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142 Living Energies by conventional concepts, the then Austrian government became very interested in his the- ories and their practical implementation, since they might be of benefit to the country as a whole. It was therefore decided to commission Prof. Philipp Forchheimer, one of the world's foremost but recently retired hydrologists, to observe Viktor Schauberger's activities and report on them. He was to try to understand the processes, which appeared to function flawlessly, but for which there were no accepted theories. At first Viktor Schauberger was rather irri- tated at having this man trotting around after him, looking over his shoulders as it were. Forchheimer, however, was always very discreet, never asking trivial questions and eventually they became firm friends, Forch- heixner ultimately enabling the publication of Viktor's treatise on water in the Austrian hydrological journal "Die Wasserwirtschaft". During their period together, and because of Forchheimer's sincere interest, Viktor was always trying to find practical examples to teach him about the substance of water, its intrinsic nature and the peculiar phenomena under which the energies in water evolve. One day he arranged a demonstration for Forchheimer and, taking him up to a certain part of the forest, they came upon a fast- flowing mountain stream which Viktor knew to contain trout. Right in the middle of this rushing cold water at the point where the flow was fastest, Schauberger pointed to the motionless stance of a so-called 'stationary trout'. The trout was standing totally still or very nearly so, apparently managing to main- tain its station effortlessly with just an occa- sional flick of its fins. Just holding a stick over it, or even the shadow of the stick, was enough to make the trout dart upstream. The direction of escape was never downstream, but it always accelerated upstream. V ery odd, because one would normally consider movement down- stream to be the fastest avenue of escape, since movement would be with the current. But not so, the movement was always upstream against the current. Once things had settled down and danger had passed, the trout would return to its former station. Viktor asked Forchheimer to explain why the trout fled upstream instead of downstream and how it was able to do this. Unable to answer, Viktor then responded mischievously, "Well, Profes- sor, it is because it never had any academic train- ing! Were you in this gushing stream, you would be swept away!" The process by which the trout stays motionless in flowing water is as follows: The trout always seeks out that part of the water- body, that part of the current flow where the water is densest and coldest, and the longitudinal vortex most intense. Here a factor discovered by Viktor Schauberger plays a very important role, namely that the forward velocity of every particle of water is associated with a specific temperature. If it exceeds this critical velocity then turbulence results. Because of its bodily form, as each filament of water passes around the trout it accelerates and in doing so exceeds the above critical velocity relative to specific temperature. In other words, due to being deflected by the mass of the trout's body and depending on its proximity to the same, in varying degrees, each water-filament is caused to move too fast (fig. 11.2). In consequence a series of vortices are created along the trout's flanks which have a component of motion in a direction opposite to the current. The combined action of these counter movements in direct contact with the hindparts of the trout's body provides the counterthrust against the downward flow of water. A zone of negative pressure or negative thrust is created within the length of the trout's body. This negative pressure couter- acts the positive pressure of the water flow and the trout rests within the zone of neutral pressure its body has created. If the trout wants to accelerate upstream, it starts to work its gills. The flapping of the gills intensifies the vortices along its flanks, which makes the ensuing upstream thrust greater than the downward pressure. The faster it flaps its gills, the faster it moves against the current, and when its gills are going at 'full bore', so to speak, it moves upstream like a streak of lightning. The increased expulsion of oxygen-deficient, CO2-rich and therefore car- bone-rich water from the faster-functioningPDF Image | Viktor Schauberger Work Explained
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