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Temperature - European Investment Bank

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WEST AFRICAN POWER POOL (WAPP) PÖYRY ENERGY LTD.<br />

Mount Coffee HPP ESIA and RAP 2012-09-18<br />

ESIA Report Page 44<br />

o Application of a value which would be reached according to Swiss<br />

legislation. Here, residual flow is based on Q347, and determined by means<br />

of a stepwise increase, leaving a higher proportion of water in smaller<br />

rivers. This rule was formulated mainly for highly seasonal rivers in alpine<br />

conditions. Applied to St. Paul river (which is not an alpine, but definitely<br />

a highly seasonal river), this would result in a residual flow of 4.3 m³/s.<br />

However, this law also specifies that this is a minimum value, which might<br />

have to be increased depending on specific site characteristics.<br />

o Using the 7Q10 value; this value represents the lowest 7-day average<br />

flow that occurs once every 10 years. This would result in a residual flow<br />

of 8 m³/s. This corresponds approximately to the lowest flow values<br />

recorded in St. Paul river.<br />

� Determination of a value based on site-specific considerations.<br />

8.2.3.3 Evaluation of Options<br />

The affected stretch of the river, between dam and tailrace channel, is rather short, and<br />

given the fact that the slope is very gentle and some riverbed pools even her might<br />

actually be below seas level, it will not dry out completely. Still, it is certainly a habitat<br />

for fish, and a minimum flow, i.e. a minimum amount of actually flowing water, as<br />

opposed to stagnant water in some pools, must be maintained. It has also to be<br />

considered that the river in this part is divided into several branches. If the residual flow<br />

is too small, it would not have the desired effect. On the other hand, the water left<br />

flowing from the spillway means a loss in energy production, a fact which also has to be<br />

taken into consideration. The following Figure illustrates the effect of different amounts<br />

of residual flows on water availability for electricity generation (only situation during<br />

low flow conditions).<br />

m³/s<br />

160<br />

140<br />

120<br />

100<br />

80<br />

60<br />

40<br />

20<br />

St. Paul river water availability for different residual flows<br />

0<br />

70.00 75.00 80.00 85.00 90.00 95.00 100.00<br />

-20<br />

% exceedance<br />

Figure 8-7: Water availability with different amounts of residual flow<br />

total flow<br />

1 unit 100%<br />

1 unit 40%<br />

residual flow 1<br />

available flow 1<br />

residual flow 2<br />

available flow 2<br />

residual flow 3<br />

available flow 3

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