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308 Chapter 6 ■ Differential Analysis of Fluid Flow<br />

1z direction2<br />

The Navier–Stokes<br />

equations are the<br />

basic differential<br />

equations describing<br />

the flow of<br />

Newtonian <strong>fluid</strong>s.<br />

z<br />

(6.127c)<br />

where u, v, and w are the x, y, and z components of velocity as shown in the figure in the margin<br />

of the previous page. We have rearranged the equations so the acceleration terms are on the left<br />

side and the force terms are on the right. These equations are commonly called the Navier–Stokes<br />

equations, named in honor of the French mathematician L. M. H. Navier 11785–18362 and the<br />

English mechanician Sir G. G. Stokes 11819–19032, who were responsible for their formulation.<br />

These three equations of motion, when combined with the conservation of mass equation 1Eq. 6.312,<br />

provide a complete mathematical description of the flow of incompressible Newtonian <strong>fluid</strong>s. We<br />

have four equations and four unknowns 1u, v, w, and and therefore the problem is “well-posed”<br />

in mathematical terms. Unfortunately, because of the general complexity of the Navier–Stokes<br />

equations 1they are nonlinear, second-order, partial differential equations2, they are not amenable<br />

to exact mathematical solutions except in a few instances. However, in those few instances in which<br />

solutions have been obtained and compared with experimental results, the results have been in close<br />

agreement. Thus, the Navier–Stokes equations are considered to be the governing differential<br />

equations of motion for incompressible Newtonian <strong>fluid</strong>s.<br />

In terms of cylindrical polar coordinates 1see the figure in the margin2, the Navier–Stokes<br />

equations can be written as<br />

1r direction2<br />

r a 0v r<br />

0t<br />

1u<br />

direction2<br />

r a 0w<br />

0t u 0w<br />

0x v 0w<br />

0y w 0w<br />

0z b 0p 0z rg z m a 02 w<br />

0x 2 02 w<br />

0y 2 02 w<br />

0z 2 b<br />

p2,<br />

v 0v r<br />

r<br />

0r v u 0v r<br />

r 0u v2 u<br />

r v 0v r<br />

z<br />

0z b<br />

0p<br />

0r rg r m c 1 0<br />

r 0r ar 0v r<br />

0r b v r<br />

r 1 0 2 v r<br />

2 r 2 0u 2 0v u<br />

2 r 2 0u 02 v r<br />

0z d 2<br />

(6.128a)<br />

x<br />

θ<br />

r<br />

v z<br />

vθ<br />

v r<br />

y<br />

r a 0v u<br />

0t<br />

v 0v u<br />

r<br />

0r v u 0v u<br />

r 0u v rv u<br />

v 0v u<br />

r z<br />

0z b<br />

1 0p<br />

r 0u rg u m c 1 0<br />

r 0r ar 0v u<br />

0r b v u<br />

r 1 0 2 v u<br />

2 r 2 0u 2 0v r<br />

2 r 2 0u 02 v u<br />

0z d 2<br />

(6.128b)<br />

1z direction2<br />

r a 0v z<br />

0t<br />

v 0v z<br />

r<br />

0r v u 0v z<br />

r 0u v 0v z<br />

z<br />

0z b<br />

<br />

0p<br />

0z rg z m c 1 0<br />

r 0r ar 0v z<br />

0r b 1 0 2 v z<br />

r 2 0u 2<br />

02 v z<br />

0z 2 d<br />

(6.128c)<br />

To provide a brief introduction to the use of the Navier–Stokes equations, a few of the<br />

simplest exact solutions are developed in the next section. Although these solutions will prove to<br />

be relatively simple, this is not the case in general. In fact, only a few other exact solutions have<br />

been obtained.<br />

6.9 Some Simple Solutions for Laminar, Viscous, Incompressible Fluids<br />

A principal difficulty in solving the Navier–Stokes equations is because of their nonlinearity arising<br />

from the convective acceleration terms 1i.e., u 0u0x, w 0v0z, etc.2. There are no general analytical<br />

schemes for solving nonlinear partial differential equations 1e.g., superposition of solutions cannot<br />

be used2, and each problem must be considered individually. For most practical flow problems, <strong>fluid</strong><br />

particles do have accelerated motion as they move from one location to another in the flow field.<br />

Thus, the convective acceleration terms are usually important. However, there are a few special cases<br />

for which the convective acceleration vanishes because of the nature of the geometry of the flow

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