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These are the Lecture Slides of Transport Process which includes Dimensional Analysis, System Variables, Empirical Relationship, Variables in System, Dimensionless Groups, Dimensional Equation, Linear Equations, Derived Groups etc.Key important points are: Flow Around Immersed Objects, Incompressible Flow, Stokes’ and Newton’s Laws, Drag Coefficient, Flow Around Objects, External Pressure Gradient, Dynamic Forces, Projected Area, Spherical Particle
Typology: Slides
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Dynamic
Fk results from the relative motion of the object and the fluid (shear stress)
Static
Fs results from external pressure gradient (Fp) and gravity (Fg).
A drag force (friction) arises in situations in which moving fluids are in contact with a solid surface (recall pipe flow.
Fw is the kinetic force exerted on the solid wall or particle, A is the wetted surface area, K is the kinetic energy per unit volume, and f is the friction factor.
V 2 2
w
The projected area used in the Fk is the area “seen” by the fluid.
A 4
2 D R
For objects having shapes other than spherical, it is necessary to specify the size, geometry and orientation relative to the direction of flow.
Axis perpendicular to flow Rectangle A LD
Axis parallel to flow Circle
For slow flow around a sphere and Re<
0
24 24
Re Du
Cd
2
2 F Cd A u^0 k
Fk 3 Du 0
As the flow rate increases wake drag becomes an important factor. The streamline pattern becomes mixed at the rear of the particle and at very high Reynolds numbers completely separate in the wake. This causes a greater pressure at the front of the particle and thus an extra force term due to pressure difference.
The gravity and buoyancy forces on an object immersed in liquids do not generally balance each other and the object will be in motion.
Ft Fk Fg Fb
Fb
Fg
It is always opposite to the direction of particle motion
When a particle whose density is greater than that of the fluid begins to fall in response to the force imbalance, it begins to accelerate (F=ma). As the velocity increases the viscous drag force also increases until all forces are in balance. At this point the particle reaches terminal velocity.
t
2
The settling (terminal) velocity of small particles is often low enough that the Reynolds number is less than unity (Cd = 24/Re).
2
p p f t
Re ^1
Between 1000<Re<200,000 Cd = 0.44 Newton’s Law applies
f
p p f t
gD u
1. 75 Fk ^ Dput^ f
2 2
Note: Intermediate flow requires iteration
Reynolds number is a poor criteria for determining the proper regime for settling. We can derive a value K that depends solely on the physical parameters
13
2
(^) f p f p
g K D
2
2 F Cd A u^0 k
6 3
3 (^0 1). 192 10
005 10
2 1. 2 1
kg m s
u D kg m m s m Re
Fig. 7.3 gives Cd ≈ 0.
Projected Area = DL = 10 m^2
N
2
2 2 3
Estimate the terminal velocity of limestone particles (Dp = 0.15 mm, = 2800 kg/m^3 ) in water @ 20°C.