46. ,
is the disk with center the origin and radius
■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■
47. Prove Property 11.
In evaluating a double integral over a region , a sum of iterated integrals was obtained as follows:
Sketch the region and express the double integral as an iterated integral with reversed order of integration.
D
yy
D
fx, y dA
y
01y
02yfx, y dx dyy
13y
03yfx, y dx dy 48. D1
D 2
yy
D
ex2y2dA 49. Evaluate , where
[Hint: Exploit the fact that is symmetric with respect to both axes.]
50. Use symmetry to evaluate , where is the region bounded by the square with vertices and .
51. Compute , where is the disk
, by first identifying the integral as the volume of a solid.
52. Graph the solid bounded by the plane and the paraboloid and find its exact volume.
(Use your CAS to do the graphing, to find the equations of the boundary curves of the region of integration, and to evaluate the double integral.)
z 4 x2 y2
x y z 1
CAS
x2 y2 1
xxDs1 x2 y2dA D
0, 5 5, 0
xxD2 3x 4y dA D D
D x, yxxD
xx2 y2 2.2tan x y3 4 dA
DOUBLE INTEGRALS IN POLAR COORDINATES
Suppose that we want to evaluate a double integral , where is one of the regions shown in Figure 1. In either case the description of in terms of rectan- gular coordinates is rather complicated but is easily described using polar coordinates.
Recall from Figure 2 that the polar coordinates of a point are related to the rect- angular coordinates by the equations
The regions in Figure 1 are special cases of a polar rectangle
which is shown in Figure 3. In order to compute the double integral , where is a polar rectangle, we divide the interval into subintervals with lengths and we divide the interval into subintervals
with lengths . Then the circles and the rays divide the polar rectangle R into the small polar rectangles shown in Figure 4.
j r ri
jjj1
j1,j ri ri ri1 , n
ri1, ri a, b m
R
xx
R fx, y dA Rr, a r b,y r sin x r cos
r2 x2 y2
x, y r,
FIGURE 1
0 x y
R
≈+¥=1
(a) R=s(r, ¨) | 0¯r¯1, 0¯¨¯2πd
x 0
y
R
≈+¥=4
≈+¥=1
(b) R=s(r, ¨) | 1¯r¯2, 0¯¨¯πd
R
R
xx
R fx, y dA R12.3
■ Polar coordinates were introduced in Section 9.3.
O y
x
¨ x r y
P(r, ¨ ) =P(x, y)
FIGURE 2
The “center” of the polar subrectangle
has polar coordinates
We compute the area of using the fact that the area of a sector of a circle with radius and central angle is . Subtracting the areas of two such sectors, each of which has central angle , we find that the area of is
Although we have defined the double integral in terms of ordinary rectangles, it can be shown that, for continuous functions , we always obtain the same answer using polar rectangles. The rectangular coordinates of the center of
are , so a typical Riemann sum is
If we write , then the Riemann sum in Equation 1 can be written as
which is a Riemann sum for the double integral
y
y
abtr, dr d mi1j1
n tri*,j* rijtr, r f r cos , r sin
mi1j
1n fri* cos j*, ri* sin j* Aiji1m j1n fri* cos j*, ri* sin j* ri*rij1
ri* cosj*, ri* sin j*
Rij
f
xx
R fx, y dA12ri ri1ri ri1 j ri*rij
Aij12ri2j12ri21j12ri2 ri21 j Rij
j
1 2r2
r
Rij
j*12j1j ri* 12ri1 ri
Rij
r, ri1 r ri,j1 jFIGURE 3 Polar rectangle O
∫ å
r=a ¨=å
¨=∫
r=b
R
r=ri
r=ri _¡ Rij (ri*, ¨j*)
¨=¨j _¡
¨=¨j
Ψj
FIGURE 4 Dividing R into polar subrectangles O
Therefore, we have
CHANGE TO POLAR COORDINATES IN A DOUBLE INTEGRAL If is contin- uous on a polar rectangle given by , , where
, then
The formula in (2) says that we convert from rectangular to polar coordinates in a double integral by writing and , using the appropriate limits of
|integration for and , and replacing by . Be careful not to forget the addi- tional factor r on the right side of Formula 2.A classical method for remembering this is shown in Figure 5, where the “infinitesimal” polar rectangle can be thought of as an ordinary rectangle with dimensions and and therefore has “area”
EXAMPLE 1 Evaluate , where is the region in the upper half-
plane bounded by the circles and .
SOLUTION The region can be described as
It is the half-ring shown in Figure 1(b), and in polar coordinates it is given by , . Therefore, by Formula 2,
7 sin 15 ■ 2 15
4 sin 2
0 152y
0[
7 cos 1521 cos 2]
dy
0[
r3cos r4sin2]
r1r2d
y
07 cos 15 sin2 dy
0y
123r2cos 4r3sin2 dr dyy
R
3x 4y2 dA
y
0y
123r cos 4r2sin2 r dr d0 1 r 2
R
x, yy 0, 1 x2 y2 4R
x2 y2 4 x2 y2 1 R
xx
R3x 4y2 dAdA r dr d.
r d dr
r dr d
dA r
y r sin x r cos
yy
R
fx, y dA
y
y
abfr cos , r sin r dr d0 2 R 0 a r b f
2
y
y
abfr cos , r sin r dr dlim
maxri,jl 0i
1m j1n tri*,j* rijy
y
ab tr, dr dyy
R
fx, y dA lim
maxri,jl 0i
1m j1n fri* cos j*, ri* sin j* AijO
d¨
r d¨
dr dA
r
FIGURE 5
■ Here we use the trigonometric identity
as discussed in Section 6.2.
sin2 121 cos 2
EXAMPLE 2 Find the volume of the solid bounded by the plane and the paraboloid .
SOLUTION If we put in the equation of the paraboloid, we get . This means that the plane intersects the paraboloid in the circle , so the solid lies under the paraboloid and above the circular disk given by
[see Figures 6 and 1(a)]. In polar coordinates is given by , .
Since , the volume is
If we had used rectangular coordinates instead of polar coordinates, then we would have obtained
which is not easy to evaluate because it involves finding . ■
What we have done so far can be extended to the more complicated type of region shown in Figure 7. It’s similar to the type II rectangular regions considered in Sec- tion 12.2. In fact, by combining Formula 2 in this section with Formula 12.2.5, we obtain the following formula.
If is continuous on a polar region of the form
then
In particular, taking , , and in this formula, we see that the area of the region bounded by , , and is
and this agrees with Formula 9.4.3.
y
r220hdy
12h 2dAD
yy
D
1 dA
y
y
0hr dr dr h
D
h2 h
h1 0 fx, y 1
yy
D
fx, y dA
y
y
hh12fr cos, r sin r dr dD
r, , h1 r h2f
3
x
1 x232dx Vyy
D
1 x2 y2 dA
y
11y
s1xs1x221 x2 y2 dy dxy
02dy
01r r3 dr 2r22 r4401 2V
yy
D
1 x2 y2 dA
y
02y
011 r2 r dr d1 x2 y2 1 r2 D 0 r 1 0 2
x2 y2 1 D
x2 yx22 y 12 1 z 0
z 1 x2 y2 z 0
V
FIGURE 6
y (0, 0, 1)
x
z
O
∫ å
r=h¡(¨)
¨=å
¨=∫ r=h™(¨)
D
FIGURE 7
D=s(r, ¨) | 寨¯∫, h¡(¨)¯r¯h™(¨)d
EXAMPLE 3 Find the volume of the solid that lies under the paraboloid , above the -plane, and inside the cylinder . SOLUTION The solid lies above the disk whose boundary circle has equation
or, after completing the square,
(See Figures 8 and 9.) In polar coordinates we have and , so the boundary circle becomes , or . Thus the disk is given by
and, by Formula 3, we have
2
[
32 sin 2 18 sin 4]
0 ■2 2
322 322
y
021 2 cos 2 121 cos 4 d8
y
02 cos4 d 8y
021 cos 22 2d4
y
22 cos4 dy
22 r4402 cos dV
yy
D
x2 y2 dA
y
22y
02 cosr2r dr dD
r, 2 2, 0 r 2 cosD r 2 cos
r2 2r cos x2 y2 r2 x r cos
x 12 y2 1
x2 y2 2x D
x2 y2 2x z x2 y2 xy
V
FIGURE 8 0 y
1 2 x
D
(x-1)@+¥=1 (or r=2 cos ¨)
FIGURE 9
y x
z
5–6 ■ Sketch the region whose area is given by the integral and evaluate the integral.
5. 6.
■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■
7–12 ■ Evaluate the given integral by changing to polar coordinates.
7. ,
where is the disk with center the origin and radius 3 8. , where is the region that lies to the left of
the -axis between the circles and
9. , where is the region that lies above the -axis within the circle
10. ,
where
, where
12. , where is the region in the first quadrant enclosed by the circle
■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■
x2 y2 25
xxRyexdA R
R x, y
1 x2 y2 4, 0 y xxxR arctan yx dA 11.
R x, y
x2 y2 4, x 0xxRs4 x2 y2dA
x2 y2 9 x
xxR cosx2 y2 dA R
x2 y2 4 x2 y2 1
y
xxRx y dA R D
xxDxy dA
y
02y
04 cos r dr dy
2y
47r dr d 1– 4 ■ A region is shown. Decide whether to use polar coor-dinates or rectangular coordinates and write
as an iterated integral, where is an arbitrary continuous func- tion on .
2.
3. 4.
■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■
0 1 3
3
1 y
x R
0 2
2 y
x R
0 2
y
x R
0 2
5 2 5
2 y
x R
1.
R
f
xxRfx, y dA R
EXERCISES
12.3
28. An agricultural sprinkler distributes water in a circular pat- tern of radius 100 ft. It supplies water to a depth of feet per hour at a distance of feet from the sprinkler.
(a) What is the total amount of water supplied per hour to the region inside the circle of radius centered at the sprinkler?
(b) Determine an expression for the average amount of water per hour per square foot supplied to the region inside the circle of radius .
Use polar coordinates to combine the sum
into one double integral. Then evaluate the double integral.
30. (a) We define the improper integral (over the entire plane
where is the disk with radius and center the origin.
Show that
(b) An equivalent definition of the improper integral in part (a) is
where is the square with vertices . Use this to show that
(c) Deduce that
(d) By making the change of variable , show that
(This is a fundamental result for probability and statistics.)
31. Use the result of Exercise 30 part (c) to evaluate the follow- ing integrals.
(a)
y
0x2ex2dx (b)y
0sx exdxy
ex22dx s2t s2 x
y
ex2dx sy
ex2dxy
ey2dya, a
Sa
yy
⺢2ex2y2dA limal
yy
Sa
ex2y2dA
y
y
ex2y2dAa Da
limal
yy
Da
ex2y2dA I
yy
⺢2
ex2y2dA
y
y
ex2y2dy dx⺢2
y
11s2y
s1xx 2xy dy dxy
1s2y
0xxy dy dxy
s22y
0s4x2xy dy dx 29.R
R r
er 13–19 ■ Use polar coordinates to find the volume of the given
solid.
13. Under the cone and above the disk
14. Below the paraboloid and above the -plane
15. A sphere of radius
16. Inside the sphere and outside the cylinder
Above the cone and below the sphere
18. Bounded by the paraboloid and the plane in the first octant
19. Inside both the cylinder and the ellipsoid
■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■
20. (a) A cylindrical drill with radius is used to bore a hole through the center of a sphere of radius . Find the vol- ume of the ring-shaped solid that remains.
(b) Express the volume in part (a) in terms of the height of the ring. Notice that the volume depends only on , not on or .
21–22 ■ Use a double integral to find the area of the region.
One loop of the rose
22. The region enclosed by the curve
■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■
23–26 ■ Evaluate the iterated integral by converting to polar coordinates.
23.
24.
25.
26.
■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■ ■
27. A swimming pool is circular with a 40-ft diameter. The depth is constant along east-west lines and increases linearly from 2 ft at the south end to 7 ft at the north end.
Find the volume of water in the pool.
y
02y
0s2xx2sx2 y2dy dxy
01y
ys2y2x y dx dyy
0ay
sa0 2y2 x2y dx dyy
33y
0s9x2 sinx2 y2 dy dxr 4 3 cos r cos 3
21.
r2
r1
h h r2
r1
4x2 4y2 z2 64
x2 y2 4
z 7 z 1 2x2 2y2 x2 y2 z2 1z sx2 y2
17.
x2 y2 4
x2 y2 z2 16 a
xy
z 18 2x2 2y2 x2 y2 4 z sx2 y2