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Ion Wave Power Generator - Aqueous, Kinetic Power Plant

  • Sydney Matinga
  • Jan 30
  • 3 min read

Updated: Feb 6

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Refer to the post, Terms of Use Agreement Xerqon Technologies, WIX Blog 2025, for early, legal due diligence.



Thought Experiment


Technical Considerations

All power generation and work circuitry should operated via a unique/private power network to prevent power, quantum leakage. Power will always depend on some sort of change of potential to generate. Constant change comes from cyclical change or specifically, wave dynamics in momentum. It may offer an industrial level of renewable power production at markedly accessible entry cost.


Marine waves are ionic, and they generate as much power as their relationships indicate, below:


E = total energy

U = potential energy

K = kinetic energy

b = breadth of the wavefront

d = wavefront, maximum height

h = displacement shift, phase shift / Pi , φ / Pi


U [gravity] = m * g * d , where h is reserved for a constant of another dimensions


P [gravity] = b * g * d * sin ^2 ( λ * Pi ( f + h ) ) , Q * v / T




Experimental Dynamic

The best way to model a realistic outcome is to apply arbitrary values to rigorously placed dimensions and derived constants of the same.


P = Power

m ~ 1.025 * 10 ^2 kg / ( 1 m^3 ) / s )

b = 1.2 * 10 ^ 2 m

d = 7.5 * 10 ^ -1 m

f = 1 Hz

h = 0 m

λ = 9.5 * 10 ^ -1 m

g ~ 9.81 m/s ^ 2


P [gravity] = (( 100 kg / ( 1 m^3 ) / s ) * (1.2 * 10 ^2 m * 7.5 * 10 ^ -1 m * 9.5 * 10 ^ -1 m)

* 9.81 m/s^2 * 7.5 * 10 ^ -1 m * sin^2 (  9.5 * 10 ^ -1 m * Pi rad

* (1 Hz + 0 m ) ) ,


= 1.53943 * 10 ^ 3 W


MW Power [gravity]


~ 1.53943 * 10 ^ 3 W / (1.2 * 10 ^2 m * 7.5 * 10 ^ -1 m * 9.5 * 10 ^ -1 m) ,


1.8005 * 10 W / m ^3 for water ,


1.025 * 1.8005 * 10 W / m ^3 for sea water ,


1.8455125 * 10 W / m ^ 3



For 1 MW, Volume (V)


= 10 ^ 6 W / 1.8455125 * 10 W / m ^ 3


~ 5.4185 * 10 ^ 4 m^3


Power should be collected across a 10km breadth, on average, and for 15 wavelengths, similarly. Collection apparatus would be two horizontally, surface-placed antenna cables. They must run parallel to the elevated land mass. One antenna would be at the highest possible elevation below the waves, close to the coastline. The other would be placed some distance further towards to the fall of the continental shelf.


Establishing the height differentials is to maximise the electrical potential difference (voltage) between the antennas, base on charge differences at each of the two elevations. The voltage rise is a power amplifier. Both cables would remain completely insulated as well as any cables connecting them in a complete circuit loop, to the power grid.


Wave front rise and fall generates power to the order of the calculations above. They are cumulative - each arithmetically contributing to the whole, singular gravitational wave function of the ocean water.


Each wave generates a sinusoidal power wave. Those waves add to a superpositioned, single wave which delivers power to the collection plant. The waves will very accurately repeat the pattern while the precision of their dimensions will vary little, under almost uniform, environmental conditions.


The identical length of the twin antennas determines the power collection capacity of the plant, along with the contributing elements outlined in the descriptive portion, immediately above.



Economic & Geopolitical Conclusion

Equipment volume in this example of power generation plant is negligible by comparison with most standard power generation units, including solar collection arrays. It is the world's simplest and most ordinately affordable, renewable and very dependable power generation technology. The tides and winds as predictable as the trade winds make the power solution extremely competitive. It will ease geopolitical conflicts and concerns over energy security for the long foreseeable future of humanity.


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