Disclaimer note - WWF - Pakistan
Disclaimer note - WWF - Pakistan
Disclaimer note - WWF - Pakistan
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Detailed Ecological Assessment Report 2008 – Keenjhar Lake<br />
1. Fish ladders in the middle as in G.M. Barrage are not suitable for fish to<br />
enter as fish avoid main currents where velocity exceeds 50 cubic<br />
feet/second.<br />
2. Present Fish ways are constructed as 10 feet wide in the lower section,<br />
which reduces to 5 feet in the upper section. Such structure is narrow for<br />
fish to enter.<br />
3. The Fish ways of G.M. Barrage change shape or direction which causes<br />
hurdles to fish to ascend.<br />
4. Overflow weirs of the fish ways are not needed<br />
Image 12 – A view of G.M. Barrage.<br />
Talbot 1959 suggested following alterations in the existing fish ways of G.M.<br />
Barrage.<br />
1. The fish ways of G.M. Barrage should be replaced by modern fish ways<br />
2. The best location of the fish ways is at the banks of river immediately<br />
below barrage.<br />
3. The velocity of water should be controlled at the raceways to 5 cubic<br />
feet/second.<br />
It is presumed that if these suggestions would have been carried out or<br />
experiments to see the effect of some changes in the fish ways were observed<br />
the Hilsa fisheries could be saved or at least its migration would have e possible<br />
beyond the G.M.Barrage.<br />
3.5.9.7 Conclusions<br />
Keti Bunder the delta of Indus River is known to be second largest delta in the<br />
World. It has historic background and source for the high production of the<br />
Arabian Sea due to discharge of sediments brought by river currents from Tibet,<br />
the ultimate origin of Indus. In the historical days the delta was a hub of fishing,<br />
navigation and other activities for major countries along the Arabian Gulf. With<br />
the establishment and modernization of <strong>Pakistan</strong> several dams appeared that<br />
considerably reduced the size of delta because of the low water and<br />
simultaneously low sediment discharge in the sea. As reported by NIO scientists<br />
zero discharged is observed during the most part of the year while from June –<br />
September fresh water reached deltaic region quite infrequently. The river thus<br />
contributing hardly into the delta and almost no sediments are brought to the sea<br />
and sea water ascends the vast area. The impact of such conditions (no<br />
freshwater and intrusion of sea) are understandable by the loss of ecological<br />
<strong>WWF</strong> <strong>Pakistan</strong> – Indus for All Programme Page 93 of 188