An Egyptian oasis : $b An account of the oasis of Kharga in the Libyan desert, with special reference to its history, physical geography, and water-supplyBeadnell, H. J. L. (Hugh John Llewellyn)
History
An Egyptian oasis : $b An account of the oasis of Kharga in the Libyan desert, with special reference to its history, physical geography, and water-supply
A very great drawback to the water of these upper sandstones is
its variable quality. In the Headquarters district it is usually
more or less ferruginous, and in some pits may contain as much as
63 grains of dissolved solids per gallon, the salts consisting of
iron, potash, and soda, with traces of lime and magnesia, mostly
in the form of sulphates and chlorides. Mr. William Garsed[9] has
calculated that this water would, if used for irrigation at the
rate of 3 gallons a minute per acre, effect an annual deposition
of over 3 tons of sulphate of potash and common salt on each acre
of land. Salts of this nature in such quantities would, of course,
have a very deleterious effect on the crops, not to mention the
mechanical binding action of the iron on the soil.
It appears that the want of uniformity in the quality of the water is
due to local causes, chief of which may be the relative abundance of
fissures, the purity of the sandstone, and the presence or absence
of mineralized shales. In those areas where the water is moving
only slowly—where, in fact, it tends towards stagnation in the
strata—it is probably liable to become more or less highly charged
with mineral salts; certainly the best qualities seem to coincide
with relative abundance, and the largest supplies are undoubtedly
found where the beds are traversed by fissures.
In many parts of the oasis perfectly sweet water is obtainable from
the sandstones of this series, and this source, as an auxiliary to
the artesian supplies obtained from deep borings, was taken full
advantage of in olden times. The ancients constructed the most
marvellous systems of subterranean aqueducts to tap these sources,
more especially in the neighbourhood of Um el Dabâdib, Qasr Lebekha,
and Qasr Gyb, where such works were especially applicable, owing to
the fact that the sandstones in those districts form extensive hills
above the general level of the surrounding cultivable ground. These
underground works are, in many respects, of far greater interest than
the ancient monuments, and they will therefore be fully described
in a later chapter.
THE ARTESIAN-WATER SANDSTONE.
Public-domain text, read in full here on John Shaqi.
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