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 accurate statistics of rainfall are required for any work, the
rainfall of the tract concerned must be specially studied and local
figures obtained for as many years as possible. Very frequently it is
necessary to set up a rain-gauge, or several if the tract is extensive
or consists of several areas at different elevations. Sometimes there
is only a year or so in which to collect figures. In this case the
ratio of the observed fall to that, for the same period, at the nearest
station where regular records are kept, is calculated. This ratio is
assumed to hold good throughout, and thus the probable rainfall figures
for the new station can be obtained for the whole period over which
the records have been kept at the regular station. The volumes of the
British Rainfall Organisation contain a vast amount of information
regarding rainfall. For a large area there should be one rain-gauge for
every 500 acres, for a small area more. In the case of a valley there
should be at least three gauges along the line of the deepest part--one
at the highest point, one at the lowest, and one midway as regards
height--and two gauges half way up the sides and opposite the middle
gauge (_Ency. Brit._, Tenth Edition, vol. xxxiii.). Some extra gauges
may be set up for short periods in order to see whether the regular
gauges give fair indications of the rainfall of the tract. If they do
not do so some allowances can be made for this.
2. =Available Rainfall.=--The area drained by a stream is called its
“catchment area” or “basin.” The available rainfall in a catchment area
is the total fall less the quantity which is evaporated or absorbed
by vegetation. The evaporation does not chiefly take place directly
from the surface. Rain sinks a short distance into the ground, and
is subsequently evaporated. The available rainfall does not all flow
directly into the streams. Some sinks deep into the ground and forms
springs, and these many months later augment the flow of the stream and
maintain it in dry seasons. The available rainfall of a given catchment
area is known as the “yield” of that area.
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