Page 221 - Fundamentals of Water Treatment Unit Processes : Physical, Chemical, and Biological
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176                            Fundamentals of Water Treatment Unit Processes: Physical, Chemical, and Biological



                              water)        ‘‘air  airbubble  concentration  C o  water)  0.024  0.024  of  entering system  be  to  with  at  of

                              air=m 3  C r ¼ Nb   pd b 3 =6)  the  *check: this is only  ‘‘required,’’ as  at B ¼ 10  (kg  air  saturated  respect  elevation  basin),  i.e.,
                            C r  0.0048  0.0069  termed,  by  Edzwald (1995, p. 8)  calculated to float the  air=m 3  Concentration  (assumed  to  atmosphere  C o ¼ H  (air)   P(atm)
                              (kg         r(air)  0.007—ok  was  C r  released’’  and is  ‘-mass  6.9 mg=L  floc  air  of


                              water)      ‘‘air-  by                       C a  water)  0.0264  0.0253  of  to  air  in  depth  at  C s ¼ H  I.e.,

                              air=m 3  f b ¼ N b   (pd b 3 =6)  bubble-volume  concentration’’  (kg  with  pressure  bubbles  nozzles,  depth)
                            f b  0.0040  0.0057  termed  (1995,              air=m 3  Saturation  concentration  respect  (air)   P(nozzle
                              (m 3      0.006—ok  was  f b  Edzwald  8)  p.

                                                                           (kg  C)   as  H(O 2 )  H(air)  X  þ  in  as


                            N b  (bubbles=m 3 )  1.2Eþ11  1.7Eþ11  ‘‘bubble-  the  concentration’’  20  H(air,  air=m 3 water=kPa air)  0.000243  0.000243  calculated  H(air)  molar  weighted  for  fraction  i.e.,  H(N 2 ),  X(O 2 )   H(O 2 )  (N 2 )   H(N 2 )-  8.4  Example


                                      Nb  is  number  N b ¼ N p   B  1.6*10 11 -ok          þ
                                                                           (mg  8C)  N 2 )  from  empirical  H(N 2 )  Data  H.6  Table
                                        per
                                          based
                                                 rise
                                      of
                     Balance  B  (bubbles=particle)  10  10  number  generated  is  and  8.10  1995,  showing  bubble–  of  agglomerate  B  of  H(N 2 ,T  water=atm  N 2 =L  19.60  19.60  as Calculated  of  fit  i.e.,  ¼ A(N 2 )    exp(B(N 2 )   T8C)  is  reference
                     Mass             the  is  B  bubbles  particle  Figure  on  (Edzwald,  14)  p.  velocity  particle  function  as  dp  and  best  data,

                     by                                                    (mg  8C)  O 2 )  from  empirical  H(O 2 )  Data
                     Conditions  (#=m 3 )  1.2.Eþ10  1.7.Eþ10  number  a  gave  13)  particles=mL  on  based  of  9)  H(O 2 ,T  water=atm  O 2 =L  44.62  44.62  as Calculated  of  fit  best  i.e.,  data,  ¼ A(O 2 )    exp(B(O 2 )   T8C)  reference  H.6  Table




                     Stated  N p  (#=mL)  12000  17000  particle  p.  (1995,  10 3 –10 5  was  used  calculations  p.  (1995,  is


                     for                the  is  concentration.  Edzwald  of  range  value  matching  Edzwald  depth)  (kPa)  108.569  104.127  pressure  nozzles,  depth)  where  equal  atmosphere
                     Solids             N p      The                       P(nozzle  Absolute  of  depth  P(nozzle  ¼ P(atm)    (1þD=10.33)  the  is  depth  one  pressure


                     Float    air=bubble)  Mass(bubble) ¼ r(air)   V(bubble)           at  i.e.,  10.33  water  to  of
                     to     Mass(bubble)  (kg  4.03486E-14  4.03486E-14                  i.e.,      for  pressure  law
                     Pressure  solids                                   8C  20  for  P(atmosphere)  (kPa)  98.987  80.693  Atmospheric  a  as  Z,  of  P(atmosphere)  ¼ 101325   10^  ( 0.00005456   Z)  vapor).  correction  water-vapor  Henry’s  using



                     Saturator  float  to  d b  (m=bubble)  4.E-05  4.E-05  bubble—  of  law  Henry’s  pressure  function  ‘-P(water  Note  in


                  (continued)  Required  concentration  air  Diameter  assumed  for  by  C a ,  D(nozzles)  (m)  1.00  3.00  of  Depth  manifold=nozzles  water  below  surface





                  CD8.3  of  of Calculation  gas)  air  from  r(molar)   MW  ¼ (P=RT)   MW(gas)=  corrected  pressure  bubbles  concentration,


                  TABLE  Calculation  (c)  r(air)  air=m 3  (kg  1.20406  1.20406  of  Density  calculated  PV ¼ nRT  r(molar)  ¼ n=V ¼ P=RT  r(mass)  ¼  (gas)=1000  1000-not  Water-vapor  air  in  Gas  (d)  Z(elevation)  (m)  0  1585  Elevation  above sea level
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