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The +4oC centre-stratum, which is incompress- ible at this temperature, is therefore increas- ingly squeezed between these two opposing pressures, namely the overburden of infil- trating water from above and the expand- ing, sometimes super-heated water from below. Its only possible avenue of escape is either laterally or vertically, or a combination of both On many mountains in Austria, for exam- ple, there are springs which emerge at between 100 and 200 metres below the summit. These mountain peaks are commonly composed of solid rock and, were such springs to be attrib- uted seepage only, there is not sufficient catchment area to provide for their continuous, year-round discharge. The temperature of these springs always lies between +4°C and +5°C very cold water indeed. From this it can be inferred with some certainty that true springwater arises and moves within the cen- tral core of the groundwater body. As the springwater rises, while rich in car- bones, particularly in the form of carbonic acid, it is very largely deficient in dissolved oxygen, for during the course of the water's initial sink- ing, various organisms and tree roots have removed whatever dissolved oxygen was available in the infiltrating rainwater. By and large such water is therefore oxygen-deficient and, this deficiency is extreme and the water is drunk directly at the place where it gushes out of the ground, its emanation of carbon- dioxide vapours are breathed in at the same time. Mountain folk in Austria call these vapours the 'waterworm'; they are also known as choke-damp and are on occasion to be f o u nd in mines, the effect of which is to do pre- cisely what its name suggests, and if no air containing oxygen is soon available then death follows. Since the water from these so-called 'poisoned springs' has no oxygen, it actively extracts this from the tissues in the area of the trachea, esophagus and stomach, while the undiluted carbon-dioxide vapour immedi- ately begins to attack the lungs for the same reason. This affliction was also known as the 'van- ishing lung disease,' or in plain English, 'galloping consumption'. Those who are unfor- tunate enough to drink much of this water are 10: The Formation of Springs 131 likely to die within a few days to the accompa- niment of excruciating stabbing pains in the chest. However, once the water has emerged and has flowed even ten metres, due to its con- voluting, splashing, flowing motion it has already made up for the lack of oxygen through its absorption from the atmosphere and the proper carbone-oxygen balance has again been restored. The absorption of oxygen, however, has the effect of increasing the volume of the water. At a spring in Montenegro, which flowed down a smooth, unfissured face of rock, Viktor Schau- berger made careful measurements of the volume of flow directly at the mouth and metre by metre below it. He discovered that it increased significantly. There being no possibil- ity of any additional inflows due to the unbro- ken formation of the rock, the only possible answer was that this resulted from the absorp- tion of oxygen. 10.2 The Rising of Springwater I 24-hour experiment designed to show the n Our Senseless Toil Viktor briefly describes a dynamics of true springs, the diurnal fluctua- tion in the height of the groundwater table and the flow of sap in trees. As we said earlier, there is no condition of equilibrium in Nature. The experimental arrangement shown in fig. 10.3, consists of a U-shaped tube with open connections on one arm to two capillary tubes and on the other to four capillary tubes. A cer- tain quantity of pure quartz sand sufficient to close the internal diameter is placed in the bot- tom of the U-tube and saturated with salt water. The effect of this saltwater and sand is to separate and prevent direct communication between the contents of the two rising arms of the U-tube. These are then filled with fresh, high-grade springwater, containing little or no oxygen, which has not been exposed to the Sun, or other light or any atmospheric influ- ence. The U-tube is then placed in an insulated vessel, such as a bucket, containing some ice at the bottom, and the whole filled with good, clean loam. The ice at the bottom is necessary to create an artificial zone of +4°C at the base of the U-tube and a positive temperaturePDF Image | Viktor Schauberger Work Explained
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