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

A five star textbook for college calculus

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section 16.7 Surface Integrals 1129

If we write F − v, then F is also a vector field on R 3 and the integral in Equation 7

becomes

yy F n dS

S

A surface integral of this form occurs frequently in physics, even when F is not v, and

is called the surface integral (or flux integral) of F over S.

8 Definition If F is a continuous vector field defined on an oriented surface S

with unit normal vector n, then the surface integral of F over S is

y

S

y F dS − y

S

y F n dS

This integral is also called the flux of F across S.

In words, Definition 8 says that the surface integral of a vector field over S is equal to

the surface integral of its normal component over S (as previously defined).

If S is given by a vector function rsu, vd, then n is given by Equation 6, and from Definition

8 and Equation 2 we have

y

S

y F dS − y

S

y F

r u 3 r v

| r u 3 r v | dS

− y

Dy FFsrsu, vdd

where D is the parameter domain. Thus we have

r u 3 r v

| r u 3 r v |G| r u 3 r v | dA

Compare Equation 9 to the similar

expression for evaluating line integrals

of vector fields in Definition 16.2.13:

y C

F dr − y b

a

Fsrstdd r9std dt

9

y

S

y F dS − y

D

y F sr u 3 r v d dA

Figure 11 shows the vector field F in

Example 4 at points on the unit sphere.

z

ExamplE 4 Find the flux of the vector field Fsx, y, zd − z i 1 y j 1 x k across the unit

sphere x 2 1 y 2 1 z 2 − 1.

SOLUTIon As in Example 1, we use the parametric representation

rs, d − sin cos i 1 sin sin j 1 cos k 0 < < 0 < < 2

Then

Fsrs, dd − cos i 1 sin sin j 1 sin cos k

and, from Example 16.6.10,

x

y

Therefore

r 3 r − sin 2 cos i 1 sin 2 sin j 1 sin cos k

FIGURE 11

Fsrs, dd sr 3 r d − cos sin 2 cos 1 sin 3 sin 2 1 sin 2 cos cos

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