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 explosion of gunpowder, by the expansion of the gases suddenly
evolved, develops an enormous force, and this force, due to the pressure
of a fluid, is exerted equally in all directions. Consequently, the
surrounding mass subjected to this force will yield, if it yield at all,
in its weakest part, that is, in the part which offers least resistance.
The line along which the mass yields, or line of rupture, is called the
line of least resistance, and is the distance traversed by the gases
before reaching the surface. When the surrounding mass is uniformly
resisting, the line of least resistance will be a straight line, and
will be the shortest distance from the centre of the charge to the
surface. Such, however, is rarely the case, and the line of rupture will
therefore in most instances be an irregular line, and often much longer
than that from the centre direct to the surface. Hence in all blasting
operations there will be two things to determine, the line of least
resistance and the quantity of powder requisite to overcome the
resistance along that line. For it is obvious that all excess of powder
is waste; and, moreover, as the force developed by this excess must be
expended upon something, it will probably be employed in doing mischief.
Charges of powder of uniform strength produce effects varying with their
weight, that is, a double charge will move a double mass. And as
homogeneous masses vary as the cube of any similar line within them, the
general rule is established that charges of powder to produce similar
results are to each other as the cubes of the lines of least resistance.
Hence when the charge requisite to produce a given effect in a
particular substance has been determined by experiment, that necessary
to produce a like effect in a given mass of the same substance may be
readily determined. As the substances to be acted upon are various and
differ in tenacity in different localities, and as, moreover, the
quality of powder varies greatly, it will be necessary, in undertaking
sinking operations, to make experiments in order to determine the
constant which should be employed in calculating the charges of powder.
In practice, the line of least resistance is taken as the shortest
distance from the centre of the charge to the surface of the rock,
unless the existence of natural divisions shows it to lie in some other
direction; and, generally, the charge requisite to overcome the
resistance will vary from 1/15 to 1/35 of the cube of the line, the
latter being taken in feet and the former in pounds. Thus, suppose the
material to be blasted is chalk, and the line of least resistance 4
feet, the cube of 4 is 64, and taking the proportion for chalk as 1/30,
we have 64/30 = 2-2/15 lb. as the charge necessary to produce
disruption.
[Illustration: Jumper.
Fig. 21.]
Public-domain text, read in full here on John Shaqi.
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