Approximation
of the terrestrial electroide size
- telemetric measured -
The electroide has a structure with real size and spherical shape.
The electroide is the consequence of the interaction between centripetal
and substance electromagnetic force.
Obviously, electromagnetism is interpreted as energy with vector properties.
The force of the attraction vectors (axial), is greater than the force
of rejection (parallel),
the difference being Newton's gravity.
The electroide is determined by this difference.
The angular electromagnetic force is the effect of centripetal acceleration
in the substance, which generates the radial electric potential.
This phenomenon does not occur inside the electroide (Meissner effect).
Therefore, the electroide is the essence of the electromagnetic bodies
in the universe.
In the case of planet earth, the radius of the sphere occupied by the
electroide (R)
can be approximated with telemetry devices, as shown in the drawing below.
Measurement benchmarks are the axis of magnetism and the lead wires, parallel
to each other.
The geometrical location of the movement of these wires around the axis,
parallel to it, should be a cylinder based on the circle of the electric
axis.
Two positions of the lead wire, parallel and collinear with the magnetic
axis,
are sufficient to determine the radius of the sphere occupied by the electroide.
The radius sought should take values between 21.3 km,
the difference of the equatorial and polar diameters and 600 km,
ie half of the diameter approximated by the seismic information.
This interpretation is much simplified, the reality being a combination
of centripetal forces.
In polar areas, the circle of centripetal forces, the combination of forces,
is distributed evenly over the plumb thresd, forming the basis of a straight
cone.
Thus, the orientation of the plumb thread is concentric with the circle
of centripetal forces.
Thus, centripetal acceleration takes the optimal, maximum possible value.
To the magnetc equator, the circle of centripetal forces becomes more
inclined,
until it enters the same plane as the magnetic equator.
In this overlap, the circle of centripetal forces mutually attenuates
their forces,
the acceleration to take the minimum possible value.
These findings have in equation the value of the sought ray,
but also the shape of the electroide and even the planet.
