Geology -- Egypt; Nile River; Water-supply -- Egypt
The dam has worked for two years and given satisfaction. When the Nile
was at its lowest in May 1903, the natural discharge of the river,
supplemented by all the subsoil infiltration water which enters the
river between Assouân and the sea, was 400 cubic metres per second. The
reservoir was adding 200 cubic metres per second to the supply, raising
the total supply available for irrigation to 600 cubic metres per
second. The reservoir was supplying one-third of the water which was
being utilized in Egypt. This water will suffice for an increase to the
perennially irrigated area of ¹⁄₂ million acres.
At the time of designing the dam it was intended that it should be of
such a section that it could be raised 6 metres in height and hold up
another milliard of cubic metres of water. Such an operation, if
performed to-day, would mean: the whole length of dam being raised 6
metres, the winches working the sluice gates being raised 6 metres and
provided with new wire ropes; and new copings being given to the
parapets. It would necessitate two more locks and three more lock gates,
and nothing else. The expenditure incurred would be about £500,000.
33. =The Wady Rayan Reservoir Project.=--When the Assouân dam will have
been raised, we shall be standing on the threshold of what it will be
able to do. The projected Wady Rayan reservoir, or the modern Lake
Mœris, will be well able to supply the two remaining milliards of cubic
metres of water when working in conjunction with the Assuân Reservoir.
The great weakness of this projected lake has lain in the fact that _by
itself_ it could give a plentiful discharge in April and May, less in
June, and very little in July, and it was for this reason that in my
report of 1894 to the Egyptian Government I had reluctantly to recommend
that it be not carried out. But when the Assouân reservoir is capable of
supplying two milliards of cubic metres of water it will be possible to
utilise the Mœris Lake to its utmost capacity. The Assouan Reservoir,
being high above the level of the Nile can give its supply at the
beginning or end of the summer; it can give it slowly or with a rush;
while the projected Lake Mœris, being directly in communication with the
Nile, and only slightly above low Nile level, its discharge would depend
entirely on the difference of level between it and the Nile, and
consequently as the summer advanced its level would gradually fall and
the lake would not be able to give at the end of the summer a quarter of
the discharge it could give at the beginning.
[Illustration: PLATE XV
PROPOSED WADI RAYAN RESERVOIR
SHOWING THE FAYOUM
_All R. L.^{s} in metres, above or below mean sea._
+ -
_Desert._
_Scale 1 : 500,000_
Lith. Sur. Dep. Cairo.]
Public-domain text, read in full here on John Shaqi.
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