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 beating, or comminution of the rock, was usually effected at Passy
at the rate of from fifteen strokes to twenty strokes a minute. The rate
of descent, of course, differed in a marked manner, according to the
nature of the rock operated upon; but, generally speaking, the trepan
was worked for the space of about eight hours at a time, after which it
was withdrawn, and the shell let down in order to remove the _débris_.
The average number of men employed in the gang, besides the foreman, or
the superintendent of the well, was about fourteen: they consisted of a
smith and hammerman, whose duty it was to keep the tools in order; and
two shifts of men entrusted with the excavation, namely, an
engine-driver and stoker, a chief workman, or sub-foreman, and three
assistants. The total time employed in sinking the shafts executed upon
this system in the North of France, where it has been applied without
meeting with the accidents encountered in the Passy well, was found to
be susceptible of being divided in the following manner: from 25 per
cent. to 56 per cent. was employed in manoeuvring the trepan; from 11
per cent. to 14-1/2 per cent. in raising and lowering the tools; from 19
per cent. to 21 per cent. in removing the materials detached from the
rocks, and cleaning out the bottom of the excavation; and from 8 per
cent. to 10-1/2 per cent. was lost, owing to the stoppage of the
engines, or to the accidents from broken tools, or to other causes
always attending these operations. In the well of Passy there was, of
course, a considerable difference in the proportions of the time
employed in the various details of the work; and the long period
occupied in obviating the effects of the slips which took place in the
clays, both in the basement beds of the Paris basin and in the
subcretaceous strata, would render any comparison derived from that well
of little value; but it would appear that, until the great accident
occurred, the various operations went on precisely as Kind had
calculated upon.
KIND-CHAUDRON SYSTEM.
[Illustration: Section through Kind-Chaudron Well at Durham.
Fig. 110.]
In the year 1872 Emerson Bainbridge, C.E., drew attention to the
Kind-Chaudron system of sinking mine shafts through water-bearing
strata, without the use of pumping machinery, in a paper read before the
Institute of Civil Engineers. As the operation is almost identical with
that which would have to be carried through in the case of a well sunk
through an upper series of water-bearing strata, of minor importance or
of impure quality, past rock and into the lower water strata, as for
instance through tertiaries and chalk into the lower greensand, the
following extract from Bainbridge's paper may be read with interest.
Public-domain text, read in full here on John Shaqi.
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