Blogs, Geothermal, Hydropower

Experiment stop.

This experiment should establish speed of the temperature reached of a liquid glass phase from a stone. The experiment stop has been caused by unusual thermal effect. In the range of time between minutes (10 ↔ 11,5), at temperature 408,1 C° and 503 C°, there was a temperature drop with 503 C° to 480 C° and fast growth which has made on 13th minute 615,6 C°. Cooling of volume of the received glass has shown absence of contact between electrodes, at the expense of the accepted high dielectric resistance. But, at pressure giving, experiment process has been continued in the same parameters. Feature
of growth and temperature drop consisted in a variable phase of spectral division of conditions between contacts. The scale of a luminescence of glass wires varied from dark red to white, including blue, light yellow, dark yellow, pink and other colors. Periodic switching-off and inclusion of various electrodes during experiment made thermogeneration between free electrodes of electric pressure adequate to consumption.    

After experiment.

Split of the glass block has opened set of metal balls of high-quality iron (Fe 89 %, Si 2 %) weight from 0,01 to two grams.  The iron maintenance in diabase
of (Fe2,5 %, Si 40 %). The insignificant expense of graphite electrodes has shown that this iron belongs to it. The chronology of distribution of temperature in stone plasma shows that iron was formed on borders of a temperature gradient in the conditions of electric field.  The width of a thermal wave corresponds to time of a spectral line. Instant thermal return created a resonance between counter thermal streams, dividing a thermal background into borders of spectral lines.

Conclusions.

Investigated thermodynamic process excludes an external high-frequency power source. Generation of the necessary frequencies dividing spectral lines, is made at the expense of structure of the module of electric charges in the conditions of the established environment. The obtained data can explain features of atmospheric layers and geothermal processes.

Results of experiment.

External temperature of the furnace:   13 min / 615,6 C° 

Fusion in rubble volume:   13 min, liquid glass, weight 2,5 kg / ~ 3500 C°

Energy expenses:    0, 22 Kw.

Difference of potentials between six electrodes: 50-70 v


Technology of modulation of electric charges.

Statement of a problem of experiment consisted in definition of interaction of the basic thermodynamic and electrodynamic processes. On the basis of statements of the problem the electrothermal element has been received. The element gross weight has made: (0,3 * 5 = 1,5 g). One of the main
statements of the problem of experiment was definition of growth rate of temperature for the established time unit.

The technical organization of experiment.

Experiment statements of the problem provided that experiment  will pass in the open environment of stone rubble (diabase), stone fraction; 5 – 10mm, weight of 13,5 Kg. An alternating voltage 50 Hz, 380v. Three phases have been doubled at the expense of three condensers 470 F (3 * 2= 6) with possibility of switching-off and inclusion of each electrode. For realization of necessary contacts between electrodes the thermoelectric element having initial resistance 500 Ω has been established. Opposite to each contact for definition of a visual spectrum, glass wires (200 X 5 mm) are placed. The open furnace in the form of the rectangular box, made of coke of oil in weight 25 Kg  with the established thermocouples.