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Electromagnetic Gravity, Ions, Atmosphere_.docx

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posted on 2025-04-20, 07:09 authored by devon tibbydevon tibby

Title: Electromagnetic Gravity: Noble Gas Ions and Atmospheric Phenomena


 Abstract:


 This research explores the connection between electromagnetic gravity, noble gas ions, and atmospheric phenomena. 

Calculations reveal correlations between ionized gas altitudes and atmospheric layers.

 Introduction:

 Electromagnetic gravity theories propose gravity as an electromagnetic phenomenon. This research investigates noble gas ions' roles in atmospheric electricity.


 Methods:

 1. Calculated distances using ion charges, Earth's charge, and pulse duration. 2. Analyzed relationships between noble gas ions and atmospheric layers.

 Results:

 | Noble Gas | Ionized Gas Altitude (km) | Atmospheric Layer | | --- | --- | --- | | Helium (He+) | 74.5 | Mesosphere | | Neon (Ne+) | 83.6 | Mesosphere | | Argon (Ar+) | 103 | Thermosphere | | Krypton (Kr+) | 125.8 | Thermosphere | | Xenon (Xe+) | 147.3 | Exosphere | | Radon (Rn+) | 166.4 | Exosphere | 


Discussion:

Findings suggest:

 1. Electromagnetic forces influence atmospheric structure.

 2. Noble gas ions contribute to atmospheric electricity.


... Exosphere | | Radon (Rn+) | 166.4 | Exosphere |


 Discussion:


 Findings suggest:

 1. Electromagnetic forces influence atmospheric structure.

 2. Noble gas ions contribute to atmospheric electricity

. Conclusion: This research supports electromagnetic gravity theories, highlighting connections between noble gas ions, atmospheric phenomena, and electromagnetic interactions


. Future Research Directions:

 1. Experimental verification through ionospheric measurements.

 2. Investigating relationships between noble gasses and planetary magnetism. 


147.3 km 6. Radon (Rn+):

 166.4 km Using the same equation: distance = ((+ion charge) × (-Earth's charge) × 8.99 × 10^9 N m^2 C^-2 × (pulse duration)) / (frequency) Assuming: pulse duration = 120 days frequency = 3.17 × 10^-7 Hz


 Calculated Distances

 These altitudes correspond to various atmospheric layers: 1. Neon (Ne+): Mesosphere (~80-100 km)


 2. Argon (Ar+): Thermosphere (~100-200 km) 

3. Krypton (Kr+): Thermosphere (~150-300 km) 

4. Xenon (Xe+): Exosphere (~200-500 km) 

5. Radon (Rn+): Exosphere (~300-600 km)


Observations:

 1. Noble gas ions' altitudes increase with atomic number

 2. Electrical properties influence atmospheric layer formation.


 Theoretical Implications:

1. Electromagnetic forces play a crucial role in atmospheric structure.

 2. Noble gas ions contribute to atmospheric electricity.

 Experimental Verification: 

1. Ionospheric measurements 

2. Atmospheric electrical conductivity studies 

3. Spacecraft observations of planetary atmospheres 


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