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CAPACITY OF RESERVOIR

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Originally appearing in Volume V28, Page 391 of the 1911 Encyclopedia Britannica.
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CAPACITY OF See also:

RESERVOIR /N GALLO See also:Note.—The figures in the right-See also:hand See also:column at the ends of the curved lines are inches of mean See also:annual rainfall over a See also:period of 5o years. The co-ordinates to any point upon any curved See also:line give respectively the required reservoir capacity and daily yield in gallons per See also:acre of drainage See also:area, corresponding with the mean annual rainfall • represented by that curved line. The curves have been See also:drawn for a mean annual evaporation of rq in. For any increased See also:rate of evaporation r / in. are to be subtracted from the rainfall for each See also:inch of evaporation above 14 in. For any decreased rate of evaporation r in. are to be added to the rainfall for each inch of evaporation below 14 in. Any excess of evaporation from the See also:water See also:surface and See also:allowance for bottom water are to be added to the storage so found. • The period over which the reservoir equalizes the flow is shown by the number of years marked on the straight radial lines. Where the See also:absolute minimum stream flow is known to be greater • than the minimum of icubic See also:foot per second per woo acres (ro8gallons • per acre per See also:day) assumed in the See also:diagram, the capacity of the reservoir as taken from the diagram may be reduced by the amount corresponding to that minimum flow for the particular rainf aU and evaporation. )FORA/NAGE AREA.

End of Article: CAPACITY OF RESERVOIR

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