Page 312 - Air pollution and greenhouse gases from basic concepts to engineering applications for air emission control
P. 312

10.3  Flue Gas Desulfurization                                  289

                                    CaCO 3 ! CO 2 þ CaO                  ð10:5Þ

              The simplified reactions for desulfurization are

                               Ca OHÞ þSO 2 ! CaSO 3 þ H 2 O             ð10:6Þ
                                  ð
                                      2
              The liquid after reaction is collected at the bottom of the scrubber and is partially
            recycled. The rest of the used solution stream is fed to the thickener to convert
            calcium sulfite to calcium sulfate by oxidation.
                                1
                 CaSO 3 þ 2H 2 O þ = 2O 2 ! CaSO 4 þ 2H 2 O ! CaSO 4   2H 2 O  ð10:7Þ
              Limestone/lime FGD is sensitive to acidic or alkaline components in the flue gas.
            Acidic components reduce the pH value and change the equilibrium for SO 2
            absorption (Eq. (10.6)). Therefore, a pre-scrubber is useful to remove the acidic
            components, fly ash, and mercury from the flue gas. It also improves the quality of
            the gypsum. Alternatively, organic buffers can be applied to maintain a constant pH
            of the solution. This also lowers the capital cost by lowering the absorber size and
            pumping accessories.



            10.3.1.1 Other Chemical Sorbents

            There are other sorbents that can also react with SO 2 in the flue gas. For example,
            Mg(OH) 2 (magnesium hydroxide) can react with SO 2 and produce MgSO 3 (mag-
            nesium sulfite):

                              Mg OHÞ þ SO 2 ! MgSO þ H 2 O               ð10:8Þ
                                 ð
                                     2              3
              Similarly, caustic (NaOH) can react with SO 2 producing sodium sulfite
                              2NaOH þ SO 2 ! Na 2 SO 3 þ H 2 O           ð10:9Þ

              Seawater is a natural alkaline to absorb SO 2 . When SO 2 is absorbed into the
                                                                             +
            seawater, it reacts with oxygen and water to form sulfate ions SO 4 − and free H .
                          +
            And surplus of H is offset by the carbonates in seawater pushing the carbonate
            equilibrium to release CO 2 gas:
                                          1
                             SO 2 þ H 2 O þ = 2O 2 ! SO 2   þ 2H þ      ð10:10Þ
                                                     4
                                          þ
                                HCO þ H ! H 2 O þ CO 2                  ð10:11Þ
                                    3
   307   308   309   310   311   312   313   314   315   316   317