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OXIDATION AND DISINFECTION             10.41

                   • o ~, of organic substrate, microorganism or NH 3
                  x~">v/                            •  Products
                 o+\°/      Slow, selective


          /

          ~'9_                 /                               "~.  Organic  radical
            N~or/          /~"     ~  organic substrate, microorganisms  or NH 3  7
               09         /       ~-
              ~%,.      /        ~o'-/¢   Fast  nonselective   ~.
              %" %~06.   /      ~b'/                             Products
                    o.~   .   ,   0
                  ~t   organic radical  )/Oxidation  of bicarbonate ion
                          ~     (                 •  Bicarbonate radical
                        Hydroxyl   ~O+..  Moderate
                         radical   \'~¢.
                                  ~'':~¢~ of  carbonate ion
                                                 ~  Carbonate radical
                                        Fast
         FIGURE  10.19  Reaction pathways of ozone in water.  (Source:  J. Hoigne  and H. Bader,  "Role  of Hy-
         droxyl  Radical  Reactions  in Ozonation  Processes  in Aqueous  Solutions,"  Water Resources Bulletin, vol.
         10, 1976, p.  377.)


        nonselective in its oxidation of organic compounds, but at the same time, it is scavenged
        by carbonate and bicarbonate ions to form carbonate and bicarbonate radicals.
           These carbonate and bicarbonate radicals are of no consequence in organic reactions.
        Furthermore, the hydroxyl radicals  and organic radicals produced by autodecomposition
        become chain carriers  and reenter the autodecomposition reaction to accelerate  it.  Thus
        low-pH conditions favor the  slow,  direct oxidation reactions involving 03,  and high-pH
        conditions or high concentrations of organic matter favor the  autodecomposition route.
        High concentrations of bicarbonate or carbonate buffer, especially carbonate buffer, re-
        duce  the  rate  of  autodecomposition by  scavenging hydroxyl radicals.  This means that
         ozone residuals last longer at low pH and in highly buffered waters.
           The rate of autodecomposition is highly dependent on many factors,  including pH, UV
         light, temperature,  ozone concentration, and the presence of radical scavengers.  Decom-
        position can be  expressed,  assuming pseudo-first-order kinetics and in terms  of  ozone
        residuals, as
                                     Ct/C0 =  e -kr
         where Ct  =  ozone concentration at time t, mg/L
             Co =  ozone concentration at time 0, mg/L
              k =  decay rate  constant, L/min
               t =  time, rain
           For design purposes,  the decay rate constant must be determined for the water to be
         treated  under  expected  operating  conditions,  including  temperature,  pH,  and  water
         quality.


         Ozone Systems
         Ozone systems are typically comprised of four basic subsystems: ozone generation, feed
         gas preparation, contacting, and off-gas  disposal.
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