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levitational current - Free Energy

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Ultimately becoming a broad river, the increasing silt content<br />

makes the water flow more sluggishly and become more opaque.<br />

This, however, protects the lower strata from the heat of the Sun.<br />

They remain cooler, retaining the spiral, vortical motion which is<br />

able to shift sediment of larger grain-size (pebbles, gravel, etc.)<br />

from the centre of the watercourse, and keep down the risk of<br />

flooding. This motion also discourages the generation of harmful<br />

bacteria and the water remains disease-free.<br />

Viktor Schauberger wrote in 1933 in his book, Our Senseless Toil,<br />

how he was able to put to practical use his discoveries about water:<br />

It is possible to regulate watercourses over any given distance<br />

without embankment works; to transport timber and other<br />

materials, even when heavier than water, for example ore,<br />

stones, etc., down the centre of such watercourses; to raise the<br />

height of the water table in the surrounding countryside and<br />

to endow the water with all those elements necessary for the<br />

prevailing vegetation. 6<br />

The temperature gradient<br />

One of Viktor Schauberger's most important discoveries was to do<br />

with temperature. He showed how small variations of temperature<br />

are as crucial to the healthy movement of water and sap as they are<br />

for the human blood. He clarified this by identifying temperature<br />

change in its relationship to the anomaly point of water +4°C<br />

(39.2°F). When the temperature departs from this anomaly point,<br />

either up or down, it is said to have a negative gradient. When it<br />

approaches the anomaly point, from either direction, or when the<br />

groundwater is colder than the air temperature, it has a positive gradient.<br />

Heat always moves towards cold.<br />

In the natural process of synthesis and decomposition in all<br />

waters, trees and other living organisms, both the rising and falling<br />

temperature gradients are active. Each form of gradient has its special<br />

function in Nature's great production; the positive (cooling)<br />

temperature gradient must play the principal role if evolution is to<br />

unfold creatively.<br />

This important factor affects all the features of a river, such as flow<br />

velocity, tractive force (shear force), sediment load, turbidity, and viscosity,<br />

and everything to do with water management generally, like its<br />

HIDDEN NATURE

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