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The water now begins to extract fresh carbones from its bed and banks, which cool it. Since the carbones now lie at the bottom and the oxygen is evenly diffused in the water above, explosions will now occur in a direction opposite to the one previously described, which act in a 'shovelling' way. The water excavates. The excavating phase is then followed by a depositing phase. The carbones present in the deeper part of the channel profile become dispersed as they rise towards the surface and the oxygen sinks towards the bottom, reintroducing the depositional phase. In this closed cycle of alternating deposition and removal, the quality of the water contin- ually deteriorates and it becomes 'sluggish and stale, lifeless and insipid'. This latter phenomenon has two main causes: (1) increase in water temperature and the associated decrease in specific weight, and (2) the fact that the water available at the beginning of each phase is always of poorer quality, because substances least ennobled by the explo- sions are driven downstream where they become the starting product for new explosions. As long as healthy conditions in the water prevail - as long as the proper proportions between the inner water-masses, the bed-gradient and the tem- perature continue to exist - the incidence of turbulent phenomena will be stronger along the upper margins of the banks while constantly weakening towards the bottom, and the axis of the current will remain unchanged. The constantly-increasing strength of the external influence resulting from the widening of the channel reduces the water's tractive force. Towards evening the temperature gradient once more approaches a positive energy-form and during the night sediment will be transported further. At a suitable temper- ature the watercourse regulates itself automatically in every respect. With its temperature properly adjusted, the watercourse will not only widen itself in the proper proportion, but will also deepen itself appropriately in the lower reaches. Thus the longitudinal profile suited to the varying cross-section is formed automatically - a necessary matter for the removal of the sediment load, which under orderly forest conditions is in any case minimal. Where undisturbed by human hand, when flooding does occur in such waterways, the influence exerted from the outside on the increasing water-masses is stronger, due to the external temperature which as a rule is low at such times. The temperature gradient becomes positive and the now cooler water-masses drain at a greater velocity without attacking the banks. With the correct reversal of temperature, the influence of temperature gra- dient is greater than that of bed-gradient, because the mass-transport of sed- iment will be appropriately regulated in proportion to the corresponding increase in flow-velocity. In this case, with an increase in the volume of water, the speed of forward motion will also be greater due to the properPDF Image | The Water Wizard
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