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(1973) n°3 - Royal Academy for Overseas Sciences

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— 594 —<br />

Fig. 6. — The Swakop and Khan Rivers watershed.<br />

cases. The fresh water thus seeping in the sand <strong>for</strong>ms a fresh<br />

water lens over saline water, and is a major source of water.<br />

These water lenses all constitute a major local source of water<br />

in many desert and generally underdeveloped areas. Their contamination<br />

by intruding salt water constitutes a pollution problem<br />

of major economic and social importance.<br />

4b. Exploitation of fresh water lenses floating over saline water.<br />

It appears that all the theoretical problems outlined in sections<br />

2 and 3 are present in this problem. First of all, a chemical<br />

stratification is present. Absorptive and exchange reactions<br />

between the moving fluid and the porous medium will be<br />

greatly favoured by the large surface areas of the medium.<br />

It should be pointed out that the equilibrium time of these<br />

reactions is usually very much smaller than the characteristic<br />

time scales of the flow. Thus, in computing the flow of the<br />

moving fluid, the chemical reactions are usually assumed to<br />

occur instantaneously (25, 23).<br />

In the exploitation of fresh water floating lenses, it is not<br />

possible to use the classical methods of fighting salt-water<br />

intrusion. One of these classical methods is used in the case<br />

of fresh water coastal aquifers in the United States, where

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