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Hydraulic gradient horizontal flow

Figure 25.3 The hydraulic gradient, defined as the slope of the (unconfined) groundwater table, Swl = A/i /Ax, is a measure for the horizontal pressure gradient that drives the flow through a porous medium from high to low pressure. Figure 25.3 The hydraulic gradient, defined as the slope of the (unconfined) groundwater table, Swl = A/i /Ax, is a measure for the horizontal pressure gradient that drives the flow through a porous medium from high to low pressure.
Consider now conditions at the valve as affected by both pipe friction and damping. When the pressure wave from N has reached a midpoint B in the pipe length L, the water in BN will be at rest and for zero flow the hydraulic gradient should be a horizontal line. There is thus a tendency for the gradient to flatten out for the portion BN. Hence, instead of the transient gradient having the slope imposed by friction, it will approach a horizontal line starting from the transient value at B. Thus... [Pg.504]

An extended investigation was done to determine relationships between two main hydrodynamic characteristics of capsule flow - capsule/liquid velocity ratio, Vc/ v< hydraulic gradient, ic, and parameters of capsule-liquid-pipe system, e.g. pipe diameter, D, capsule/pipe diameter ratio, d/D, capsule length/diameter ratio, l/d, capsule/carrier liquid density ratio. Pc Ipo, capsule shape, B, concentration of solids, Cv, liquid viscosity, po and liquid mean velocity, v<,. However, majority of the research was focussed on straight horizontal pipe. The knowledge about behaviour of capsules in bend or inclined pipe sections has been up to now insufficient. [Pg.521]

Regarding flow conditions, typical appUcaiions of unidirectional steady-flow conditions are earth dams, embankments, retaining walls, landfills, drainage trenches, and vertical and horizontal drains. The range of boundary conditions, in terms of vertical effective stress and applied hydraulic gradients, for these applications is shown in Table 8.3. [Pg.173]

Figure 8 shows a snapshot of hydraulic heads at 19 ka, for the permafrost distribution at the same time shown in figure 7. The main flow is horizontal, being driven to the left by the leftward pressure gradient generated by the ice load shown in figure 4. Head gradients increase leftwards... [Pg.297]

HYDRAULIC FRICTION GRADIENT OF HORIZONTAL HETEROGENEOUS FLOWS... [Pg.180]

Considerations of distributions across the flow channel, transverse to the primary flow direction, were first included in basically one-dimensional models by approximating the temperature distribution in the fluid parallel to the flow direction. Recently there is an increasing application of CFD to various single- and two-phase thermal-hydraulic analyses, including NCLs and supercritical fluid states, in nuclear power systems. These approaches also allow for resolution of the thermal stratification in horizontal and vertical sections of the loop as well as resolution of gradients normal to the primary flow direction and the consequent effects on calculated stability. Fully three-dimensional analyses are becoming the norm, but only for simple idealized single-phase cases. [Pg.496]


See other pages where Hydraulic gradient horizontal flow is mentioned: [Pg.601]    [Pg.210]    [Pg.223]    [Pg.1035]    [Pg.1153]    [Pg.71]    [Pg.410]    [Pg.472]    [Pg.77]    [Pg.210]    [Pg.223]    [Pg.69]    [Pg.314]    [Pg.379]    [Pg.526]    [Pg.528]    [Pg.195]    [Pg.62]    [Pg.37]    [Pg.492]    [Pg.674]    [Pg.273]    [Pg.195]    [Pg.144]    [Pg.197]    [Pg.200]    [Pg.101]    [Pg.365]    [Pg.247]   
See also in sourсe #XX -- [ Pg.195 , Pg.199 ]




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