Viktor Schauberger Work Explained

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9.3 Temperature Nutrient Supply Gradients and 9: The Hydrological Cycle 125 reduces the capacity of the groundwater to rise as high as it might otherwise do were the trees left untouched. If the temperature of the incident rainwater is, say, +18°C and the tem- perature of the receiving ground surface +20°C, the rain will not penetrate, but will flow off laterally to areas where it can, always presuming that a healthy balance between open space and forest has been maintained. In such a case problems of salinity will be kept to a minimum, since the overall level of the groundwater table is not unduly affected. It does rise, however, under the areas where the trees have been removed, due to the geot- hermally induced upward pressure from below and the reduction in the quantity of overburdening groundwater lying above the +4°C centre-stratum. In other words the coun- teracting downward pressure has been dimin- ished. (This effect is discussed in more detail in chapter 10.) As this water rises so too are the salts elevated, though in this case not into the root-zone of the vegetation. However, if all the trees are removed (fig. 9.5), then there is no rainwater penetration at all, the groundwater table initially rises, bringing up all the salts with it, only eventually to sink or disappear altogether, because under these conditions no recharge is possible. This is how oversalination of the soil occurs, and the only way the prob- lem can be remedied is to recreate a positive temperature gradient through reafforestation. In the beginning such trees will have to be pioneer, salt-loving trees and other primi- tive plants, such species being the only ones that can survive under such conditions. Later, as the soil climate improves and its salt con- tent diminishes, other species of tree can replace them since, over a period of time and due to the cooling of the ground by the shad- ing of the pioneer trees, the rainwater enters the ground, taking the salts with it. Eventually the pioneer trees die off, because the evolved soil conditions are now no longer suitable, and the dynamic balance of Nature is restored. Irrigation only exacerbates the problem, because during the night the ground temper- atures cool somewhat, allowing the irrigation water to percolate a certain distance into the upper, now salt-containing strata. There it collects the salts and, with the increase in We shall now examine the temperature gradients in the ground and their effects in connection with figs. 9.3, 9.4 & 9.5, because the solution, transport and deposition of nutri- ents are all functions of the temperature gradi- ent. Positive and negative temperature gradients produce opposite effects. The direc- tion of the temperature gradient indicates the direction of movement. The direction of energy or nutrient transfer is always from heat to cold. Vikttor Schauberger's important principle on this subject states that under the exclusion of light air the precipitation of salts and min- erals occurs with cooling, whereas with expo- sure to light and air precipitation takes place with heating. In both cases the highest quality matter is precipitated last. In the former case all the various nutrients and salts are deposited well below the ground surface as the water cools to +4°C. In the latter case, however, due to heat-evaporation and little penetration, the lowest quality nutrients are precipitated at the surface, which not only has dire conse- quences for soil fertility, but also for the proper formation of trees, as we shall see later. To recapitulate, a positive temperature gra- dient occurs when the incident rainwater is warmer than the receiving soil. This naturally implies that the soil is protected from the heat- ing effect of the Sun by trees and other vegeta- tion and, if the whole surface of the Earth is forested, then the groundwater table hugs the configuration of the ground-surface. As shown in fig. 9.3 the water infiltrates down to the lower strata, the groundwater body and aquifers are recharged, subterranean retention basins are created and the salts (shown as a dotted mass) remain at a level where they can- not contaminate the upper strata and are not damaging to those plants unable to metabolise them. Should a part of the forest be felled and the ground surface exposed to the direct light of the Sun, as in fig. 9.4, the temperature of ground in that area rises. With this in mind it is essential that if any felling is to occur, then the trees should never be cut at the top of a hill. This creates a bald patch exposed to the Sun's heat and effectively

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