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components of groundwater also become less aggressive. The higher-grade the carbone s , the less complex the oxygen groups need to be in order to com- plete the interaction, and vice versa. The relative position of the boundary layer of +4°C also varies, due to fluctuations in ground temperatures caused by the rising and setting of the Sun and the alternation of the seasons. Generally speaking, this layer lies higher by day and deeper by night. When assessing the causes of fluctuations in the groundwater table, the introduc- tion of the already well-known concept of the saturation deficit is necessary, with which the relation between temperature and water-vapour content of the atmosphere is determined. The climatic conditions of Central Europe are of moderate continental character and are distinguished by maximum rainfall in the summer months. However, this is associated with a corresponding increase in evapo- ration due to higher temperature - thus the saturation deficit will be greater. The annual rainfall distribution in Central Europe amounts to 9%-13% in the summer months and 4%-6% in the winter months. According to Mayer's findings (Meteorologische Zeitung, 1887), these values for rainfall distribution are to be compared with summer and winter saturation deficits of 3mm- 7mm and 0.3mm-1.0mm respectively. With equal levels of relative humidity, and with rises in temperature from -10°C to +30°C, the water content of the atmosphere can rise more than fif- teen-fold. Only when data concerning the amounts of rainfall and the satu- ration deficit have been studied will it be possible to arrive at laws governing the fluctuations in the height of the groundwater table. Generally speaking, however, since at present these two meteorological components can neither be added together directly, nor cancel each other out, fluctua- tions in the groundwater table must therefore be dependent primarily on their reciprocal interaction. The possibilities for practically applying the here-decisive conformities with natural law encompass the effortless and almost costless raising of the deep-lying groundwater table in deserts. Apart from the mechanical interplay of forces co-active in the raising and sinking of the groundwater table, another factor to be taken into account is the physical interaction - the absorption of portions of carbone elements and the binding of gaseous carbones, which are diffused (dispersed) through the water at a suitable temperature if isolated from light and external air. The highest dispersion of carbone groups is always present in the immediate proximity of a concentration of oxygen that occurs under these circum- stances - which means that the water can complete its reconstitution and become internally mature. The water lying above the boundary layer now further charges itself with carbones present in the vegetation zone of the Earth, using up more and more of its oxygen in the process. When a certain degree of saturation isPDF Image | The Water Wizard
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