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Salinity Intrusion and Seasonal Water Quality Variations in the Tidal ...

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The status report presented above depicts that <strong>the</strong> water availability is less than<br />

90L per head per day, a value much less than that ofa developed country. It may be noted<br />

that per capita dem<strong>and</strong> depends on season <strong>and</strong> way of life. A realistic estimate is 360L<br />

percapita per day. Accord<strong>in</strong>g to Prof. Mal<strong>in</strong> Falkenmark 100Uday (36.5 cubic meters per<br />

year) is <strong>the</strong> m<strong>in</strong>imum per capita water requirement to meet one's basic domestic needs.<br />

(Falkenmark <strong>and</strong> Widestr<strong>and</strong>, 1992). In India, of<strong>the</strong> urban population 84.9% had access<br />

to clean dr<strong>in</strong>k<strong>in</strong>g water <strong>in</strong> 1993 as compared to 69% <strong>in</strong> 1985, but rural population figure<br />

fell from 82 % <strong>in</strong> 1985 to 78.45 % <strong>in</strong> 1993 (State of India's Environment, Report<br />

No.1995EE52, 1996). When Coch<strong>in</strong> catches up with <strong>the</strong> Western <strong>in</strong>dustrialized<br />

democracies it will require ten times more water even if <strong>the</strong> population rema<strong>in</strong>s<br />

unchanged (Figure 1.9). This fact itself is reason enough to turn to <strong>the</strong> natural water<br />

bodies of<strong>the</strong> city. The Coch<strong>in</strong> back waters are fresh enough for at least some part of<strong>the</strong><br />

year <strong>and</strong> <strong>the</strong> study zeros upon <strong>the</strong>se water bodies. Many of<strong>the</strong> major rivers of<strong>the</strong> world<br />

f<strong>in</strong>ally reach <strong>the</strong> ocean through deltas, which have some of <strong>the</strong> characteristics of an<br />

estuary. In many <strong>in</strong>stances <strong>the</strong> flow <strong>in</strong> <strong>the</strong>se rivers is so great that <strong>the</strong> dilution of <strong>the</strong><br />

ocean can be measured for miles out <strong>in</strong>to <strong>the</strong> sea. Some plants have used <strong>the</strong> brackish<br />

waters of <strong>the</strong> tidal bas<strong>in</strong>s as cool<strong>in</strong>g tower make up, s<strong>in</strong>ce <strong>the</strong> water is low enough <strong>in</strong><br />

dissolved solids to be concentrated by evaporation without severe scal<strong>in</strong>g problems just as<br />

fresh waters. One example is a chemical plant on <strong>the</strong> isl<strong>and</strong> ofTr<strong>in</strong>idad which uses water<br />

from <strong>the</strong>bay side of<strong>the</strong> isl<strong>and</strong> as cool<strong>in</strong>g tower make up (NALCO, 1979)<br />

1.3 Estuary<strong>and</strong> <strong>the</strong> urban situation<br />

An estuary is a semi enclosed coastal body of water which has a free connection<br />

with <strong>the</strong> open sea <strong>and</strong> with<strong>in</strong> which <strong>the</strong> sea water is measurably diluted with fresh water<br />

10

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