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Page 1: MULTIPLE INTEGRALS 16. 2 MULTIPLE INTEGRALS 16.9 Change of Variables in Multiple Integrals In this section, we will learn about: The change of variables

MULTIPLE INTEGRALSMULTIPLE INTEGRALS

16

Page 2: MULTIPLE INTEGRALS 16. 2 MULTIPLE INTEGRALS 16.9 Change of Variables in Multiple Integrals In this section, we will learn about: The change of variables

2

MULTIPLE INTEGRALS

16.9Change of Variables

in Multiple Integrals

In this section, we will learn about:

The change of variables

in double and triple integrals.

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3

CHANGE OF VARIABLES IN SINGLE INTEGRALS

In one-dimensional calculus. we often

use a change of variable (a substitution)

to simplify an integral.

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4

By reversing the roles of x and u, we can

write the Substitution Rule (Equation 6 in

Section 5.5) as:

where x = g(u) and a = g(c), b = g(d).

SINGLE INTEGRALS

( ) ( ( )) '( )b d

a cf x dx f g u g u du

Formula 1

Page 5: MULTIPLE INTEGRALS 16. 2 MULTIPLE INTEGRALS 16.9 Change of Variables in Multiple Integrals In this section, we will learn about: The change of variables

5

Another way of writing Formula 1 is

as follows:

SINGLE INTEGRALS

( ) ( ( ))b d

a c

dxf x dx f x u du

du

Formula 2

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6

A change of variables can also be useful

in double integrals.

We have already seen one example of this: conversion to polar coordinates.

CHANGE OF VARIABLES IN DOUBLE INTEGRALS

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7

The new variables r and θ are related to

the old variables x and y by:

x = r cos θ

y = r sin θ

DOUBLE INTEGRALS

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8

The change of variables formula (Formula 2

in Section 16.4) can be written as:

where S is the region in the rθ-plane that

corresponds to the region R in the xy-plane.

DOUBLE INTEGRALS

( , ) ( cos , sin )R S

f x y dA f r r r dr d

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9

More generally, we consider a change of

variables that is given by a transformation T

from the uv-plane to the xy-plane:

T(u, v) = (x, y)

where x and y are related to u and v by:

x = g(u, v) y = h(u, v)

We sometimes write these as: x = x(u, v), y = y(u, v)

TRANSFORMATION Equations 3

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10

We usually assume that T is a C1

transformation.

This means that g and h have continuous first-order partial derivatives.

C1 TRANSFORMATION

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11

A transformation T is really just

a function whose domain and range

are both subsets of .

TRANSFORMATION

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12

If T(u1, v1) = (x1, y1), then the point (x1, y1)

is called the image of the point (u1, v1).

If no two points have the same image,

T is called one-to-one.

IMAGE & ONE-TO-ONE TRANSFORMATION

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13

The figure shows the effect of a transformation

T on a region S in the uv-plane. T transforms S into a region R in the xy-plane

called the image of S, consisting of the images of all points in S.

CHANGE OF VARIABLES

Fig. 16.9.1, p. 1049

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14

If T is a one-to-one transformation, it

has an inverse transformation T–1 from

the xy–plane to the uv-plane.

INVERSE TRANSFORMATION

Fig. 16.9.1, p. 1049

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15

Then, it may be possible to solve Equations 3

for u and v in terms of x and y :

u = G(x, y)

v = H(x, y)

INVERSE TRANSFORMATION

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16

A transformation is defined by:

x = u2 – v2

y = 2uv

Find the image of the square

S = {(u, v) | 0 ≤ u ≤ 1, 0 ≤ v ≤ 1}

TRANSFORMATION Example 1

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17

The transformation maps the boundary

of S into the boundary of the image.

So, we begin by finding the images of the sides of S.

TRANSFORMATION Example 1

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18

The first side, S1, is given by:

v = 0 (0 ≤ u ≤ 1)

TRANSFORMATION Example 1

Fig. 16.9.2, p. 1050

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19

From the given equations,

we have:

x = u2, y = 0, and so 0 ≤ x ≤ 1.

Thus, S1 is mapped into the line segment from (0, 0) to (1, 0) in the xy-plane.

TRANSFORMATION Example 1

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20

The second side, S2, is:

u = 1 (0 ≤ v ≤ 1)

Putting u = 1 in the given equations, we get:

x = 1 – v2

y = 2v

TRANSFORMATION E. g. 1—Equation 4

Fig. 16.9.2, p. 1050

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21

Eliminating v, we obtain:

which is part of a parabola.

TRANSFORMATION

2

1 0 14

yx x

E. g. 1—Equation 4

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22

Similarly, S3 is given by:

v = 1 (0 ≤ u ≤ 1)

Its image is

the parabolic arc

TRANSFORMATION

2

14

( 1 0)

yx

x

E. g. 1—Equation 5

Fig. 16.9.2, p. 1050

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23

Finally, S4 is given by:

u = 0(0 ≤ v ≤ 1)

Its image is:

x = –v2, y = 0

that is,

–1 ≤ x ≤ 0

TRANSFORMATION Example 1

Fig. 16.9.2, p. 1050

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24

Notice that as, we move around the square

in the counterclockwise direction, we also

move around the parabolic region in

the counterclockwise

direction.

TRANSFORMATION Example 1

Fig. 16.9.2, p. 1050

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25

The image of S is

the region R bounded

by: The x-axis.

The parabolas given by Equations 4 and 5.

TRANSFORMATION Example 1

Fig. 16.9.2, p. 1050

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26

Now, let’s see how a change

of variables affects a double

integral.

DOUBLE INTEGRALS

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27

We start with a small rectangle S in

the uv-plane whose:

Lower left corner is the point (u0, v0).

Dimensions are ∆u and ∆v.

DOUBLE INTEGRALS

Fig. 16.9.3, p. 1050

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28

The image of S is a region R in the xy-plane,

one of whose boundary points is:

(x0, y0) = T(u0, v0)

DOUBLE INTEGRALS

Fig. 16.9.3, p. 1050

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29

The vector

r(u, v) = g(u, v) i + h(u, v) j

is the position vector of the image of

the point (u, v).

DOUBLE INTEGRALS

Fig. 16.9.3, p. 1050

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30

The equation of the lower side of S is:

v = v0

Its image curve is given by the vector function r(u, v0).

DOUBLE INTEGRALS

Fig. 16.9.3, p. 1050

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31

The tangent vector at (x0, y0) to this image

curve is:

DOUBLE INTEGRALS

0 0 0 0( , ) ( , )u u u

x yg u v h u v

u u

r i j i j

Fig. 16.9.3, p. 1050

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32

Similarly, the tangent vector at (x0, y0) to

the image curve of the left side of S (u = u0)

is:

DOUBLE INTEGRALS

0 0 0 0( , ) ( , )v v v

x yg u v h u v

v v

r i j i j

Fig. 16.9.3, p. 1050

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33

We can approximate the image region

R = T(S) by a parallelogram determined by

the secant vectors

DOUBLE INTEGRALS

0 0

0 0

0 0

0 0

( , )

( , )

( , )

( , )

u u v

u v

u v v

u v

a r

r

b r

r

Fig. 16.9.4, p. 1051

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34

However,

So,

Similarly,

DOUBLE INTEGRALS

0 0 0 0

0

( , ) ( , )limu u

u u v u v

u

r r

r

0 0 0 0( , ) ( , ) uu u v u v u r r r

0 0 0 0( , ) ( , ) vu v v u v v r r r

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35

This means that we can approximate R by

a parallelogram determined by the vectors

∆u ru and ∆v rv

DOUBLE INTEGRALS

Fig. 16.9.5, p. 1051

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36

Thus, we can approximate the area of R

by the area of this parallelogram, which,

from Section 13.4, is:

|(∆u ru) x (∆v rv)| = |ru x rv| ∆u ∆v

DOUBLE INTEGRALS Equation 6

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37

Computing the cross product,

we obtain:

DOUBLE INTEGRALS

0

0

u v

x y x xx y u u u v

x y y yu ux y v u u vv u

i j k

r r k k

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38

The determinant that arises in this

calculation is called the Jacobian of

the transformation.

It is given a special notation.

JACOBIAN

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39

The Jacobian of the transformation T

given by x = g(u, v) and y = h(u, v) is:

JACOBIAN OF T Definition 7

( , )

( , )

x xx y x y x yu v

y yu v u v v u

u v

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40

With this notation, we can use Equation 6

to give an approximation to the area

∆A of R:

where the Jacobian

is evaluated at (u0, v0).

JACOBIAN OF T

( , )

( , )

x yA u v

u v

Approximation 8

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41

The Jacobian is named after the German

mathematician Carl Gustav Jacob Jacobi

(1804–1851).

The French mathematician Cauchy first used these special determinants involving partial derivatives.

Jacobi, though, developed them into a method for evaluating multiple integrals.

JACOBIAN

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42

Next, we divide a region S in the uv-plane

into rectangles Sij and call their images in

the xy-plane Rij.

DOUBLE INTEGRALS

Fig. 16.9.6, p. 1052

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43

Applying Approximation 8 to each Rij , we

approximate the double integral of f over R

as follows.

DOUBLE INTEGRALS

Fig. 16.9.6, p. 1052

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44

where the Jacobian is evaluated at (ui, vj).

DOUBLE INTEGRALS

1 1

1 1

( , )

( , )

( , )( ( , ), ( , ))

( , )

R

m n

i ji j

m n

i j i ji j

f x y dA

f x y A

x yf g u v h u v u v

u v

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45

Notice that this double sum is a Riemann

sum for the integral

DOUBLE INTEGRALS

( , )( ( , ), ( , ))

( , )S

x yf g u v h u v du dv

u v

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46

The foregoing argument suggests

that the following theorem is true.

A full proof is given in books on advanced calculus.

DOUBLE INTEGRALS

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47

Suppose:

T is a C1 transformation whose Jacobian is nonzero and that maps a region S in the uv-plane onto a region R in the xy-plane.

f is continuous on R and that R and S are type I or type II plane regions.

T is one-to-one, except perhaps on the boundary of S.

CHG. OF VRBLS. (DOUBLE INTEG.) Theorem 9

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48

Then,

CHG. OF VRBLS. (DOUBLE INTEG.)

( , )

( , )( ( , ), ( , ))

( , )

R

S

f x y dA

x yf x u v y u v du dv

u v

Theorem 9

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49

Theorem 9 says that we change from

an integral in x and y to an integral in u and v

by expressing x and y in terms of u and v

and writing:

CHG. OF VRBLS. (DOUBLE INTEG.)

( , )

( , )

x ydA du dv

u v

Page 50: MULTIPLE INTEGRALS 16. 2 MULTIPLE INTEGRALS 16.9 Change of Variables in Multiple Integrals In this section, we will learn about: The change of variables

50

Notice the similarity between

Theorem 9 and the one-dimensional

formula in Equation 2.

Instead of the derivative dx/du, we have the absolute value of the Jacobian, that is,

|∂(x, y)/∂(u, v)|

CHG. OF VRBLS. (DOUBLE INTEG.)

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51

As a first illustration of Theorem 9,

we show that the formula for integration

in polar coordinates is just a special case.

CHG. OF VRBLS. (DOUBLE INTEG.)

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52

Here, the transformation T from the rθ-plane

to the xy-plane is given by:

x = g(r, θ) = r cos θ

y = h(r, θ) = r sin θ

CHG. OF VRBLS. (DOUBLE INTEG.)

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53

The geometry of

the transformation is

shown here.

T maps an ordinary rectangle in the rθ-plane to a polar rectangle in the xy-plane.

CHG. OF VRBLS. (DOUBLE INTEG.)

Fig. 16.9.7, p. 1053

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54

The Jacobian of T is:

CHG. OF VRBLS. (DOUBLE INTEG.)

2 2

cos sin( , )

sin cos( , )

cos sin

0

x xrx y r

y x rr

r

r r

r

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55

So, Theorem 9 gives:

This is the same as Formula 2 in Section 16.4

CHG. OF VRBLS. (DOUBLE INTEG.)

( , )

( , )( cos , sin )

( , )

( cos , sin )

R

S

b

a

f x y dx dy

x yf r r dr d

u v

f r r r dr d

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56

Use the change of variables x = u2 – v2,

y = 2uv to evaluate the integral

where R is the region bounded

by: The x-axis. The parabolas y2 = 4 – 4x and y2 = 4 + 4x,

y ≥ 0.

CHG. OF VRBLS. (DOUBLE INTEG.) Example 2

R

y dA

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57

The region R is pictured here.

CHG. OF VRBLS. (DOUBLE INTEG.) Example 2

Fig. 16.9.2, p. 1050

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58

In Example 1, we discovered that

T(S) = R

where S is the square [0, 1] x [0, 1].

Indeed, the reason for making the change of variables to evaluate the integral is that S is a much simpler region than R.

CHG. OF VRBLS. (DOUBLE INTEG.) Example 2

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59

First, we need to compute the Jacobian:

CHG. OF VRBLS. (DOUBLE INTEG.) Example 2

2 2

2 2( , )

2 2( , )

4 4 0

x xu vx y u v

y y v uu v

u v

u v

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60

So, by Theorem 9,

CHG. OF VRBLS. (DOUBLE INTEG.) Example 2

1 1 2 2

0 0

1 1 3 3

0 0

1 14 2 31 14 2 00

1 13 2 4

00

( , )2

( , )

(2 )4( )

8 ( )

8

(2 4 ) 2

R S

u

u

x yy dA uv dA

u v

uv u v du dv

u v uv du dv

u v u v dv

v v dv v v

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61

Example 2 was not very difficult to solve as

we were given a suitable change of variables.

If we are not supplied with a transformation,

the first step is to think of an appropriate

change of variables.

CHG. OF VRBLS. (DOUBLE INTEG.) Note

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62

If f(x, y) is difficult to integrate,

The form of f(x, y) may suggest a transformation.

If the region of integration R is awkward,

The transformation should be chosen so that the corresponding region S in the uv-plane has a convenient description.

CHG. OF VRBLS. (DOUBLE INTEG.) Note

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63

Evaluate the integral

where R is the trapezoidal region

with vertices

(1, 0), (2, 0), (0, –2), (0,–1)

CHG. OF VRBLS. (DOUBLE INTEG.) Example 3

( ) /( )x y x y

Re dA

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64

It isn’t easy to integrate e(x+y)/(x–y).

So, we make a change of variables

suggested by the form of this function:

u = x + y v = x – y

These equations define a transformation T–1 from the xy-plane to the uv-plane.

CHG. OF VRBLS. (DOUBLE INTEG.) E. g. 3—Eqns. 10

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65

Theorem 9 talks about a transformation T

from the uv-plane to the xy-plane.

It is obtained by solving Equations 10

for x and y:

x = ½(u + v) y = ½(u – v)

CHG. OF VRBLS. (DOUBLE INTEG.) E. g. 3—Equation 11

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66

The Jacobian of T is:

CHG. OF VRBLS. (DOUBLE INTEG.)

1 12 2 1

21 12 2

( , )

( , )

x xx y u v

y yu v

u v

Example 3

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67

To find the region S in the uv-plane

corresponding to R, we note that:

The sides of R lie on the lines y = 0 x – y = 2 x = 0 x – y = 1

From either Equations 10 or Equations 11, the image lines in the uv-plane are:

u = v v = 2 u = –v v = 1

CHG. OF VRBLS. (DOUBLE INTEG.) Example 3

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68

Thus, the region S is

the trapezoidal region

with vertices

(1, 1), (2, 2),

(–2, 2), (–1 ,1)

CHG. OF VRBLS. (DOUBLE INTEG.) Example 3

Fig. 16.9.8, p. 1054

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69

S =

{(u, v) | 1 ≤ v ≤ 2,

–v ≤ u ≤ v}

CHG. OF VRBLS. (DOUBLE INTEG.) Example 3

Fig. 16.9.8, p. 1054

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70

So, Theorem 9 gives:

CHG. OF VRBLS. (DOUBLE INTEG.) Example 3

( ) /( ) /

2 / 121

2 /12 1

2 1 1312 41

( , )

( , )

( ) ( )

x y x y u v

R S

v u v

v

u vu v

u v

x ye dA e du dv

u v

e du dv

ve dv

e e v dv e e

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71

There is a similar change of variables

formula for triple integrals.

Let T be a transformation that maps a region S in uvw-space onto a region R in xyz-space by means of the equations

x = g(u, v, w) y = h(u, v, w) z = k(u, v, w)

TRIPLE INTEGRALS

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72

The Jacobian of T is this 3 x 3 determinant:

TRIPLE INTEGRALS

( , , )

( , , )

x x x

u v wx y z y y y

u v w u v wz z z

u v w

Equation 12

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73

Under hypotheses similar to those

in Theorem 9, we have this formula for

triple integrals:

TRIPLE INTEGRALS

( , , )

( ( , , ), ( , , ), ( , , ))

( , , )

( , , )

R

S

f x y z dV

f x u v w y u v w z u v w

x y zdu dv dw

u v w

Formula 13

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74

Use Formula 13 to derive the formula for

triple integration in spherical coordinates.

The change of variables is given by:

x = ρ sin Φ cos θ

y = ρ sin Φ sin θ

z = ρ cos Φ

TRIPLE INTEGRALS Example 4

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75

We compute the Jacobian as follows:

TRIPLE INTEGRALS

( , , )

( , , )

sin cos sin sin cos cos

sin sin sin cos cos sin

cos 0 sin

x y z

Example 4

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76

TRIPLE INTEGRALS

2 2 2 2

2 2 2 2

2 2 2 2

2

sin sin cos coscos

sin cos cos sin

sin cos sin sinsin

sin sin sin cos

cos ( sin cos sin sin cos cos )

sin ( sin cos sin sin )

sin cos sin sin

sin

Example 4

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77

Since 0 ≤ Φ ≤ π , we have sin Φ ≥ 0.

Therefore,

TRIPLE INTEGRALS

2

2

( , , )sin

( , , )

sin

x y z

Example 4

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78

Thus, Formula 13 gives:

This is equivalent to Formula 3 in Section15.8

TRIPLE INTEGRALS

2

( , , )

( sin cos , sin sin , cos )

sin

R

S

f x y z dV

f

d d d

Example 4