(1973) n°3 - Royal Academy for Overseas Sciences
(1973) n°3 - Royal Academy for Overseas Sciences
(1973) n°3 - Royal Academy for Overseas Sciences
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tion points exist above and below the interface, (figure 10c),<br />
but each point involves a stagnation stream-line which lies inside<br />
the mixing layer. It can be shown that the amount of dissolved<br />
salt moving to the upper sink decreases rapidly as uodo is increased<br />
beyond the value of 1/2. Thus, it is quite possible to<br />
selectively withdraw in the upper sink fresh water only slightly<br />
contaminated and of great economical importance. The saline<br />
water pumped from the lower sink can of course be discharged<br />
somewhere else.<br />
January 5, <strong>1973</strong><br />
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