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tion of otherwise dangerous levels of ultra- violet radiation, a process which is vital for all life on Earth. The result is a net loss of water. The greater the amount of water vapour propelled into the atmosphere through the overheating resulting from excessive defor- estation, the greater the consequent losses; losses indeed that can never be recovered (see pp. 121 & 123). What differentiates water from all other liquids, a factor that will be discussed in more detail later, is its so-called 'anomaly point' or 'point of anomalous expansion'; that is to say, water's volume does not decrease continually with increasing cold. Its behaviour is anomalous, and hence the term 'anomalous expansion' or 'anomaly point'. This point of reversal is reached when the water attains its greatest density and energy content at a temperature of +4°C, below which it eventually crystallises as ice at 0°C, a process greatly assisted if so-called 'impuri- ties' are present which provide the nucleus around which the ice forms. Another important factor is water's dielec- tric value. The base dielectric value for calcu- lating all other values is based on the permittivity of a vacuum and has a value of 1. Permittivity is the extent to which a sub- stance can be penetrated or traversed by an electric current or charge. Apart from a vacuum, a dielectric can be formed of an electrically neutral, interstitial membrane separating positive and negative electric charges, i.e. a non-conducting substance such as paraffin wax. The dielectric value of pure water (distilled water) is 81 (=92) and is therefore 81 times more effective as a charge separator than a vacuum and almost the highest dielectric value there is 1 mm3 of the purest water at room temperature, for example, has an elec- trical resistance equal to a lmm2 copper wire, 15,000,000km long. It thus possesses a tremendous innate resistance to the transfer of charge. Pure water will only freeze at tem- peratures of around -40°C or in clouds at about -10°C, which again is fairly important, as we shall discover later. In comparison with a temperature of -273.15°C (= absolute zero or 0oKelvin), supposedly the lowest possible 6: The Earth's Atmospheric Envelope 89 temperature to be found anywhere in the Universe, the temperature of 0°C, or freezing point, is relatively warm. Lying between approximately +40°C and -10°C, the temperature range in which we live is not very large. In fact it is a fairly nar- row band-width between extremes to which we are not normally subjected. Our radius of action, our living space, as it were, lies within the upper and lower boundaries of the troposphere, itself a stratum or 'sphere' within the overall atmospheric envelope and defined by temperature and water vapour content. To glean more facts about the structure of the atmosphere, from the Phaidon Concise Encylopedia of Science and Technology3 we are provided with the classifications shown in fig. 6.1, which should be viewed in conjunc- tion with fig. 6.2. My own questions and com- ments are printed in bold type. 6.2 The Terrestrial Bio-Condenser eeping in mind water's dielectric value K of 81 and its enormous resistance to the transfer of charges, let us now examine the thermal structure of the atmosphere (fig. 6.2), for this may explain to us another way in which, apart from the accumulation of heat, the Earth could become charged with life energy. The portion of the atmosphere most impor- tant to us and which affects us most is the troposphere, which from fig. 6.2 can be seen to terminate at the tropopause between 6km and 18km up. Curiously enough, we also find that the temperature neither decreases nor increases constantly (shown as wavy broken line), but fluctuates as we ascend through the various atmospheric layers, so that at a certain altitude, at 29km for instance, the temperature is -60°C, whereas at a height of 80km it is +10°C. Somewhere between these two temperatures, therefore, there is a layer where the temperature is +4°C. According to my calculations there are at least four such levels where the temperature equals +4°C, at altitudes of about 3.5km, 77km, 85km and 175km.PDF Image | Viktor Schauberger Work Explained
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