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                                                                            2.3 Storage as a Function of Draft and Runoff  35
                    2.3  STORAGE AS A FUNCTION OF DRAFT AND RUNOFF

                                         A dam thrown across a river valley impounds the waters of the valley. Once the reservoir
                                         has filled, the water drawn from storage is eventually replenished by the stream, provided
                                         runoff, storage, and draft are kept in proper balance. The balance is struck graphically or
                                         analytically on the basis of historical records or replications generated by suitable statisti-
                                         cal procedures of operational hydrology.
                                             Assuming that the reservoir is full at the beginning of a dry period, the maximum
                                                               2
                                                                         2
                                         amount of water S (MG/mi or ML/km ) that must be withdrawn from storage to maintain
                                                                             2
                                                                   2
                                         a given average draft D (MG/mi or ML/km ) equals the maximum cumulative difference
                                                                                        2
                                                                              2
                                         between the draft D and the runoff Q (MG/mi or ML/km ) in a given dry period, or
                                                                S   maximum value of  (D   Q)                 (2.1)
                                             To find S,  (D   Q) is summed arithmetically or graphically. The mass diagram
                                          method illustrated in Fig. 2.7 is a useful demonstration of finding  (D   Q)   D   Q.
                                          The shorter the interval of time for which runoff is recorded, the more exact the result. As
                                          the maximum value is approached, therefore, it may be worthwhile to shift to short inter-
                                          vals of time—from monthly to daily values, for example. The additional storage identified
                                          by such a shift may be as much as 10 days of draft.

                                            700
                                                                           Reservoir drawn down
                                                                        Depletion            Replenishment
                                                                           of                     of
                                            600                          storage                storage  Reservoir  full



                                            500              Reservoir full  1. Draw cumulative draft   D  Reservoir empty  Must intersect
                                           Cumulative runoff and draft, MG  400  period at point  parallel to rate of draft A  Cumulative


                                                                                                     runoff curve,
                                                                and tangent to curve B.
                                                                                                      if reservoir
                                                                                                      is to refill.
                                                                           3. Measure maximum
                                                                                                Curve B.
                                                   Start of dry
                                                                           deficiency cumulative
                                                                            D  Q   124 MG
                                            300
                                                                                                runoff,  Q
                                                  of tangency.
                                                                 Storage, S
                                                                                               End of dry
                                            200                Q  D   124 MG                 period at point
                                                                                              of tangency.
                                                                     2. Draw parallel to line A
                                                                     and tangent to curve B.
                                            100                                 Line A, slope   rate of draft.
                                                       Must intersect runoff curve,
                                                         if reservoir is to be full
                                                         at start of dry period.
                                              0
                                               0   1    2   3    4   5   6    7   8   9   10   11  12  13   14  15
                                                                          Order of months

                                         Figure 2.7 Mass-Diagram Method for the Determination of Storage Required in Impounding Reservoirs
                                                                      2
                                                                                  2
                                         (A constant draft of 750,000 gpd/mile   23 MG/mile for a month of 30.4 days is assumed)
                                         Conversion factors: 1 MG   1,000,000 gal   3.785 ML   3,785,000 L;
                                                                         2
                                                               2
                                                  2
                                         1 MG/mile   1.461 ML/km ; 1 gpd/mile   1.461 L/d/km 2
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