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cycle. The release of water from this reservoir then follows. As will be described later, the lateral expansion of the centre stratum (formation of springs) can also occur due to pressure acting on it from above and below. Fig. 14a41 below, schematically illustrates a cross-section through a groundwater reservoir. This depicts how not only the lateral but also the upward flow of the centre stratum (under the greatest pressure from all other strata) can come about. In contrast, as described previously, high surface temperatures permit hard- ly any water to infiltrate into the ground at all. The accretion of groundwater ceases, or it only accumulates in small quantities at great depths. Through evaporation of small residues of groundwater still present, the ground becomes increasingly incapable of absorption. Due to the effect of too high a ground temperature, percolating water will develop into surface run-off, lead- ing to rapid re-evaporation connected with it (a half-cycle). In this case no accretion of groundwater in the previously-described sense therefore comes about. In such districts hot springs frequently make their appearance, forced up to the surface through fissures by upward pressure from below, for which no counter-pressure exists due to the lack of over-burdening groundwater.42 The absorptive capacity of the ground is thus dependent on the condi- tions of temperature which give rise to the regulation of the groundwater table as described above, and hence on the existence and height of the groundwater-table. In summary it can be stated: a positive temperature gradient is the pre- condition for the soil's ability to absorb, for the accretion of groundwater and for the creation of the full hydrological cycles associated with it. A nega- tive temperature gradient prevents the accretion of any groundwater and gives rise to half-cycles only. 41It is known that Viktor Schauberger was unhappy with the original diagram and the translator has submitted his own interpretation in figure 14b. - Ed. 42"In the years 1911-1914 and 1918-1924, I was able to observe that on the occasion of sharply contrasting temperatures - for example, with the onset of hard frosts after a very dry autumn - and after the streams had dried up, hot water was forced upwards from great depths through craters, fissures and holes. It is characteristic of this case that grotto-olms, (a species of salaman- der) about 30cm long, will be thrown up at the same time, causing a large influx of crows to the area. A particularly striking case happened in the presence of witnesses in October 1923, in which year there was a dry autumn. The 'E'- impoundment of the Steyrling timber-flotation system was suddenly filled with hot water under an outside temperature of -12°C; within 10 minutes about 1,500m3 (1,900 cu yds) of water welled up out of the old crater at Parnstall-Futterung, filling the basin. After cool- ing off, these waters subside and, forming whirlpools, and with a great rumbling commo- tion, fall back into the Earth again. The districts are: Odsee (Parish of Grunau), locally known as the 'Roaring Lake', Lahner Alpe (Stier-Kar), Bauernschlag Alpe (above the new hunting lodge), Kasbergmulden Alpe, Luketerwald, Mangstlberg (from the forest house 'Hofjager' to Parnstall, especially in the vicinity of the so- called 'E'-impoundment. Conversely, after pro- tracted periods of rainfall and with the advent of warmer weather, cold water-masses will be driven upwards. After having cooled and with much turmoil they disappeared back into the depths within a short space of time. I would like to point out that these areas are large enclosed hunting reserves and are not generally accessible." This is an extract from a letter to Die Wasserwirtschaft, Vol. 3,1931, p.47. - Ed.PDF Image | The Water Wizard
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