Page 100 - Water and wastewater engineering
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GENERAL WATER SUPPLY DESIGN CONSIDERATIONS 2-43

                2-8.    Using a spreadsheet you have written and the data in  Table 2-7 , continue the analysis
                   of the required storage volume begun in  Example 2-3  through April, 2001. What size
                   reservoir is required? Is it full at the end of the April 2001? Ignore the need for
                   increased volume for sediment.
                2-9.    Using a spreadsheet you have written and the data for the Hoko River near Sekiu,
                   WA, below, determine the required storage volume for a uniform demand
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                   of 0.35 m  /s for the period January 1969 through December 1973. Assume a regula-
                   tory restriction that allows only 6% of the flowrate to be withdrawn. What size reser-
                   voir is required? Is it full at the end of December, 1973? Ignore the need for
                   increased volume for sediment.
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                2-10.   Eudora is served by a single well that pumps at a rate of 0.016 m  /s. They anticipate
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                   the need for a pumping rate of 0.025 m  /s. They would like to use the current well and
                   replace the pump with a higher capacity pump. The artesian aquifer is 10 m thick with
                   a piezometric surface 40 m above the bottom confining layer. The aquifer is a medium
                   sand. After 300 days of pumping, the drawdown at a nonpumping well 200 m from
                   the pumping well is 1 m. The pumping well is 1 m in diameter. Assuming a typical
                   hydraulic conductivity for medium sand, determine the maximum allowable sustained
                   pumping rate.


          Hoko River near Sekiu, WA
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          Mean monthly discharge (m /s)
          Year      Jan    Feb     Mar     Apr    May     June   July    Aug     Sept   Oct     Nov    Dec
          1963      12.1   15.0     8.55   9.09   5.78    1.28   2.59    1.11     .810  13.3    26.1   20.3
          1964      27.3   12.2    18.0    8.21   4.08    3.62   4.53    2.44    4.28    7.67   13.3   14.7
          1965      27.4   27.3     5.01   5.61   6.68    1.38    .705    .830    .810   7.31   16.8   19.6
          1966      29.8   11.3    17.6    5.18   2.67    2.10   1.85     .986   1.54   10.3    17.0   39.0
          1967      35.6   26.8    18.5    6.51   3.43    1.46    .623    .413    .937  25.7   14.2    27.8
          1968      34.2   22.4    15.7    9.20   3.68    2.65   1.72    1.55    9.12   16.8   16.5    25.2
          1969      17.2   18.5    12.9   12.8    3.74    2.23   1.19     .810   6.15    7.84   9.15   15.9
          1970      17.3   12.1     8.50  17.7    3.85    1.32    .932    .708   4.22    7.96   13.9   25.4
          1971      32.7   21.0    21.1    8.13   3.43    2.83   1.83     .932   2.22   10.7    22.7   22.0
          1972      27.4   26.9    25.4   14.6    3.00    1.00   5.32     .841   2.00    1.14   11.8   37.8
          1973      28.0    9.23   11.3    4.13   5.30    4.93   1.63     .736    .810  13.1    29.8   31.5


                  2-11.   Your supervisor has asked you to make a first approximation estimate of the maxi-
                   mum allowable sustained pumping rate for a 1 m diameter well located in a confined
                   aquifer. She has given you the well boring log shown below. Your firm uses a 2 m
                   safety factor to ensure that the piezometric surface is not lowered below the aqui-
                   clude. She has said you may assume that the aquifer has a typical hydraulic conduc-
                   tivity. For a first trial assume that the drawdown in an observation well 100 m away
                   from the pumping well is 0.0 m; that is, the pumping well’s radius of influence is
                     100 m.
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