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132 Living Energies gradient from the outer surface of the loam inwards. The whole arrangement is then placed out- side under the Sun's heating influence. Once the lowest water has reached its ice-induced anomaly point of +4°C, where it attains its highest density and weight, and the higher- lying water begins to heat up, losing its 'tem- peratureless' state, the water slowly rises up the arm to which the bundle of four capillary tubes is attached and overflows due to its greater communication with atmospheric influences; the water in the other arm remain- ing at rest. While I have not found more explicit details of this experiment in the material in my pos- session, I think this upward movement is most probably due to two factors: 1) the conversion with warming of the car- bonic acid content into carbon dioxide bub- bles, which rise, pushing individual packets of water ahead of them (see description of rising sap in chapter 18), and 2) the suctional effect of rising atmospheric gases, which become specifically lighter with exposure to the Sun's heat. At day's end this water column subsides with cooling, and overnight is in a state of rest, its contained carbones now replete with absorbed oxygen and other atmospheric gases. During the night, however, the carbone-rich water in the arm under the bundle of two capillaries becomes active. This may be due partially to its largely unsatisfied appetite for oxygen, whose supply has been limited by the fewer number of capillary tubes; also to the combined pres- sures of the night-cooled, therefore specifically heavier, atmospheric gases entering the now evacuated bundle of 4 capillaries; and to the marginally specifically heavier weight of the condensed gas-enriched, recently subsided water. Both of these exert pressure on the salt- water in the base of the U-tube, causing it to shift laterally. This in turn exerts an uplift pres- sure on the unoxygenated water in the oppo- site arm, causing the water to rise up the bundle of two capillaries. This emulates the continuous temperature-, pressure- and suction-related pulsation, which is the hallmark of all natural fluid movement - water, blood and sap. These capillary tubes are very fine, i.e. their internal diameter is minute, in this case about 0.4mm internal diameter. In terms of plant anatomy, the bundle of 4 capil- laries represents the xylem tubelets. These gen- erally have a larger cross-sectional area than the phloem tubelets, which are represented by the bundle of 2 capillaries. What is not explained in Viktor's description is whether both arms of the U-tube are posi- tioned parallel to the Sun's rays, or at right- angles, the 2-capillary bundle lying behind the 4-capillary bundle. Not explained either is whether both capillary bundles are to be pro- tected from light and heat. However, as this experiment is designed in part to demonstrate the ebb and flow of sap which occurs beneath the bark, it is desirable that the capillary tubes should be adequately shielded and insulated. If the bundle of four capillary tubes is removed, then water emerges from the top of the U-tube leg, demonstrating the formation of natural springs. On the diagram, it can be seen that the two water levels on each side of the U- tube are not in communication, but remain independent of each other, representing another phenomenon in Nature inexplicable according to current theory. This decrease in atmospheric density close to the ground during the day is also responsi- ble for the slight diurnal fluctuation in the height of the groundwater table. Being specifically lighter, the atmosphere exerts less pressure and the groundwater rises in con- sequence. The weight of the atmosphere is thus a contributing factor to the height of the groundwater table and to the rate of flow of springs, which are known to deliver more water during the night than during the day. Another experiment showing the action of true springs and one much simpler to carry out is described in Etidorpha (Aphrodite spelt back- wards), a book published by John Uri Lloyd in 1896. The book gives an account of the experi- ences of William Morgan, who was mysteri- ously abducted on the 12th of August 1826 which he related when he appeared to Llwellyn Drury some 30 years previous to the book's publication1. The book gives a number of interesting insights into many natural phe- nomena including water and its movement.PDF Image | Viktor Schauberger Work Explained
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