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Settling of suspended particles

In order to quantify the sedimentation of suspended particles, the ratio R of sedimentation layer volume (V ) to total suspension volume (Vq) [Pg.567]


The rate of settling of suspended particles in a gas stream may be greatly increased if centrifugal rather than gravitational forces are employed. In the cyclone separator shown... [Pg.72]

In natural systems there are two types of transport phenomena (1) transport by random motion, and (2) transport by directed motion. Both types occur at a wide range of scales from molecular to global distances, from microseconds to geological times. Well-known examples of these types are molecular diffusion (random transport) and advection in water currents (directed transport). There are many other manifestations such as dispersion as a random process (see Chapters 24 and 25) or settling of suspended particles due to gravitation as a directed transport. For simplicity we will subdivide such transport processes into those we will call diffusive for ones caused by random motions and those called advective for ones resulting from directed motions. [Pg.779]

Most processes listed in Box 23.1 have been discussed before. However, the term describing the settling of suspended particles, k Ct, and the exchange between the water and the sediments, sedex [C qd - Ct ], need further explanation. A detailed discussion follows in Section 23.2. First, we discuss the fate of vinyl acetate in a pond (Illustrative Example 23.1) for which the solute-particle interaction is not important. [Pg.1054]

Figure 23.3 The processes which contribute to the exchange flux between open water (op) and sediment column (sc) (a) settling of suspended particles (b) exchange flux of dissolved phase across a stagnant bottom boundary layer, (c) particle resuspension followed by equilibration between particle and open water. Figure 23.3 The processes which contribute to the exchange flux between open water (op) and sediment column (sc) (a) settling of suspended particles (b) exchange flux of dissolved phase across a stagnant bottom boundary layer, (c) particle resuspension followed by equilibration between particle and open water.
The process of sedimentation in which the settling of suspended particles results in a dense compaction, or coagulation, of particles in which liquid is squeezed out. Geologically, significant compaction of clay layers caused by lowering of the water table (dewatering). [Pg.395]

Sedimentation The settling of suspended particles or droplets due to gravity or an applied centrifugal field. Negative sedimentation, when droplets rise upwards, is also called flotation and is a part of the creaming process. [Pg.401]

Sedimentation The settling of suspended particles or droplets due to gravity or an applied centrifugal field. The sedimentation rate (or velocity) divided by acceleration is termed the sedimentation coefficient. The sedimentation coefficient extrapolated to zero concentration of sedimenting species is termed the limiting sedimentation coefficient. The sedimentation coefficient reduced to standard temperature and solvent is termed the reduced sedimentation coefficient. If the sedimentation coefficient is... [Pg.516]

The process of sedimentation involves the separation from water, by gravitational settling of suspended particles that are heavier than water. The resulting effluent is then subject to rapid filtration to separate out solids that are still suspended in the water. Rapid filters typically consist of 24 - 36 inches of 0.5- to 1-mm-diameter sand and/or anthracite. Particles are removed as water is filtered through the media at rates... [Pg.144]

Adsorption affects the electrostatic properties of suspended particles and colloids, which, in turn, influences their tendency to aggregate and attach (coagulation, settling, filtration). [Pg.4]

A colloidal solution is defined as a solution intermediate in character between a suspension and a true solution. Particles with diameters < 10 pm are usually called colloids [19,65], although the distinction based on size is arbitrary. The size of particles is a continuum and the point at which large macromolecules end and small colloids begin is subject to judgment, as is the upper end of the size continuum, where colloids and suspended particles merge. The tendency of suspended particles to settle out of solution is not really a function of size alone, rather the relative density of the particles and the motion of the water will determine what is suspended and what settles. [Pg.126]

A reactive contaminant may be adsorbed on the soil surface prior to rainfall then, following rainfall that canses erosion, the soil is transported by rnnoff water in the form of suspended particles redistribnted on the land snrface. In general, the settling velocity distribntion dnring runoff indicates that the finer particles are resettled initially (Proffit et al. 1991), although the details of the settling process are affected by different environmental factors, such as soil type and rainfall rate. [Pg.244]

The vertical mass fluxes caused by the settling of suspended matter (process 5 in Fig. 21.10) are relevant whenever the chemical i is either incorporated in the suspended particles or sorbed to their surface. A thorough discussion on particle settling will follow in Chapter 23. At this point we just note that the total flux per unit time leaving the epilimnion can be written as ... [Pg.985]

Yet, in view of the often strong currents in rivers, it would be difficult to interpret ks as a vertical settling velocity divided by the mean depth of the river bed as done in Eq. 23-16. In fact, ks should be understood as an empirical coefficient describing the specific first-order removal rate of suspended particles from the river. [Pg.1116]

Clarification Also called sedimentation (Spellman, 2003), 476. In water treatment, the removal of suspended particles from water through settling, flotation, and/or filtration. [Pg.443]

Lerman A. L. D. and Dacey M.F. (1974) Stoke s settling and chemical reactivity of suspended particles in natural waters. In Suspended Solids in Water (ed. R.J. Gibbs), pp. 17-47. Plenum Press, New York. [Pg.643]

Lerman A. L. and Dacey M. F. (1974) Stokes settling and chemical reactivity of suspended particles in natural waters. [Pg.3550]

SLS system design and scale up are frequently dependent on settling velocity of suspended particles, flow rate, specific cake resisfance, cake % solids, medinm resistance, clarity of filtrate, or overflow, which are obtained from tests. In-plant testing is snggested. If replacement equipment is to be considered for processes in operation, in-plant testing shonld be performed and if a new product is involved, pilot-plant and bench-scale tests of separability should be conducted so that the maximum design information is available. [Pg.1663]


See other pages where Settling of suspended particles is mentioned: [Pg.84]    [Pg.249]    [Pg.335]    [Pg.392]    [Pg.760]    [Pg.154]    [Pg.129]    [Pg.567]    [Pg.335]    [Pg.84]    [Pg.249]    [Pg.335]    [Pg.392]    [Pg.760]    [Pg.154]    [Pg.129]    [Pg.567]    [Pg.335]    [Pg.354]    [Pg.7]    [Pg.916]    [Pg.426]    [Pg.118]    [Pg.347]    [Pg.1087]    [Pg.384]    [Pg.110]    [Pg.149]    [Pg.384]    [Pg.389]    [Pg.468]    [Pg.264]    [Pg.2386]    [Pg.821]    [Pg.2001]    [Pg.874]    [Pg.66]    [Pg.110]    [Pg.58]   


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