Issue 17 - Free-Energy Devices

energy and the dynamics of the solar activity
influences considerably on its operation.
METHOD OF PHYSICAL SIMULATING OF
GEOELECTROMECHANICAL
PHENOMENA
In order to prove that the given theory of
geoelectromechanics is true the experimental
investigation of these natural phenomena using
the method of physical simulation with the help
of simple physical models was conducted with
further comparison of the experimental results and
accumulated by natural sciences already known
geophysical facts.
PHYSICAL MODELS, EXPERIMENTAL
PLANTS AND EXPERIMENTS
Several simple experimental plants simulating the
combined electrostatic and unipolar
electromagnetic motor-generator of the Earth in
a simplified way have been developed, mounted
and tested during operation. The information
about their structure and experimental results is
given below.
a) Simplest physical model of the unipolar Earth
generator
The modernized plant of the simple unipolar
electromagnetic Faraday generator (Fig.1) was
assembled in order to prove in experimental way
that the effect of unipolar induction arises from
EMF provided that the Earth magnetic field is
fixed in space relative to the rotating planet.
Fig. 1
It consists of the ring-shaped permanent magnet
with axial magnetization (magnet poles are
indicated with colour), which simulates magnetic
dipole of the Earth; non-magnetic, for example,
copper disk simulating current-conducting media
of the Planet located above the ring-shaped
magnet and device for forced axial rotation of this
magnet-disc couple (not shown), the device for
brush-type current collection with electrical
connection of rotation axis and disc face. The
milliammeter has been inserted between two
current collection brushes into the gap of
connecting conductor (not shown). The
experiments have been carried out for examining
the unipolar motor-generator of the Planet.
Particularly for finding out what conditions are
required for unipolar induction arising. The first
experiment represented the axial rotation of only
magnet on fixed disk. The unipolar induction has
not arisen and there was no current in circuit
between brushes. Experiment 2 consisted in
combined syncronous axial rotation of the magnet
and disk. Emf of unipolar induction has arisen and
the milliammeter has indicated the current of
certain direction.
Experiment 3 consisted in rotation of the current
–conducting disk relative to fixed magnet. The
results of measurements are the same as in
experiment 2. Then all these 3 experiments have
been repeated many times at different angles of
inclination of magnetic axes relative to axes of disk
rotation. It was found out that when the position
of magnet was inverse one (its turning was 180
degrees) the values of emf and current from disc
were the same as in experiments 2 and 3 but the
direction was opposite one. The results of
experiments while having different other angles
of rotation axis and magnetic one have shown that
while increasing this angle within range from 0 to
90 degrees the values of emf in the currentconducting
circuit were being decreased and when
the shift angle was equal 90 degrees they were
equal 0.
The conclusions concerning experiments with the
simplest physical model of the Earth unipolar
geomagnetic machine are the following ones
(Fig.1):
1.When the magnet rotation is axial one its lines
of force are fixed in space.
2.When increasing the shift angle of disk and
magnet rotation axes from 0 to 90 degrees the emf
value of the unipolar induction is being decreased.
When further turning from 90 to 180 degrees it is
again being increased but it has opposite sign.
20 New Energy Technologies, Issue #3(18) 2004