Page 268 - Materials Chemistry, Second Edition
P. 268

Groundwater Remediation                                          251



           ozone. Each mole of hydrogen peroxide in water can dissociate into 0.5 mole
           of oxygen and 1 mole of water, while 1 mole of ozone in water can dissociate
           into 1.5 moles of oxygen as:

                                    H O  → H O + 0.5 O 2                  (6.28)
                                        2
                                      2
                                             2
                                        O  → 1.5 O 2                      (6.29)
                                          3
             Ozone is 10 times more soluble in water than pure oxygen. Hydrogen per-
           oxide and ozone can be added to the extracted groundwater before it is put
           back to the impacted aquifer. It should be noted that hydrogen peroxide and
           ozone are also strong oxidants. In addition to providing oxygen for biodegra-
           dation, they can also generate radicals to oxidize COCs and other inorganic
           and organic compounds present in the aquifer. However, at higher concen-
           tration levels, they may become toxic to indigenous aerobic microorganisms
           and suppress their biological activities [3].
             Various  enhanced  in  situ  biodegradation  approaches  rely  on  oxygen-
           releasing compounds. The common ORCs include calcium and magne-
           sium peroxides that are introduced to the saturated zone in solid or slurry
           phases. These peroxides release the oxygen to the aquifer when hydrated
           by groundwater. Magnesium peroxide has been more commonly used
           than calcium peroxide due to its lower solubility and prolonged release
           of oxygen. Oxygen amounting to ≈10% of the mass of magnesium perox-
           ide placed in the saturated zone is released to the aquifer over the active
           period [3].


           Example 6.14:   Determine the Necessity of Oxygen Addition
                         for In Situ Groundwater Bioremediation

           A subsurface is impacted by gasoline. The average dissolved-gasoline con-
           centration of the groundwater samples is 20 mg/L. In situ bioremediation
           is being considered for aquifer restoration. The aquifer has the following
           characteristics:

              •  Porosity = 0.35
              •  Organic content = 0.02
              •  Subsurface temperature = 20°C
              •  Dry bulk density of aquifer materials = 1.6 g/cm 3
              •  DO concentration in the aquifer = 4.0 mg/L


             Illustrate that the addition of oxygen to the aquifer is necessary to support
           biodegradation of the intruded gasoline.
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