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Viktor Schauberger Work Explained

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128 Living Energies tion and the length of the periods of the ground's exposure to heat. There are other conditions which also pertain to nutrient flow and, while slightly out of place here, since rivers and stream management will be discussed more fully in later chapters, it nev- ertheless seems more appropriate to address them while we are on the subject. Through the corrasion and abrasion of their sediment, all healthy rivers and streams are metabolisers and transporters of nutritive material, and as such are major contributors to the supply of nutri- ents to the surrounding vegetation. However they can only impart nutrients where the con- ditions are conducive to a nutrient transfer, i.e. where a positive temperature gradient between water and ground prevails. Fig. 9.6 shows a river flowing through an entirely forested area. As an illustration the river water has a temperature range of between +10°C and +8°C from surface to riverbed. In contrast the ground temperatures under the forest are cooler, ranging from +8°C at the surface to +4°C at the level of the groundwater centre-stratum. The river water is therefore warmer than the surrounding soil, a positive temperature gradient exists and the transfer of nutrients, energy and moisture takes place from warmer to cooler regions, namely from the river in the direction of the ground. The fertility of the soil is enhanced and the groundwater table recharged. Conversely, if the opposite condition of a negative temperature gradient prevails as shown in fig. 9.7, then the flow of energy, moisture and nutrients proceeds from the warmer ground strata towards the cooler river. Here the river actually extracts from the ground the nutrients which have themselves been raised to the upper strata due to the processes mentioned earlier and illustrated in fig. 9.5 above. This results in an increasing leaching of the minerals, trace-elements and nutrients from the surrounding soil, leading to a nutrient deficit and eventual infertility. For the same reasons no groundwater recharge results. A corollary of this phenomenon is that the longer a river flows through irrigated, sun- lit farmlands, the more it becomes contami- nated with salts, artificial fertilisers, pesticides etc. making it increasingly unusable as a source of water in the lower reaches. In fig. 9.8 both negative and positive tem- perature gradients are active simultaneously. Here the variation in river water temperature, again for the purposes of discussion, is from +17°C at the water surface to +13°C at the bot- tom. The ground under the forested area on one side of the river has lower temperatures than the river water, whereas the cleared, tree- less land on the opposite side gives rise to higher ground temperatures. In this instance the river acts to convey nutrients from the warmer left bank to the cooler right bank fol- lowing the dictates of the prevailing tempera- ture gradient which, from examination of the various ground temperatures, on the left hand side is negative and the right hand side posi- tive. The cooling effect of the forest also affects the shape of the channel profile and is mir- rored in the greater depth of water on that side, since cooler water flows faster and in a more laminar fashion, removing sediment and thereby deepening the bed at that point. Notes 1. British scientific journal Nature, 30th June 1988. 2. The Memory of Water — Homeopathy and the Battle of Ideas in the New Science by Michel Schiff, Thorsons, an imprint of Harper Collins, 1995, ISBN 0-7225- 3262-8. 3. Information from Brauer Biotherapies, 1 Para Road, P.O.Box 234, Tanunda 5352, So. Australia. 4. Nexus New Times magazine, V ol.2, No.17, Dec.1993-Jan.1994, quoting from New Scientist 23rd October 1993. 5. Christopher Bird has kindly supplied information from Mme Annie Asada, director for develop- ment at 'Science Innovative', and from Jack Dupre, a close associate of Dr. Marie Nonclerce pharmacist and author of a book on Antoine Bechamp; (Louis Pasteur, Bechamp's contempo- rary, was responsible for suppressing his signif- cant findings). 'Science Innovative' was set up by Mme. Evelyne Besso who is also its President S.I.'s headquarters are presently situated at 30 Ave. D'Elyau, Paris 75116 (tel: 01.4656.6650). Its aim is to foster enquiry and interest into the essential nature of water, and to support Jacques Benveniste's continuing research.

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