The Fayûm and Lake MœrisBrown, R. H. (Robert Hanbury)
History
The Fayûm and Lake Mœris
Brown, R. H. (Robert Hanbury)
Fayyum (Egypt) -- Description and travel; Moeris, Lake (Egypt)
Colonel Western, in a note on the Wadi Raiân, shows that for a
certain number of years out of sixteen years (1872 to 1887, of which
he had the statistics to work with) there is a surplus discharge in
the Nile which might be abstracted without in any way interfering with
the ordinary irrigation of the Delta. In his calculations he takes 565
million cubic metres in twenty-four hours as the discharge required
by the Delta during September and the first half of October. He is,
of course, referring to the conditions of the Delta at the present
time. He gives the table which appears on the preceding page, to
which I have added the corresponding gauge levels at Beni Suef and
Magnûnah mouth for reference further on.
The month of August has not been given, as the conclusion was come to
that there was no water to spare in August under present conditions.
The calculation, giving these figures, is made assuming that
regulation on the Barrage below Cairo is not called in to assist;
the discharges allowed to Lower Egypt, after abstracting the above
quantities, being sufficient to give a water surface at the level
required for irrigation without any heading-up. Now, the quantity
required to fill the lake to R.L. 25·00, as found before, is 11,800
million cubic metres. This, let us suppose, would be made up thus:—
September 30 days at 112 millions = 3,360 millions.
October 31 „ 192 „ = 5,952 „
Parts of August
and November 29 „ 86 „ = 2,494 „
------
Total 11,806 „
These discharges could be abstracted without affecting Lower Egypt
irrigation, as it exists now, for eleven years out of sixteen. This,
however, is not a quite correct statement as applied to each of
the eleven years, since the discharges given in the table are
the _averages_ of those years in which a surplus discharge is
available. Among these would be some very high years, in which it
would be possible to fill the lake to a higher level than 25·00,
and years when this level would not be reached.
Besides the years, for which the averages of surplus discharges
are taken, there would be five years out of sixteen when the supply
would fall short in September, the month of highest level.
There is no necessity in this stage to seek for a connection between
the lake and the Nile for filling the lake, as the water would find
its way in large volumes across all the low parts of the valley
into the drainage depression along the edge of the Libyan Desert,
now known as the Bahr Yûsuf.
Public-domain text, read in full here on John Shaqi.
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