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The net pressure<br />

force on a particle<br />

is determined by the<br />

pressure gradient.<br />

3.2 F ma along a Streamline 97<br />

Thus, if dF ps is the net pressure force on the particle in the streamline direction, it follows that<br />

dF ps 1p dp s 2 dn dy 1p dp s 2 dn dy 2 dp s dn dy<br />

0p ds dn dy 0p<br />

0s 0s dV<br />

Note that the actual level of the pressure, p, is not important. What produces a net pressure<br />

force is the fact that the pressure is not constant throughout the <strong>fluid</strong>. The nonzero pressure gradient,<br />

§p 0p0s ŝ 0p0n nˆ , is what provides a net pressure force on the particle. Viscous forces,<br />

represented by t ds dy, are zero, since the <strong>fluid</strong> is inviscid.<br />

Thus, the net force acting in the streamline direction on the particle shown in Fig. 3.3 is given by<br />

a dF s dw s dF ps ag sin u 0p<br />

0s b dV<br />

By combining Eqs. 3.2 and 3.3, we obtain the following equation of motion along the streamline<br />

direction:<br />

g sin u 0p 0V<br />

rV (3.4)<br />

0s 0s ra s<br />

We have divided out the common particle volume factor, dV, that appears in both the force and<br />

the acceleration portions of the equation. This is a representation of the fact that it is the <strong>fluid</strong> density<br />

1mass per unit volume2, not the mass, per se, of the <strong>fluid</strong> particle that is important.<br />

The physical interpretation of Eq. 3.4 is that a change in <strong>fluid</strong> particle speed is accomplished<br />

by the appropriate combination of pressure gradient and particle weight along the streamline. For<br />

<strong>fluid</strong> static situations this balance between pressure and gravity forces is such that no change in<br />

particle speed is produced—the right-hand side of Eq. 3.4 is zero, and the particle remains stationary.<br />

In a flowing <strong>fluid</strong> the pressure and weight forces do not necessarily balance—the force<br />

unbalance provides the appropriate acceleration and, hence, particle motion.<br />

(3.3)<br />

E XAMPLE 3.1<br />

Pressure Variation along a Streamline<br />

GIVEN Consider the inviscid, incompressible, steady flow<br />

along the horizontal streamline A–B in front of the sphere of radius<br />

a, as shown in Fig. E3.1a. From a more advanced theory of<br />

flow past a sphere, the <strong>fluid</strong> velocity along this streamline is<br />

FIND Determine the pressure variation along the streamline<br />

from point A far in front of the sphere 1x A and V A V 0 2 to<br />

point B on the sphere 1x B a and V B 02.<br />

as shown in Fig. E3.1b.<br />

V V 0 a1 a3<br />

x 3b<br />

z<br />

1 V o<br />

0.75 V o<br />

V<br />

0.5 V o<br />

V A = V ˆ O i<br />

V = Vi ˆ V B = 0<br />

A<br />

B<br />

a<br />

x<br />

0.25 V o<br />

(a)<br />

–3a –2a –1a 0<br />

x<br />

(b)<br />

∂p __<br />

∂x<br />

0.610 ρV 2 0<br />

/a<br />

p<br />

2<br />

0.5 ρV 0<br />

–3a –2a –a 0 x<br />

(c)<br />

–3a –2a –a 0<br />

x<br />

(d)<br />

F I G U R E E3.1

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