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<strong>Model</strong> <strong>of</strong> <strong>the</strong> D;spers;on<strong>of</strong><strong>Fresh</strong> <strong>Water</strong>.<br />

29<br />

Results <strong>and</strong> Discussion<br />

The results <strong>of</strong> <strong>the</strong> studied elements in <strong>the</strong> surface water <strong>of</strong> Jeddah coast are pre.<br />

sented in <strong>the</strong> form <strong>of</strong> distributions shown in Fig. 2, 5-8.<br />

SALINITY (.,..)<br />

N-..<br />

39 ..., .> 39 .<br />

"<br />

SALINITYC",,)<br />

A--<br />

~\\" ~<br />

J) '. .<br />

..\ \;-1<br />

A--<br />

'""-<br />

." N<br />

" OV ..~) 1981<br />

APRIL 1982<br />

/\..-'"<br />

> 39<br />

h;, --:.<br />

"'~'~~-J<br />

.."/,<br />

.~DEC. 1981<br />

v<br />

/<br />

~~ MAY 1982<br />

vv<br />

FIG. 2. Distribution <strong>of</strong> salinity in <strong>the</strong> surface water <strong>of</strong> <strong>the</strong> Red Sea coast in front <strong>of</strong> Jeddah.<br />

Figure 2 shows <strong>the</strong> surface distribution <strong>of</strong> salinity. Figure 3 shows <strong>the</strong> vertical distribution<br />

<strong>of</strong> salinity along <strong>the</strong> section extended fro~ Bankalah seaward. From <strong>the</strong>se<br />

figures, it is easy to define <strong>the</strong> place <strong>of</strong> <strong>the</strong> discharge <strong>of</strong> <strong>the</strong> fresh water (that accompanied<br />

<strong>the</strong> effluent <strong>of</strong> <strong>the</strong> domestic sewage), which is at Bankalaharea at <strong>the</strong> sou<strong>the</strong>astern<br />

side <strong>of</strong> <strong>the</strong> studied area, where salinity values less than 39.0, minimum 8.4,<br />

were found. The minimum salinity was always found at station 1 near to Bankalah.<br />

Whereas <strong>the</strong> rest <strong>of</strong> Jeddah coast were characterized by salinity values greater than<br />

39.0, maximum 39.6. From Fig. 2, it can be seen that <strong>the</strong> isohalines <strong>of</strong> values < 39.0<br />

were close to one ano<strong>the</strong>r near <strong>the</strong> entrance <strong>of</strong> Bankalah zone indicating that <strong>the</strong> rate<br />

<strong>of</strong> mixing during <strong>the</strong> inflowing <strong>of</strong> <strong>the</strong> discharged waste water with <strong>the</strong> Red Sea water<br />

was greater <strong>the</strong>re. But <strong>the</strong> isohalines were changing <strong>the</strong>ir positions back <strong>and</strong> forth (or<br />

in <strong>and</strong> out) <strong>of</strong> Bankalah zone from one cruise to ano<strong>the</strong>r. For example, <strong>the</strong>y were out<br />

during <strong>the</strong> November 1981 <strong>and</strong> January 1982 (<strong>and</strong> May 1982) cruises <strong>and</strong> were in,<br />

during <strong>the</strong> cruises <strong>of</strong> October <strong>and</strong> December 1981 (<strong>and</strong> April 1982).<br />

--- ~

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