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144 Living Energies was hot enough, Viktor Schauberger gave the signal to pour it into the stream, while he and Forchheimer continued to observe the trout's behaviour very closely. As soon as the hot water hit the stream, the trout started to flail its tail, moving backwards all the while as it struggled to maintain its station. Something drastic had happened to the water and its pat- tern of energy, which normally aided the trout in the maintenance of its position. The upward flow of levitational energy had been totally disrupted by the introduction of the hot water 150m above. The trout was no longer able to stay where it was in the fast flow without effort, as was the case before. Missing was the energy that the trout also exploits to progress upstream and to make its famous leaps, which it must do periodically in order to reach the spawning grounds, which are always to be found in the zone of high- quality water near the spring. When the hot water was introduced, this counter-movement of energy was cut. The energy was suddenly dissipated and became chaotic. All structure in terms of the natural thermal stratification of the water was lost and the regularity of the longitudinal vortex with its cold core, essential for the trout motionless stance, had been destroyed. All its valiant efforts to maintain station were in vain and it was swept down- stream. Over a certain period of time the counter-flow of energy was slowly restored through the continuing descent of cold water and eventually the trout was able to return to its former position. On another occasion, Viktor pointed out a stone in the middle of a stream and asked Forchheimer whether he thought the water would be hotter or colder after flowing past it. The Professor scratched his head and thinking to himself, "Hmm, friction; friction produces heat", answered "Hotter!" Schauberger then suggested he measure it to confirm his opin- ion, stating, however, that he thought Forch- heimer's answer was incorrect. Equipped with his accurate thermometers and first furling up his trousers, the Professor entered the water. Viktor's son, Walter, who at the time was about 16 years old, was requested to hold onto the spindly professor's belt, lest he lose his footing on the slippery stones and be swept away by the torrent. Forchheimer carefully measured the water temperature both above and below the stone and was very surprised to find there was a difference of about 2/10ths of a degree Celsius - colder on the downstream side of the stone. After a number of measure- ments were made later on, Forchheimer found that the cooling at these points varied from 0.1°C to 0.4°C. When moving naturally, water develops a series of vortices and eddies which brake its otherwise unimpeded forward movement and at the same time cool it. The steadiness of flow in naturally flowing river systems is closely associated with this vortical motion, which is due to the turbulence arising through the exceeding of the critical velocity relative to water temperature as mentioned previously. Such water will never accelerate continuously and rush headlong down a given gradient but, depending on its temperature and the type of temperature gradient in force, it will fairly quickly develop vortices and thereby slow its rate of forward flow, for the simple reason that these vortices represent the application of an automatic brake by creating a counter move- ment in an upstream direction, a phenomenon that will be explained in the following chapter. 11.3 Fishes from Eggs Another interesting aspect about the trout in that the form of its body arises from the combination of three egg-shapes, two elon- gated in the form of seeds or grain and the other in the form of an egg (fig. 11.3), all of which can be precisely calculated with the hyperbolic mathematical system devised by Walter Schauberger. We are therefore con- cerned with a complex egg-form. As was demonstrated in the measuring jar, the egg- shape does seem to have a certain affinity for vortical motion and it is very possible that the resistance of this form to forward motion, or any kind of pressure, is much less than it would be in the case of a cylindrical or an elliptical system. Here we need briefly to address Walter Schauberger's Pythagoras-Kepler System and its associated mathematics, which are are devel-PDF Image | Viktor Schauberger Work Explained
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