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Gas exchange                                                          263

                   per °C. Usually a value of 2.4 percent per °C is adopted (Thomann and Mueller, 1987)
                   (compare Equation 13.20):

                    k  (T )   k  ( 20o )  . 1 (  024 ) T  20                          (14.22)
                     L        L
                   where T = the water temperature (°C).
                      Example 14.2  Reaeration

                      In a small lake at an altitude of 100 m above sea level, the dissolved oxygen  concentration
                             -1
                      is 4 mg l , the water temperature is 13 °C, and the wind speed 10 m above the water
                                     -1
                      surface is 7.5 m s . Estimate the oxygen  flux density  during a rain shower with an
                                       -1
                      intensity of 10 mm h .
                      Solution
                      First, calculate the oxygen  exchange coefficient at 20 °C due to wind. As the wind speed
                                               -1
                      at 10 m is greater than 1.82 m s , use Equation (14.17):
                      k  L ,W     . 0  0864    . 8  5 . 7  5 . 0  . 3  67  5 . 7     . 0  43  5 . 7  2   43     . 1  706  m d  -1

                      Second, calculate the oxygen  exchange coefficient at 20 °C due to precipitation, using
                      Equations (14.19) and (14.20):
                       B     10  6     . 0  103  100  2390    10  . 1 26     . 0  0437
                      k  L  ,P     24 . 45  . 0  0437    . 1  068  m d -1

                      Thus, wind contributes more to the reaeration  than precipitation. The resulting oxygen
                      exchange coefficient at 20 °C is estimated using Equation (14.21):

                      k        . 1  706    . 1  068  . 0  047  . 1  706  . 1  068    . 2  689  m d -1
                        , L  20oC
                      The oxygen exchange coefficient at 13 °C is calculated using Equation (14.22):

                      k        . 2  689  . 1  024  7     . 2  277  m d -1
                        , L  15oC
                      Then estimate the saturated dissolved oxygen  concentration at 13 °C, using Equation
                      (14.14):

                                                                           3
                                                                                         -3
                                                                                    -1
                      DO sat    14 . 652  . 0  41022  13   . 0  007991  13 2  . 0  0000777774  13   10  5 .  mg l  (=g m )
                      Finally, determine the oxygen  flux density  across the air–water interface (see Equation
                      14.10):
                                                                    -2
                                                                      -1
                                                                                     -1
                                                                                   -2
                      J     k  L  (DO  DO sat  )    . 2  277  7 (  10  ) 5 .     . 7  97  g m  d  = 0.092 mg m  s .
                   14.4  GAS EXCHANGE CONTROLLED ON THE WATER SIDE
                   The empirical relationships presented above can, in principle, also be used for gases
                   other than oxygen, provided that the gas exchange is controlled on the water side (K’  >>
                                                                                        H
                   0.01) and the gas is non-reactive. The gas exchange coefficient  k  must be corrected for

                                                                        L







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