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Flocculation                                                                                     325



            Flocculent: (1) A chemical, e.g., a polymer, that contributes  of fully turbulent motion in a turbulent flow field
                   to the aggregation and growth of floc particles; the  (Casson and Lawler, 1990, p. 55) (see also
                   mechanism would be ‘‘bridging,’’ i.e., two or more  Chapter 10).
                   floc particles are attached to a molecular strand of  Kolmogorov’s universal equilibrium theory: Relates to the
                   polymer. (2) A coagulant chemical, e.g., alum or   net rate of change in the energy contained in the
                   ferric ion is sometimes called a ‘‘flocculent’’ (this  small-scale motions to the energy dissipation rate
                   definition is mentioned only because of its use in  of these motions (Casson and Lawler, 1990, p. 55).
                   the literature and is not defined unequivocally;  Monodisperse: A suspension having but one particle size.
                   rather, its definition is implied).          Orthokinetic flocculation: (1) Refers to flocculation induced
            Fractal: (1) A structure of formed aggregates (Gmachowski,  by a velocity gradient (Argaman and Kaufman,
                   1995, p. 1815). (2) See Chapter 9. (3) The concepts  1968, p. 5; Ives, 1978, p. 39). (2) See Chapter 9.
                   of fractal geometry provide a mathematical frame-  Perikinetic flocculation: (1) Refers to flocculation induced
                   work for description of the structure of irregular flocs  by a Brownian motion (Argaman and Kaufman,
                   (Spicer and Pratsinis, 1996a, p.1052).             1968, p. 5; Ives, 1978, p. 39). (2) See Chapter 9.
                                                               Primary particles: (1) Particles at the commencement of
            Fractal dimension: (1) An exponent in the relation, N ¼
                   z(d=d o ) D F  that characterizes the aggregate mass  flocculation in which all particles are considered to
                   of fractal (dimensionless). (2) A solid three-     be covered with coagulant and have diameters nearly
                   dimensional body has a mass which depends on the   equal (Tambo and Watanabe, 1979, p. 430). (2)
                   third power of some characteristic length (such as  Destabilized particles ready for aggregation (Arga-
                   the diameter of a sphere), so that a log–log plot of  man, 1971, p. 775). (3) The particles to be removed
                   mass against size should give a straight line with a  from the raw water, e.g., turbidity, microorganisms
                   slope of 3. When such plots are made for aggregates,  (viruses, bacteria, cysts, oocysts, algae, and other
                   lower slopes are found, with non-integer values. The  microscopic particulates).
                   slope of the line is known as the fractal dimension,  Root mean square velocity gradient: The root mean square
                   D F . In three-dimensional space, D F may take values  (rms) of the velocity fluctuation, u ,is defined,
                                                                                                  0
                   between 1 and 3, the lower value representing a
                                                                                            1=2
                   linear aggregate and the upper one an aggregate of                    02
                                                                                  u   u
                                                                                   0
                   uniform density or porosity. Generally, intermediate
                   values are found, and the lower the fractal dimen-
                   sion, the more ‘‘open’’ or ‘‘stringy’’ the aggregate  In a turbulent flow field, the velocity at any point
                   structure (Gregory, 1989, p. 215).                 fluctuates randomly; this fluctuation is dealt with
                                                                      statistically as the rms.
            G: A term defined by Camp and Stein (1943) as G ¼ dv=dy ¼
                          0.5
                   [P=(mV)] .                                  Scale of turbulence: Distance across which the velocity of an
            Heterodisperse: A suspension having a distribution of par-  eddy changes (François, 1987b, p. 1023). Energy
                   ticle sizes.                                       content of an eddy depends upon the scale of turbu-
            Hydrogen bond: Considered having a minor role in intra-   lence; the large eddies contain most of the energy of
                   particle bonding because of their short range; ener-  the system and to not dissipate energy.
                   gies are 3–10 kcal=mol (Hannah et al., 1967, p. 846).  Sludge blanket clarifier: See solids contact unit.
                   Considered, however, to be a major force in attach-  Solids contact unit: (1) A tank that has a center well used for
                   ment of flexible polymer chains to floc particles to  coagulation, with outer portion maintained as a
                   permit bridging and agglomeration.                 ‘‘sludge blanket.’’ The microflocs resulting from
            Isotropic turbulence: Isotropic turbulence is characterized  coagulation are forced up through the blanket, per-
                   by equal strain rates, i.e., velocity gradients, with  haps 0.7 m (2 ft) depth and fluidized, of larger
                   respect to direction. According to Tennekes and    floc particles; during their flow through the blanket,
                   Lumley (1972, p. 262), small eddies exhibit ‘‘local  these primary particles make contact during with
                   isotropy,’’ where any sense of direction is lost with  these previously formed floc particles. The solids
                   turbulence being increasingly scrambled at small   blanket is maintained at a desired depth by waste
                   scales. The range of wave numbers exhibiting local  flow of sludge from the bottom. The effluent flow
                   isotropy is called the equilibrium range (see also  leaves the clarifier by peripheral weirs. For those
                   anisotropic turbulence).                           floc particles that are suspended in the flow leaving
            Kolmogorov’s microscale: (1) The Kolmogorov’s micro-      the solids blanket, they may fall back to the
                   scale of turbulence is a particular eddy size, calcu-  sludge blanket. (2) Proprietary devices that combine
                   lated by the fluid viscosity and the energy dissipation  rapid mixing, flocculation, and sedimentation in
                                                                      one unit. These units provide separate coagulation
                   (François, 1987, p. 1023), i.e., l(Kolmogorov) ¼
                     3
                   (n =e) 1=4 . (2) Based on the universal equilibrium  and flocculation zones and are designed to cause
                   theory, the Kolmogorov’s microscales of length,    contact between newly formed floc and settled
                   time, and velocity are defined as the smallest scales  solids.
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