Scientific American Supplement, No. 595, May 28, 1887Various
Science
Scientific American Supplement, No. 595, May 28, 1887
Various
Science -- Periodicals
It was the practice until comparatively recently to make the discharge
outlet by laying pipes in a trench under the dam, generally at the lowest
point in the valley, or constructing a culvert in the same position and
carrying the pipes through this, and in the earlier works the valves or
sluices regulating the outflow were placed at the tail of the down stream
bank, the pipes under the bank being consequently at all times subject to
the pressure of the full head of the water in the reservoir. An instance
of the first mentioned method is afforded by the Dale Dyke reservoir,
Fig. 2, where two lines of pipes of 18 in. diameter were laid in a trench
excavated in the rock and resting upon a bed of puddle 12 in. in
thickness, and surrounded by puddle; the pipes were of cast iron, of the
spigot and faucet type, probably yarned and leaded at the joints as
usual, and the sluice valves were situated at the outer end of the pipes.
As the failure of this embankment was, as we all know, productive of such
terrible consequences, it may be of interest to enter a little more fully
into the details of its construction. It was situated at Bradfield, six
or seven miles from Sheffield, and at several hundred feet higher level.
Its construction was commenced in 1858, the puddle trench was probably
taken down to a depth of 40 ft. to 50 ft., a considerable amount of water
being encountered. This trench was 15 ft. to 20 ft. broad at the top, and
of course had to be crossed by the before mentioned line of pipes; and
although the trench was filled with puddle, and the gullet cut in the
rock already mentioned for carrying the pipes under the site of the dam
was "padded" with a layer of 12 in. of puddle, we can imagine that the
effect of the weight of the puddle wall and bank upon this line of pipes
would be very different at the point where they crossed the puddle trench
to what it would be where they were laid in the rock gullet and partially
protected from pressure by the sides of the latter. At the trench
crossing there would be a bed of puddle 50 ft. in thickness beneath the
pipe, in the gullet a bed of 1 ft. in thickness. So much as regards the
laying of the pipes.
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