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Solid-phase velocity

Figure 9 (a) Three-dimensional view of 3D solid concentration with a horizontal gas jet in the fluidized bed (b) 3D voxel-volume-averaged solid phase velocity vector map in the Y-Z plane of the fluidized bed (c) 3D voxel-volume-averaged solid phase vector map (Wang et al., 2008) (see Plate 12 in Color Plate Section at the end of this book). [Pg.195]

Dimensionless concentration of A in the fluid phase Dimensionless concentration of A at the isotherm inflection point Solid phase velocity... [Pg.296]

The condition for complete separation given in Eq. 17.16 is clearly illustrated in Figure 17.3. The switching time, t, (or, alternately, the solid phase velocity) must be selected in such a way that the first component front passes the raffinate node but that the second component front does not reach it. This latter condition is equivalent to j6 > 1. When = 1, the extract reaches just the raffinate node at time t. This is the limit situation. We can see from Eq. 17.19 that, in this case, Lq is equal to 0. [Pg.792]

In these equations is the density of fluid (water), p - density of solid phase, - fluid velocity in transport pores, - fluid velocity between clay particles, V, - solid phase velocity. [Pg.445]

Figure 4.19 Time-averaged particle movement and time-averaged lateral profile of the axial solids phase velocity for different heights in the fluidized bed with (A) 40% gas extraction, (B) 20% gas extraction, (C) the reference series with no gas addition/extraction, (D) 20% gas addition, and (E) 40% gas addition, in all experiments, the background fluidization veiocity was kept constant (uo = 100%). Reprinted from DeJong et al. (2011) with permission from Elsevier. Figure 4.19 Time-averaged particle movement and time-averaged lateral profile of the axial solids phase velocity for different heights in the fluidized bed with (A) 40% gas extraction, (B) 20% gas extraction, (C) the reference series with no gas addition/extraction, (D) 20% gas addition, and (E) 40% gas addition, in all experiments, the background fluidization veiocity was kept constant (uo = 100%). Reprinted from DeJong et al. (2011) with permission from Elsevier.
Note that since there are only two phases, i = (l- 2). Consider steady state the terms on the left-hand side disappear. We now employ the linear driving force assumption (7.1.5b) along with linear equilibrium relation (7.1.18a), C,i/Ca=Ka and the relation v z - z/t) relating the solid-phase velocity to time and axial coordinates ... [Pg.759]


See other pages where Solid-phase velocity is mentioned: [Pg.1509]    [Pg.29]    [Pg.18]    [Pg.295]    [Pg.196]    [Pg.1331]    [Pg.1813]    [Pg.786]    [Pg.786]    [Pg.229]    [Pg.1805]    [Pg.1513]    [Pg.198]    [Pg.205]    [Pg.207]    [Pg.744]    [Pg.747]    [Pg.631]   
See also in sourсe #XX -- [ Pg.198 ]




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Solids velocity

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