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Adsorption                                                                                       459



            natural organic matter (NOM) from natural waters at low pH,  blood, petroleum residues, etc. The characteristics of activated
            e.g., by addition of acid prior to the column. The NOM is  carbon are derived from both the nature of the raw material
            eluted by adding a concentrated base.              used and the conditions of manufacture. For example, coal as
                                                               a source results in a hard and dense product; but no two coal
            15.1.2.1.3  Activated Alumina                      seams are alike (Greenbank and Spotts, 2003).
            Activated alumina is amphoteric, i.e., it has a positive charge
            at pH < pHpzc and a negative charge at pH > pHpzc (pHpzc  15.1.2.3  Manufacturing of Activated Carbon
            is the pH at which the charge is zero). The removal of ions is
                                                               The preparation of an activated carbon from a given raw
            complex and occurs by chemisorption, forming a surface
                                                               material generally involves three main steps (West, 1971,
            complex via covalent bond, or by ion-exchange (Fleming,
                                                               p. 6): (1) grinding, (2) carbonization, and (3) activation. The
            1986, pp. 159–160). Activated alumina is an oxide or hydrox-
                                                               grinding produces a specified particle size. Carbonization or
            ide of aluminum. It is one of the few options for the removal
                                                               pyrolysis, the second step, is the heating of the raw material in
            of fluoride ion. It is classified here as an ion-exchange mater-
                                                               an inert atmosphere to drive off volatile substances and
            ial rather than an adsorbent and, therefore, is discussed more
                                                               increase the proportion of pure carbon. The process tempera-
            thoroughly in Chapter 16.
                                                               ture is about 8008C; the product is called a ‘‘calcinate.’’ The
                                                               final step is ‘‘activation,’’ an oxidation reaction, which burns
            15.1.2.1.4  Aluminum Hydroxide Floc
                                                               residual hydrocarbons at temperatures 8008C–9508C. The
            Natural organic matter (NOM) has been found to adsorb on  oxidizing gas may be steam, carbon dioxide, or oxygen.
            aluminum hydroxide floc (see Section 9.3.2.3) in accordance  This reaction increases the pore volume producing a network
            with an isotherm relation. While the removal of NOM during  of microscopic pores and creates active functional groups on
            coagulation has become a goal in drinking water treatment,  the internal surfaces. To give an idea of the effect of carbon-
            the context is that of a passive removal vis-à-vis an engineered  ization, in one example involving a Wyoming coal, the per-
            reactor. In other words, NOM removal occurs, but coagula-  cent of fixed carbon increased from about 45% in the coal to
            tion is the primary objective; NOM removal is increased in  about 90% in the calcinate product.
            accordance with a stoichiometric addition of alum (called  The skeleton of calcinate is composed of plates of graphite
            ‘‘enhanced coagulation,’’ Section 9.1.2.1).        created from the starting material. The size and degree of
                                                               imperfection of the plates (i.e., spacing, angle, size of gaps
            15.1.2.1.5  Soil Organic Carbon                    between neighboring plates, and the general structural order)
            The organic fraction in soils is largely amorphous matter and  is related to the chemical building blocks that comprised the
            (Marshall, 1964, p. 158). Its adsorptive character is difficult to  starting material and the heat of activation. Two character-
            determine.                                         istics of interest are (1) the surface area of the resulting
                                                               carbon, and (2) kinetics. Surface area is determined by the
            15.1.2.1.6  Soil Minerals                          voids between plates and the pore structure. Kinetics is deter-
            Clays, e.g., montmorillonite, illite, kaolinite, function as ion-  mined by the size of the pores and their nature (e.g., their
            exchangers (see Chapter 16) and are noted for small size and  tortuosity).
            large specific surface areas, e.g.,
                                                               15.1.2.4  Characteristics of GAC
                             Particle Size a  Specific Surface Area a  Activated carbon is manufactured as powdered or granular.
                                                   2
                                (mm)             (m =g)        Granular carbons are those larger than US Sieve Series
                                                               No. 50, i.e., d(50)   0.3 mm, while powdered carbons are
              Kaolinite         0.3–3            10–20
                                                               smaller. Granular carbons are used in packed beds or fluidized
              Illite            0.1–2            80–100
                                                               beds while powdered carbons are used in slurries or in com-
              Montmorillonite   0.1–1           800
                                                               plete-mix reactors. Table 15.1 compares data for four manu-
              a
                Lambe and Whitman (1969).                      factured granular activated carbons, illustrating the variation
                                                               in properties; each manufacturer produces a range of products.
            As seen, nominal sizes are 1 mm, with specific surface areas  15.1.2.4.1  Physical Properties
                    2
            10–800 m =g; also, the clays tend to be ‘‘platy’’ in shape. The
                                                       2
            large surface areas for these clays, i.e., even 10–20 m =g for  The properties of activated carbon which are of interest
            kaolinite, render them amenable to adsorption as well as ion-  include hardness, resistance to abrasion, density, and size.
            exchange.                                          The values of a few representative carbons are given in
                                                               Table 15.1. Standard tests (USEPA, 1973) have been devised
            15.1.2.2  Sources of Activated Carbon              as measures of these properties and are summarized in the
            Almost any carbonaceous matter can serve as raw material in  following paragraphs.
            the manufacture of activated carbon. Some of these materials  Hardness number: Hardness is a quality of the retention
            include wood, coal, peat, lignin, nut shells, lignite, bone,  of original surfaces. It is measured by subjecting 50.0 g of
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