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terrestrial residue

Schauberger
insulation against heat are bound into the water, which is swirled in towards the central axis by the inclined angle of the resistances - guide-vanes.[4]. Having been drawn there by the increase in axial velocity, the water-masses inwinding towards the central axis now bind the highly active dynagens, which have been released through the mutual abrasion of the carbones. No longer reacting to any mechanical centrifugence, these energised terrestrial elements then begin to encircle the centrally moving oxygenes. Through the continuous approach of the through-flowing water-masses towards the anomaly point of +4°C (+39.2°F), on the one hand the terrestrial elements attain their relatively highest energetic state and on the other, the oxygenes become increasingly indifferent and more dispersed, thus reaching the condition proper to a fertilising substance. If this state is reached at the anomaly point, then the highly energised terrestrial residues (the former carbones) bind their fertilising counter-parts, and the naturalesque product of synthesis is complete.[The Energy Evolution - Harnessing Free Energy from Nature, The Liquefaction of Coal by Means of Cold Flows]

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terrestrial

Created by Dale Pond. Last Modification: Tuesday November 8, 2022 01:26:48 MST by Dale Pond.