Oort}} / r_{\text{Bohr}} = 2.20 \times 10^{26}\)
Gravitational Constants
- At SL0 (macro scale): \(G_0 = 6.674 \times 10^{-11}\) m\(^3\)/(kg\(\cdot\)s\(^2\))
- At SL-1 (atomic scale): \(G_{-1} = 5.980 \times 10^{11}\) m\(^3\)/(kg\(\cdot\)s\(^2\))
G Scaling Relationship (Empirical)
\(G_{-1} = G_0 \times k^{5/6}\)
Ratio: \(G_{-1} / G_0 = 8.96 \times 10^{21}\)
The 5/6 power was derived empirically to match observed spectral frequencies.
Nuclear Mass
- Proton
mass : \(M_{\text{proton}} = 1.673 \times 10^{-27}\) kg
Planetron Orbital Radii Calculation
Using the scaling relationship:
\(r_{\text{planetron}} = r_{\text{Bohr}} \times (r_{\text{planet,solar}} / r_{\text{Oort}})\)
Solar System Planetary Distances
| Planet | Distance (AU) | Distance (m) |
|---|---|---|
| Mercury | 0.39 | \(5.83 \times 10^{10}\) |
| Venus | 0.72 | \(1.08 \times 10^{11}\) |
| Earth | 1.00 | \(1.50 \times 10^{11}\) |
| Mars | 1.52 | \(2.27 \times 10^{11}\) |
| Jupiter | 5.20 | \(7.78 \times 10^{11}\) |
| Saturn | 9.54 | \(1.43 \times 10^{12}\) |
| Uranus | 19.19 | \(2.87 \times 10^{12}\) |
| Neptune | 30.07 | \(4.50 \times 10^{12}\) |
Calculated Planetron Radii in Hydrogen Atom
| Planetron | \(r_{\text{planet}}\) (m) | \(r_{\text{planetron}}\) (m) | Ratio to Bohr |
|---|---|---|---|
| Mercury | \(5.83 \times 10^{10}\) | \(2.65 \times 10^{-16}\) | 0.00501 |
| Venus | \(1.08 \times 10^{11}\) | \(4.90 \times 10^{-16}\) | 0.00926 |
| Earth | \(1.50 \times 10^{11}\) | \(6.81 \times 10^{-16}\) | 0.01287 |
| Mars | \(2.27 \times 10^{11}\) | \(1.03 \times 10^{-15}\) | 0.01952 |
| Jupiter | \(7.78 \times 10^{11}\) | \(3.53 \times 10^{-15}\) | 0.06679 |
| Saturn | \(1.43 \times 10^{12}\) | \(6.48 \times 10^{-15}\) | 0.12255 |
| Uranus | \(2.87 \times 10^{12}\) | \(1.30 \times 10^{-14}\) | 0.24649 |
| Neptune | \(4.50 \times 10^{12}\) | \(2.04 \times 10^{-14}\) | 0.38619 |
Key result: Mercury
Nucleus Size Constraint
Upper Bound from Mercury Orbit
The nucleus must fit inside the innermost
\(r_{\text{nucleus}} \lt r_{\text{Mercury}} = 2.65 \times 10^{-16}\) m
This is our hard constraint \(\unicode{x2014}\) the nucleus cannot be larger than this without interfering with the Mercury planetron's orbit.
Comparison to Bohr Radius
The Mercury planetron orbits at only 0.5% of the Bohr radius:
\(r_{\text{Mercury}} / r_{\text{Bohr}} = 0.00501\)
This means the nucleus is much smaller than the traditional "
Nucleus Mass from Kepler's Third Law
Kepler's Third Law
For any
\(T = 2\pi \sqrt{r^3 / (G_{-1} \times M_{\text{nucleus}})}\)
Equivalently:
\(M_{\text{nucleus}} = 4\pi^2 r^3 / (G_{-1} T^2)\)
Using Mercury Planetron Data
From Validation 1.1, Mercury planetron:
- Orbital radius: \(r = 2.65 \times 10^{-16}\) m
- Orbital frequency: \(f = 1.17 \times 10^{15}\) Hz
- Orbital period: \(T = 1/f = 8.55 \times 10^{-16}\) s
Calculation
\(M_{\text{nucleus}} = 4\pi^2 (2.65 \times 10^{-16})^3 / [(5.98 \times 10^{11})(8.55 \times 10^{-16})^2]\)
\(M_{\text{nucleus}} = 4\pi^2 \times 1.86 \times 10^{-47} / [5.98 \times 10^{11} \times 7.31 \times 10^{-31}]\)
\(M_{\text{nucleus}} = 7.34 \times 10^{-46} / 4.37 \times 10^{-19}\)
\(M_{\text{nucleus}} = 1.68 \times 10^{-27}\) kg
Comparison to Proton Mass
Standard proton
Match:
\(M_{\text{nucleus,calculated}} / M_{\text{proton}} = 1.68 \times 10^{-27} / 1.673 \times 10^{-27} = 1.004\)
Error: 0.4%
This is excellent validation \(\unicode{x2014}\) our Kepler calculation recovers the known proton mass.
Nucleus Radius Estimation
Approach 1: Assume Maximum Size (Conservative)
If we assume the nucleus is as large as possible without interfering with Mercury:
\(r_{\text{nucleus,max}} = r_{\text{Mercury}} = 2.65 \times 10^{-16}\) m
This gives minimum density (most conservative estimate).
Approach 2: Solar Analog Scaling (Main Sequence)
If nucleus were like current Sun (main sequence):
- Sun radius: \(R_\odot = 6.96 \times 10^{8}\) m
- Sun
mass : \(M_\odot = 1.99 \times 10^{30}\) kg
Scaling to proton mass:
\(r_{\text{nucleus,sun-like}} = R_\odot \times (M_{\text{proton}} / M_\odot)^{1/3}\)
\(r_{\text{nucleus,sun-like}} = 6.96 \times 10^{8} \times (8.41 \times 10^{-58})^{1/3}\)
\(r_{\text{nucleus,sun-like}} = 1.41 \times 10^{-10}\) m
Problem: This is \(2.7\times\) larger than Bohr radius.
This can't be right \(\unicode{x2014}\) it would be \(531\times\) larger than the Mercury orbit constraint.
Conclusion:
White Dwarf / Iron Core Scaling
White Dwarf Properties
White dwarfs represent a compact stellar configuration analogous to
- Dense iron-rich core from progressive enrichment through repeated transition cycles
- Collapsed under gravity
- Supported by degeneracy pressure at the relevant similarity level
- Much smaller and denser than main sequence stars
Typical white dwarf:
Mass : \(\sim 0.6\, M_\odot\)- Radius: ~5,000 - 10,000 km (Earth-sized!)
- Density: \(\sim 10^{6}\) g/cm\(^3\) (million times denser than Sun)
Radius Scaling
Empirical relationship: For similar mass, white dwarf radius is about 1/100th of main sequence radius.
\(r_{\text{white dwarf}} \approx r_{\text{main sequence}} / 100\)
Applying to Nucleon
If the nucleon iron core is like a white dwarf analog (compact iron-rich remnant from
\(r_{\text{nucleus,iron core}} = r_{\text{nucleus,sun-like}} / 100 = 1.41 \times 10^{-10} / 100\)
\(r_{\text{nucleus,iron core}} = 1.41 \times 10^{-12}\) m
Check against Mercury constraint:
\(r_{\text{nucleus,iron core}} / r_{\text{Mercury}} = 1.41 \times 10^{-12} / 2.65 \times 10^{-16} = 5{,}320\)
The nucleus iron core is \(5{,}320\times\) smaller than the Mercury orbit. This is physically reasonable \(\unicode{x2014}\) plenty of room for Mercury to orbit.
Note: Per the
Best Estimate for Nucleus Radius
\(r_{\text{nucleus}} \approx 1.4 \times 10^{-12}\) m
Nucleon Density Calculation
Using White Dwarf Scaled Radius
\(\rho_{\text{nucleon}} = M_{\text{nucleus}} / V_{\text{nucleus}} = M_{\text{proton}} / [(4/3)\pi\, r_{\text{nucleus}}^3]\)
\(\rho_{\text{nucleon}} = 1.673 \times 10^{-27} / [(4/3)\pi\, (1.4 \times 10^{-12})^3]\)
\(\rho_{\text{nucleon}} = 1.673 \times 10^{-27} / 1.15 \times 10^{-35}\)
\(\rho_{\text{nucleon}} = 1.45 \times 10^{8}\) kg/m\(^3\)
Comparison to Solar Density
Sun's average density: \(\rho_\odot = 1{,}408\) kg/m\(^3\)
\(\rho_{\text{nucleon}} / \rho_\odot = 1.45 \times 10^{8} / 1{,}408 = 1.03 \times 10^{5}\)
This matches the white dwarf scaling \(\unicode{x2014}\) white dwarfs are typically \(10^{6}\) times denser, and we're getting \(10^{5}\) here (same order of magnitude).
Comparison to White Dwarf Density
Typical white dwarf density: \(\rho_{\text{WD}} \sim 10^{9}\) kg/m\(^3\)
\(\rho_{\text{nucleon}} / \rho_{\text{WD}} = 1.45 \times 10^{8} / 10^{9} = 0.145\)
Our nucleon is about 1/7th the density of a typical white dwarf.
This makes sense! White dwarfs have much more
Summary: Key Results
What We've Calculated
| Property | Value | Notes |
|---|---|---|
| Mercury at \(2.65 \times 10^{-16}\) m | Innermost orbit | |
| Nucleus mass | \(1.68 \times 10^{-27}\) kg | Matches proton within 0.4%! |
| Nucleus radius | \(\approx 1.4 \times 10^{-12}\) m | White dwarf scaling |
| \(1.45 \times 10^{8}\) kg/m\(^3\) | \(100{,}000\times\) denser than Sun |
Key Validations
- Kepler calculation recovers known proton mass
- White dwarf scaling gives physically reasonable nucleus
iron core size - Nucleus iron core fits comfortably inside Mercury orbit (\(5{,}320\times\) smaller)
- Density ratio matches white dwarf vs main sequence comparison
Significance for Maxwell's Equations
We now have the critical value for Gauss's Law derivation:
\(\rho_{\text{nucleon}} = 1.45 \times 10^{8}\) kg/m\(^3\)
This validated framework connects to:
- Gauss's Law: Uses nucleon density in derivation
- G Scaling: Explains why \(G_{-1} = G_0 \times k^{5/6}\)
Connections to Other AAM Principles
Related Topics
- Hydrogen Spectral Analysis: Source of
planetron orbital frequencies. - Iron Star G Scaling: Explains the 5/6 exponent origin.
AAM Axiom References
| Axiom | Version | Key Concepts Used |
|---|---|---|
| Axiom 1 \(\unicode{x2014}\) The Foundation of Physical Reality | v1.6 | Chirality-surplus/deficit dual mechanism for |
| Axiom 3 \(\unicode{x2014}\) The Nature of Matter | v1.2 | |
| Axiom 7 \(\unicode{x2014}\) The Nature of Energy | v2.3 | |
| Axiom 10 \(\unicode{x2014}\) Self-Similarity Across Scales | v2.3 | SSP: nucleons are active stars with iron cores, not dead/settled objects; basin of convergence; |