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James Stewart-Calculus_ Early Transcendentals-Cengage Learning (2015)

A five star textbook for college calculus

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section 16.8 Stokes’ Theorem 1137

the disk x 2 1 y 2 < 1 and so using Equation 16.7.10 with z − tsx, yd − 2 2 y, we have

y F dr −

C

yy curl F dS − y

S

D

y s1 1 2yd dA

− y 2

0

y 1

0

s1 1 2r sin d r dr d

2

− y F r 2

0 2 1 2 r 3 1

3 sin d − y 2

( 1 2

0

G0

1 2 3 sin ) d

− 1 2 s2d 1 0 − ■

z

0

S

C

≈+¥+z@=4

ExamplE 2 Use Stokes’ Theorem to compute the integral yy S

curl F dS, where

Fsx, y, zd − xz i 1 yz j 1 xy k and S is the part of the sphere x 2 1 y 2 1 z 2 − 4 that

lies inside the cylinder x 2 1 y 2 − 1 and above the xy-plane. (See Figure 4.)

SOLUTIon To find the boundary curve C we solve the equations x 2 1 y 2 1 z 2 − 4 and

x 2 1 y 2 − 1. Subtracting, we get z 2 − 3 and so z − s3 (since z . 0). Thus C is the

circle given by the equations x 2 1 y 2 − 1, z − s3 . A vector equation of C is

x

y

≈+¥=1

rstd − cos t i 1 sin t j 1 s3 k

0 < t < 2

FIGURE 4

so

r9std − 2sin t i 1 cos t j

Also, we have

Fsrstdd − s3 cos t i 1 s3 sin t j 1 cos t sin t k

Therefore, by Stokes’ Theorem,

yy curl F dS − y F dr −

C

y 2

Fsrstdd r9std dt

0

S

− y 2

(2s3 cos t sin t 1 s3 sin t cos t) dt

0

− s3 y 2

0 dt − 0 ■

0

Note that in Example 2 we computed a surface integral simply by knowing the values

of F on the boundary curve C. This means that if we have another oriented surface with

the same boundary curve C, then we get exactly the same value for the surface integral!

In general, if S 1 and S 2 are oriented surfaces with the same oriented boundary curve C

and both satisfy the hypotheses of Stokes’ Theorem, then

3 y

S 1

y curl F dS − y C

F dr − y

S 2

y curl F dS

This fact is useful when it is difficult to integrate over one surface but easy to integrate

over the other.

We now use Stokes’ Theorem to throw some light on the meaning of the curl vector.

Suppose that C is an oriented closed curve and v represents the velocity field in fluid

flow. Consider the line integral

y C

v dr − y C

v T ds

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