Engineering Wonders of the World
Volume I
År: 1945
Serie: Engineering Wonders of the World
Sider: 448
UDK: 600 Eng -gl.
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388
ENGINEERING WONDERS OF THE WORLD.
which there are many in Egypt), it would run
dry as soon as the river had fallen below the
canal bed at E, and no more
Perennial crOpS COuld be raised on these
Irrigation. .r
Rai lands unless other means
of irrigation were provided. If, however, the
canal bed, C, be cut deeper than the lowest
summer level of the river at E, another method
of irrigation, the perennial, is possible. Let
us assume the canal to be constructed for per-
ennial irrigation. Since the gradient of the
canal bed is much more gradual than that of
the Nile Valley—1 in 20,000 as against 1 in
12,000—if we follow the course of the canal
from its inflow at E (where the land is higher
than the water level of the canal) in a direc-
tion parallel to the river, there will come a
point, say at V, where the water level of the
canal and the land level will be the same.
From that point onward the farther we pro-
ceed the lower will be the level of the land
relatively to the water level in the canal.
Eventually the point M will be attained,
whereat th© water level of the canal
will command even the land, marked
lying above the flood level of the Nile,
follows that below the point V, at X,
M, etc., wheresoever it may be required for
irrigation, the water will flow on to the
land by gravitation. In summer, the basins,
1, 2, 3, 4, 5, 6, 7—some of these, it may be
said, have an area of 40,000 acres—which had
been flooded and drained off in the winter, are
divided up by distributing canals and low
banks into diminutive basins, and are flooded
to a depth of two or three inches according to
the requirements of the crops.
It should be remembered, in connection with
the perennial system of irrigation, that, where
gravitation is relied on solely, the area of cul-
tivable land each year is determined by the
general level of the Nile in summer. The
lower the Nile at E the farther away from the
inflow will be the point V, where the water
level of the canal C and the land level are
c
A,
It
Y,
the same. It should also be noted that when
the average level of the low Nile falls below
the normal, the volume of water in the canal
is decreased, and the area of land capable of
being reached is diminished.
We have seen that in ordinary circum-
stances the water level of the canal C is the
same at point V as the level of the adjacent
fields. If, however, a barrage were built
across the river, down-stream of the intake
E, so that during high Nile the flood water
would be allowed to pass freely, and during
the summer the river could be dammed back,
the point at which the level of the canal water
and the level of the adjacent fields were the
same would then be brought proportionately
nearer the intake—say, to the point K. The
effect of this would be to increase the volume
of water in the canal C, to enlarge greatly
the area of irrigable land, and to reduce the
effects of a “ bad ” Nile. Such, in fact, is
the purpose served by the Assiout Barrage.
Comparing our illustration (Fig. 3) with this
important work and the great canal it serves,
W may be said to represent the Assiout Bar-
rage, and canal C the Ibrahimiyeh Canal.
In the foregoing description of perennial
irrigation we have assumed that both means
—flooded basins for winter crops, and gravita-
tion irrigation (Sefi water) for summer crops—
were used. The crops so cultivated are wheat,
beans, barley, maize, durra, etc. But cotton
cannot be cultivated under the same condi-
tions, for the seed of this most important
crop is sown in March, and the
. . Cotton,
harvest is not ripe for picking
until September, at the middle of what is
known as the flood season. So the land used
for cotton cannot be irrigated on the basin
system. During the flood season it is watered
in a manner similar to that employed through-
out the summer, by a system of miniature
waterways running off the main canal.
Where, as often happens, the canal or river
is not sufficiently high to allow water to pass by