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9.3 Drag 499<br />

TABLE 9.4<br />

Low Reynolds Number Drag Coefficients (Ref. 7) ( Re RUDM, A PD 2 4)<br />

C D d<br />

( RU 2 A2)<br />

Object ( for Re f 1) Object<br />

a. Circular disk normal 20.4Re<br />

c. Sphere<br />

to flow<br />

C D<br />

24.0Re<br />

U<br />

D<br />

U<br />

D<br />

b. Circular disk parallel 13.6Re<br />

d. Hemisphere<br />

to flow<br />

22.2Re<br />

U<br />

U<br />

D<br />

D<br />

For very small<br />

Reynolds number<br />

flows, the drag coefficient<br />

varies inversely<br />

with the<br />

Reynolds number.<br />

where Re rU/m. The use of the dynamic pressure, rU 2 2, in the definition of the drag coefficient<br />

is somewhat misleading in the case of creeping flows 1Re 6 12 because it introduces the<br />

<strong>fluid</strong> density, which is not an important parameter for such flows 1inertia is not important2. Use of<br />

this standard drag coefficient definition gives the 1Re dependence for small Re drag coefficients.<br />

Typical values of C D for low Reynolds number flows past a variety of objects are given in<br />

Table 9.4. It is of interest that the drag on a disk normal to the flow is only 1.5 times greater than<br />

that on a disk parallel to the flow. For large Reynolds number flows this ratio is considerably larger<br />

1see Example 9.12. Streamlining 1i.e., making the body slender2 can produce a considerable drag<br />

reduction for large Reynolds number flows; for very small Reynolds number flows it can actually<br />

increase the drag because of an increase in the area on which shear forces act. For most objects,<br />

the low Reynolds number flow results are valid up to a Reynolds number of about 1.<br />

E XAMPLE 9.10<br />

Low Reynolds Number Flow Drag<br />

GIVEN A small grain of sand, diameter D 0.10 mm and<br />

specific gravity SG 2.3, settles to the bottom of a lake after<br />

having been stirred up by a passing boat.<br />

FIND<br />

Determine how fast it falls through the still water.<br />

SOLUTION<br />

A free-body diagram of the particle 1relative to the moving particle2<br />

is shown in Fig. E9.10a. The particle moves downward with a constant<br />

velocity U that is governed by a balance between the weight<br />

of the particle, w, the buoyancy force of the surrounding water, F B ,<br />

and the drag of the water on the particle, d.<br />

F B<br />

From the free-body diagram, we obtain<br />

w d F B<br />

where<br />

w g sand V SG g p H2 O<br />

6 D3<br />

and<br />

F B g H2 O V g p H2 O<br />

6 D3<br />

(1)<br />

(2)<br />

<br />

<br />

U<br />

F I G U R E E9.10a<br />

We assume 1because of the smallness of the object2 that the<br />

flow will be creeping flow 1Re 6 12 with C D 24 Re 1see Table<br />

9.42 so that<br />

d 1 2 r H 2 OU 2 p 4 D2 C D 1 2 r H 2 OU 2 p 24<br />

4 D2 a<br />

b<br />

r H2 OUDm H2 O

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