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
If a stream can be turned into a large pond or low ground--a bank being
built round it if necessary--it can be made to part with some or all of
its silt whether rolled or suspended. Even if the pond is so large that
the velocity becomes imperceptible, the whole of the suspended matter
will not deposit unless it has sufficient time, but the matter which
remains in the water is likely to be extremely small in amount. The
silting up of marshes, pools, borrow-pits, etc., is now being effected,
or should be effected, in places where mosquitoes and malaria are
prevalent.
In the upper or torrential part of a stream, a high dam, provided with
a sluice and a high-level waste weir, may be built across it. The space
above the dam becomes more or less filled with gravel, etc. This has
been done in Switzerland (_Min. Proc. Inst. C.E._, vol. clxxi.). In
the U.S.A. long weirs have been built in order to stop the progress of
detritus from gold mines. Such detritus was liable to choke up rivers
and damage the adjoining lands. The detritus from hill torrents can
also be reduced by afforestation of the hill sides.
[Illustration: FIG. 3.]
[Illustration: FIG. 4.]
When a stream is in embankment--irrigation channels are frequently
so--the bank can be set back (fig. 3), and suspended silt will then
deposit on the berms. The object of this arrangement is generally to
create very strong banks in low ground. A similar plan can be adopted
when the berm is only slightly below the water-level and even when it
is only occasionally submerged. In this case the deposit of a small
bank of silt along the edge of the berm next the stream will prevent
the access of fresh supplies of silt-bearing water to the parts further
away. Gaps should be cut in the bank of silt at intervals, and cross
banks made to form “silting tanks,” as shown in fig. 4. The inlets to
the tank should be large, and the outlets small, so that the water in
the tank may have little velocity. It is not, however, correct to have
the outlet so small--unless the water contain very little silt--that
there is very little flow through the tank. The tanks will generally
be silted up most quickly by allowing a good flow through them, even
though only a small proportion of the silt in the water is deposited.
Regular banks arranged to form tanks on the above principle can be made
behind the original banks of a canal in cases where the original banks
were not, for any reason, set back.
When a channel is made in low ground and the excavation is not
sufficient to make the banks, borrow-pits can be dug in the bed of the
channel. Such pits should not be long and continuous, but wide bars
should be left so that a number of short pits will result. These pits
will trap rolled material as well as suspended silt. The object in
this case is to free the water from silt and to reduce the size of the
channel and thus reduce the loss of water from percolation.
Public-domain text, read in full here on John Shaqi.
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