Water Supply: the Present Practice of Sinking and Boring Wells: With Geological Considerations and Examples of Wells ExecutedSpon, Ernest
Science
Water Supply: the Present Practice of Sinking and Boring Wells: With Geological Considerations and Examples of Wells Executed
Spon, Ernest
Boring; Water-supply; Wells
The boring operations are carried on uninterruptedly during the process
of tubing, excepting only for a few minutes when fresh tubes are being
added. It will be seen that the cast-iron well is in this case the
ultimate abutment against which the pressure is exerted in forcing the
tubes down, instead of the weight of the boring machine with stones and
pig iron added, as in the case where the screw-jacks are used; the
hydraulic method was designed specially for the work at Gosport, and has
acted most perfectly. Both the cast-iron well and the bore-hole are
entirely shut off from all percolation of sea-water, by first filling up
the well 30 feet with clay round the tubes, and making the tubes
themselves water-tight at the joints at the time of putting them
together.
In the event of any accident occurring to the tubes while they are being
forced down the bore-hole, such as requires them to be drawn up again
out of the hole, the prong grapnel, Fig. 204, is employed for the
purpose, having three expanding hooked prongs, which slide down readily
inside the tube, and spring open on reaching the bottom; the hooks then
project underneath the edge of the tube, which is thus raised on hauling
up the grapnel. In case the tubes get disjointed and become crooked
during the process of tubing, the long straightening plug, Fig. 205,
consisting of a stout piece of timber faced with wrought-iron strips, is
lowered down inside them; above this is a heavy cast-iron block, the
weight of which forces the plug past the part where the tubes have got
displaced, and thereby straightens them again.
Although there are few localities where the geological formation is not
favourable to the yield of pure water if a boring be carried deep
enough, yet it rarely happens that free-flowing wells such as those in
Paris and Hull are the result. Generally after the water-bearing strata
have been pierced, the level to which the water will rise is at some
depth below the surface of the ground; and only by the aid of pumps can
the desired supply be brought to the surface. Various pumping
arrangements have therefore been adopted to suit the different
conditions that are met with.
It is not the object of the present work to treat of the forms and
fittings of pumps, and the following details are only given as
completing Mather and Platt's system.
Public-domain text, read in full here on John Shaqi.
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