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
When the water-level is raised by a weir or by narrowing the
channel--though in the latter case the raising may not be permanent--it
is generally best to commence the work from the upstream end. The
raising of the water-level will then not interfere with the execution
of the rest of the work. But in a case of widening, where the
water-level upstream of the work is lowered, the work can conveniently
be begun at the downstream end, and the remark applies also to a case
of straightening, provided that the new channel is not so small that
it at first causes no lowering. In any case in which there is a doubt
whether the whole of the scheme will be carried out, the reach to be
dealt with first can be decided on according to circumstances. There is
no general reason for selecting an upstream or downstream reach, except
that any raising or lowering of the water-level will extend upstream of
the reach and not downstream of it (CHAP. I., _Art. 4_).
Training walls and groynes, if made with stakes or fascines or any
materials except stone, require careful watching and maintenance.
CHAPTER IX
CANALS AND CONDUITS
1. =Banks.=--All banks which have to hold up water should be carefully
made. The earth should be deposited in layers and all clods broken
up. In high banks the layers should be moistened and rammed. The
dotted lines in fig. 29 show two possible courses of percolation
water. The vertical height--from the water-level to the ground outside
the bank,--divided by the length of the line of percolation is the
hydraulic gradient, as in the case of a pipe, and this gradient is
more or less a measure of the tendency to leakage. A bank which has
water constantly against it nearly always becomes almost water-tight in
time. The time is less or greater according as the soil is better, and
according to the amount of care with which the bank is made.
[Illustration: FIG. 29.]
The side slopes of banks vary with the soil. Generally they are 1½ to
1, but they are sometimes 2 to 1 or even 3 to 1 if the soil is bad or
sandy, or if great precautions against breaches are to be taken.
Leakage can sometimes be stopped by throwing chaff or other finely
divided substances into the water at the site of the leak. In other
cases it is necessary to dig up part of the bank, find the channel
by which the water is escaping, and fill it up by adding earth and
ramming. On some navigable canals in France it was at one time the
custom to lay the reach dry, when a bad leak occurred, and to dig away
the bank and lay slabs of concrete or puddle over the place. This plan
was abandoned, and instead of it sheet piles are driven in. They are
then withdrawn one at a time and, if any leakage occurs, the space is
filled with concrete.
Public-domain text, read in full here on John Shaqi.
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