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Precipitation                                                                                    669



            and with residual Ca 2þ  and Mg 2þ  concentrations measured as  a ‘‘complex’’ ion (or a ‘‘chelate’’). Manganese, as another
            the dependent variables. The jar test results are plotted with  example, has several oxidation states, for example, Mn(s),
            Ca 2þ  and Mg 2þ  concentrations plotted on the ordinate against  which reacts with H þ  in the aqueous phase to form
            the lime or lime=soda dosages on the abscissa.     Mn (aq) and H 2 (g), E 8 ¼ 1.1.8 V (Silberberg, 1996,
                                                                  2þ
                                                               pp. 982–984). Also, as stated by Silberberg, like chromium,
            21.2.2.5  Lime-Soda Process                        manganese can use all its valence electrons in its compounds,
            The portion of hardness that has no alkalinity counterions  exhibiting every possible oxidation state, with the þ2, þ4,
            associated with it is ‘‘permanent’’ hardness. For example, if  and þ7 states being most common. As the oxidation state of
                                                               manganese increases, its ‘‘valence state electronegativity’’
            the counterions are Cl ,SO 4 ,NO 3 , etc., the carbonate,
                                    2


            that is, CO 3 , must be supplied from an external source; the  also increases and its oxides change from basic to acidic.
                     2
            most common is soda, that is, Na 2 CO 3 . Looking at the net  Mn(II) is basic, and manganese (III) oxide, Mn 2 O 3 , is ampho-
            reaction only, the associated reaction is          teric. Manganese (IV) oxide, MnO 2 , is insoluble and thus
                                                               shows no acid–base properties. Manganese (VII) oxide,
                                                               Mn 2 O 7 , forms by reaction of Mn with pure O 2 and reacts
                          Ca 2þ  þ CO 3  2   ! CaCO 3   (21:7)
                                                               with water to form permanganic acid, HMnO 4 , a strong oxi-
                                                               dizing agent. All manganese species with oxidation states
            The soda ash demand is the stoichiometric amount needed to
                                                               >þ2 act as oxidizing agents, but the permanganate ion is
            satisfy the requirement for permanent hardness.
                                                               particularly powerful. As with chromium in its highest oxida-
                                                               tion state, MnO 2 is a much stronger oxidant in acidic solu-

            21.2.3 CHEMISTRY OF METALS                         tion than in a basic solution, that is,
            The chemistry of metal ions may be rather complex because of
                                                                        MnO 4 (aq) þ 4H (aq) þ 3e
                                                                                      þ

            the different valence states and complexes that may form. For
            example, arsenic is stable in four oxidation states, that is, þ5,  ! MnO 2 (s) þ 2H 2 O E ¼ 1:68 V  (21:8)

            þ3, 0, and –3, depending on the redox potential (with values
                                                                         MnO 4 (aq) þ 2H 2 O(aq) þ 3e

            high to low, respectively). The aqueous forms are mostly
            arsenite, As(III), and arsenate, As(V); and in an oxidizing    ! MnO 2 (s) þ 4OH    E ¼ 0:59 V  (21:9)

            environment the arsenate predominates, and under moderately
            reducing conditions arsenite is the major species. Because of  Table 21.4 summarizes the foregoing discussion, showing
            slow kinetics, however, both arsenite and arsenate may exist in  oxidation states of manganese, with examples on the line
            either redox environment. Some forms of arsenic are removed  below, and the acid–base level associated with the respective
            more easily than others, with oxidation state being a major  oxidation state. The top line depicts the expected appearances
            factor. To illustrate further the complexity of removal, the  of the respective oxidation states, with the second line
            reaction between arsenate and iron (Fe ) forms an insoluble  describing color.
                                           3þ
            precipitate, ferric arsenate, FeAsO 4 ; on the other hand, ferric  As related to natural cycles of manganese, Mn , the
                                                                                                          2þ
            arsenite, FeAsO 3 , is soluble in water and does not precipitate.  reduced form, occurs in a reducing atmosphere, that is,
              Many of the other metals, for example, Al, Cd, Cr, Cu, Fe,  anoxic. When withdrawn for drinking water, the Mn 2þ  will
            Hg, Mn, Pb, also have multiple oxidation states and=or may  oxidize at some point in the system, with MnO 2 being a
            serve as the ‘‘central’’ atom with associated ‘‘ligands’’ to form  product; MnO 2 causes the black water noted by customers
                           TABLE 21.4
                           Examples of Oxidation States of Manganese





                            Depiction
                            Color         Pale pink a  Black     Br-blake a   Green a   Purple a
                            Oxidation state  Mn(II) b  Mn(III)   Mn(IV) b     Mn(VI)    Mn(VII) b
                            Example       Mn 2+       Mn 2 O 3   MnO 2        MnO 4 2–  MnO 4 –
                            Oxide acidity  Basic                                        Acidic

                           Source: Adapted from Silberberg, M., Chemistry—The Molecular Nature of Matter and Change,
                                  Mosby-Year Book, Inc., St. Louis, MO, 1996.
                           a
                             Silberberg (1996, p. 984; Casale et al. 2002, p. 109).
                           b
                             Most common species.
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