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
As an instance, suppose the catchment area to be 1000 acres, the mean
annual fall 60 inches, with a loss from evaporation and absorption
of 14 inches. The available rainfall of the year is (see last column
of table below) 23·8 inches, or 1·983̇ feet. The water impounded and
consumed during the year is 1000 × 43,560 × 1·983̇ × 6·25 = 539,962,000
gallons. The reservoir capacity must be 3/10ths of this, or 161,988,600
gallons. This is represented by the height C E. If the mean available
rainfall in January and February is 6·3 inches, or ·525 feet, the
water impounded during those months is 1000 × 43,560 × ·525 × 6·25 =
143,931,000 gallons, and the consumption is 539,962,000/6 = 89,993,667
gallons. The difference, 53,937,333 gallons, represents the addition
A C, to the reservoir. Similarly, the light summer rainfall causes
the depletion A E, and the heavy rainfall in the last four months of
the year the addition E B. If the height of the reservoir above A B
were less than A C, there would be overflow at the end of February;
and if the depth below A B were less than A E, the reservoir would go
dry before the drought ended. If the capacity of the reservoir were
increased either at the top or bottom, the cost would be increased and
nothing would be gained. It is not meant that the highest and lowest
levels of any reservoir designed as above would always, in the driest
year, exactly correspond with the points of overflow and going dry, but
they would do so nearly. Deacon states that such a reservoir would fail
only once in fifty years, and then only for a short time.
The reservoir considered above does not, as already remarked, fully
utilise the yield of the catchment area. In a wetter year there
would be overflow and the yield from the reservoir would not be much
increased. In order to equalise the flow of the two driest years
the capacity of the reservoir must be increased, its yield being
also increased, and so on for larger groups of years. By collecting
information for large numbers of places in the British Isles, Deacon
has prepared diagrams and tables which show the capacities and yields
of reservoirs. The following table gives the figures for the case where
the rainfall is 60 inches and the loss by evaporation and absorption 14
inches:--
Public-domain text, read in full here on John Shaqi.
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