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
In order to arrive at some sort of idea as to the holding capacity
of the artesian-water strata of the oasis I made an examination of
between sixty and seventy samples of sand brought up from varying
depths from a few selected bores in the oasis. As, however, owing
to the methods of drilling employed, only powdered samples were
available, it was necessary in the first instance to ascertain the
relative porosity of sandstone in its ordinary state and broken up
into the form of sand. For this purpose I collected eight specimens
of the Surface-water Sandstone from various points in Northern
Kharga, and subjected them to absorption tests, both in the whole
and in the powdered states. In six out of the eight examples the
absorption was more when powdered than when whole, the average for
the eight rock samples being 22·44 per cent.; for the same when
powdered, 23·55 per cent. There is, moreover, no reason to suspect
that in ordinary lithological characters the Surface-water Sandstone
differs in any important respect from the Artesian-water Sandstone,
so that if we estimate the porosity of the latter from powdered
samples, we shall obtain a figure only about 5 per cent. too high.
The average porosity of sixty-four samples, collected from Bores
14, 16, 18, 31, 39, and 44, at various depths in the water-bearing
strata, was found to be 19·45 per cent. If we confine our attention
to a single bore, and examine a representative sample from every
stratum of the water-bearing sandstone, and, in deducing the
porosity, take into account the thickness of each individual
bed, we shall obtain a still more reliable figure. This was
done in the case of Bore No. 18, which passed through 122 metres
of water-bearing strata, thirty-one samples being collected and
subjected to examination. The absorptions obtained varied from 15·3
to 25·5 per cent., the average porosity of the whole column being
calculated as 19·6 per cent. I believe this figure may be accepted
without misgiving as a satisfactory working value for the porosity
of powdered Nubian Sandstone, that of the solid rock being taken
as 5 per cent. lower, or, say, 18·5 per cent.
Public-domain text, read in full here on John Shaqi.
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