River and Canal Engineering, the characteristics of open flowing streams, and the principles and methods to be followed in dealing with them.Bellasis, E. S. (Edward Skelton)
Science
River and Canal Engineering, the characteristics of open flowing streams, and the principles and methods to be followed in dealing with them.
Bellasis, E. S. (Edward Skelton)
Canals; Hydraulic engineering; Rivers
At the site of the railway bridge over the river Tista in Bengal, it
was necessary to close the main stream (fig. 25), which flowed at the
left side of the channel, while the bridge had been built at the right.
The bed was of sand, width 500 feet, depth 6 feet, and discharge 3700
cubic feet per second. The first attempt to close the stream was made
at M N, a floor of stone 200 feet long, 20 feet wide, and 2 feet
thick, being laid in the middle of the stream, and dams of earth,
sandbags, and stones being run out from each bank. As the gap decreased
in width the bed was torn up and the work failed. The heading up was 3
feet 9 inches. It was recognised later that the site should have been
at the bifurcation higher up, and that the stone floor should have been
laid on a mattress.
In the next working season the dams C D and E F G were made. The dam C
D was of earth. Two walls, each consisting of a double line of bamboos
with the spaces between the lines filled with bundles of grass weighted
with earth, were run out 50 feet in advance of the earthwork near the
lines of the toes of the slopes. Along the line of the upper wall a
mattress of broken bricks 10 feet in width, and 1 foot thick, was laid,
and was kept 50 feet in advance of the wall. A total length of 1000
feet of embankment was made in five months and pitched on its upstream
side. The end was strongly protected by a mass of stone. The embankment
F G was of earth. The dam E F consisted of three lines of piles driven
10 feet into the bed. A mattress weighted with stones extended for 20
feet upstream of the dam and 40 feet downstream. A gap of 150 feet was
left at D E, and was not protected by a floor of any kind. A channel,
parallel to F G and extending to K, had been dug to a width of 200
feet. During the floods the heading up at D E was about 2·5 feet, and
the water was 30 feet deep. The line E F was greatly damaged and was
repaired. The cut F G K gradually enlarged, and by the end of the
floods more water was going down it than down the main stream. The gap
D E was finally closed by means of a line of bamboos and grass, the
bed being protected by a carpet, 100 × 50 feet, made of common cloth
weighted with sandbags. The success of the operations turned on the
scouring out of the cut F G K. It is remarkable that the gap D E did
not become wholly unmanageable in the floods (_Min. Proc. Inst. C.E._,
vol. cl.).
CHAPTER VIII
THE TRAINING AND CANALISATION OF RIVERS
Public-domain text, read in full here on John Shaqi.
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