Skip to ContentGo to accessibility page
Calculus Volume 3

5.3 Double Integrals in Polar Coordinates

Calculus Volume 35.3 Double Integrals in Polar Coordinates

5.3 Double Integrals in Polar Coordinates

Learning Objectives

  • 5.3.1 Recognize the format of a double integral over a polar rectangular region.
  • 5.3.2 Evaluate a double integral in polar coordinates by using an iterated integral.
  • 5.3.3 Recognize the format of a double integral over a general polar region.
  • 5.3.4 Use double integrals in polar coordinates to calculate areas and volumes.

Double integrals are sometimes much easier to evaluate if we change rectangular coordinates to polar coordinates. However, before we describe how to make this change, we need to establish the concept of a double integral in a polar rectangular region.

Polar Rectangular Regions of Integration

When we defined the double integral for a continuous function in rectangular coordinates—say, gg over a region RR in the xyxy-plane—we divided RR into subrectangles with sides parallel to the coordinate axes. These sides have either constant xx-values and/or constant yy-values. In polar coordinates, the shape we work with is a polar rectangle, whose sides have constant rr-values and/or constant θθ-values. This means we can describe a polar rectangle as in Figure 5.28(a), with R={(r,θ)|a≤r≤b,α≤θ≤β}.R={(r,θ)|a≤r≤b,α≤θ≤β}.

In this section, we are looking to integrate over polar rectangles. Consider a function f(r,θ)f(r,θ) over a polar rectangle R.R. We divide the interval [a,b][a,b] into mm subintervals [ri−1,ri][ri−1,ri] of length Δr=(b−a)/mΔr=(b−a)/m and divide the interval [α,β][α,β] into nn subintervals [θj−1,θj][θj−1,θj] of width Δθ=(β−α)/n.Δθ=(β−α)/n. This means that the circles r=rir=ri and rays θ=θjθ=θj for 1≤i≤m1≤i≤m and 1≤j≤n1≤j≤n divide the polar rectangle RR into smaller polar subrectangles RijRij (Figure 5.28(b)).

Figure 5.28 (a) A polar rectangle RR (b) divided into subrectangles Rij.Rij. (c) Close-up of a subrectangle.

As before, we need to find the area ΔAΔA of the polar subrectangle RijRij and the “polar” volume of the thin box above Rij.Rij. Recall that, in a circle of radius r,r, the length ss of an arc subtended by a central angle of θθ radians is s=rθ.s=rθ. Notice that the polar rectangle RijRij looks a lot like a trapezoid with parallel sides ri−1Δθri−1Δθ and riΔθriΔθ and with a width Δr.Δr. Hence the area of the polar subrectangle RijRij is

ΔA=12Δr(ri−1Δθ+riΔθ).ΔA=12Δr(ri−1Δθ+riΔθ).

Simplifying and letting rij*=12(ri−1+ri),rij*=12(ri−1+ri), we have ΔA=rij*ΔrΔθ.ΔA=rij*ΔrΔθ. Therefore, the polar volume of the thin box above RijRij (Figure 5.29) is

f(rij*,θij*)ΔA=f(rij*,θij*)rij*ΔrΔθ.f(rij*,θij*)ΔA=f(rij*,θij*)rij*ΔrΔθ.
Figure 5.29 Finding the volume of the thin box above polar rectangle Rij.Rij.

Using the same idea for all the subrectangles and summing the volumes of the rectangular boxes, we obtain a double Riemann sum as

∑i=1m∑j=1nf(rij*,θij*)rij*ΔrΔθ.∑i=1m∑j=1nf(rij*,θij*)rij*ΔrΔθ.

As we have seen before, we obtain a better approximation to the polar volume of the solid above the region RR when we let mm and nn become larger. Hence, we define the polar volume as the limit of the double Riemann sum,

V=limm,n→∞∑i=1m∑j=1nf(rij*,θij*)rij*ΔrΔθ.V=limm,n→∞∑i=1m∑j=1nf(rij*,θij*)rij*ΔrΔθ.

This becomes the expression for the double integral.

Definition

The double integral of the function f(r,θ)f(r,θ) over the polar rectangular region RR in the rθrθ-plane is defined as

∬Rf(r,θ)dA=limm,n→∞∑i=1m∑j=1nf(rij*,θij*)ΔA=limm,n→∞∑i=1m∑j=1nf(rij*,θij*)rij*ΔrΔθ.∬Rf(r,θ)dA=limm,n→∞∑i=1m∑j=1nf(rij*,θij*)ΔA=limm,n→∞∑i=1m∑j=1nf(rij*,θij*)rij*ΔrΔθ.
(5.8)

Again, just as in Double Integrals over Rectangular Regions, the double integral over a polar rectangular region can be expressed as an iterated integral in polar coordinates. Hence,

∬Rf(r,θ)dA=∬Rf(r,θ)rdrdθ=∫θ=αθ=β∫r=ar=bf(r,θ)rdrdθ.∬Rf(r,θ)dA=∬Rf(r,θ)rdrdθ=∫θ=αθ=β∫r=ar=bf(r,θ)rdrdθ.

Notice that the expression for dAdA is replaced by rdrdθrdrdθ when working in polar coordinates. Another way to look at the polar double integral is to change the double integral in rectangular coordinates by substitution. When the function ff is given in terms of xx and y,y, using x=rcosθ,y=rsinθ,anddA=rdrdθx=rcosθ,y=rsinθ,anddA=rdrdθ changes it to

∬Rf(x,y)dA=∬Rf(rcosθ,rsinθ)rdrdθ.∬Rf(x,y)dA=∬Rf(rcosθ,rsinθ)rdrdθ.

Note that all the properties listed in Double Integrals over Rectangular Regions for the double integral in rectangular coordinates hold true for the double integral in polar coordinates as well, so we can use them without hesitation.

Example 5.24

Sketching a Polar Rectangular Region

Sketch the polar rectangular region R={(r,θ)|1≤r≤3,0≤θ≤π}.R={(r,θ)|1≤r≤3,0≤θ≤π}.

Now that we have sketched a polar rectangular region, let us demonstrate how to evaluate a double integral over this region by using polar coordinates.

Example 5.25

Evaluating a Double Integral over a Polar Rectangular Region

Evaluate the integral ∬R3xdA∬R3xdA over the region R={(r,θ)|1≤r≤2,0≤θ≤π}.R={(r,θ)|1≤r≤2,0≤θ≤π}.

Checkpoint 5.17

Sketch the region R={(r,θ)|1≤r≤2,−π2≤θ≤π2},R={(r,θ)|1≤r≤2,−π2≤θ≤π2}, and evaluate ∬RxdA.∬RxdA.

Example 5.26

Evaluating a Double Integral by Converting from Rectangular Coordinates

Evaluate the integral ∬R(1−x2−y2)dA∬R(1−x2−y2)dA where RR is the unit disk on the xyxy-plane.

Example 5.27

Evaluating a Double Integral by Converting from Rectangular Coordinates

Evaluate the integral ∬R(x+y)dA∬R(x+y)dA where R={(x,y)|1≤x2+y2≤4,x≤0}.R={(x,y)|1≤x2+y2≤4,x≤0}.

Checkpoint 5.18

Evaluate the integral ∬R(4−x2−y2)dA∬R(4−x2−y2)dA where RR is the circle of radius 22 on the xyxy-plane.

General Polar Regions of Integration

To evaluate the double integral of a continuous function by iterated integrals over general polar regions, we consider two types of regions, analogous to Type I and Type II as discussed for rectangular coordinates in Double Integrals over General Regions. It is more common to write polar equations as r=f(θ)r=f(θ) than θ=f(r),θ=f(r), so we describe a general polar region as D={(r,θ)|α≤θ≤β,h1(θ)≤r≤h2(θ)}D={(r,θ)|α≤θ≤β,h1(θ)≤r≤h2(θ)} (see the following figure).

Figure 5.32 A general polar region between α≤θ≤βα≤θ≤β and h1(θ)≤r≤h2(θ).h1(θ)≤r≤h2(θ).

Theorem 5.8

Double Integrals over General Polar Regions

If f(r,θ)f(r,θ) is continuous on a general polar region DD as described above, then

∬Df(r,θ)rdrdθ=∫θ=αθ=β∫r=h1(θ)r=h2(θ)f(r,θ)rdrdθ∬Df(r,θ)rdrdθ=∫θ=αθ=β∫r=h1(θ)r=h2(θ)f(r,θ)rdrdθ
(5.9)

Example 5.28

Evaluating a Double Integral over a General Polar Region

Evaluate the integral ∬Dr2 · sin θ · rdrdθ∬Dr2 · sin θ · rdrdθ where DD is the region bounded by the polar axis and the upper half of the cardioid r=1+cosθ.r=1+cosθ.

Checkpoint 5.19

Evaluate the integral

∬Dr2sin22θrdrdθwhereD={(r,θ)|-π4≤θ≤π4, 0≤r≤2cos2θ}.∬Dr2sin22θrdrdθwhereD={(r,θ)|-π4≤θ≤π4, 0≤r≤2cos2θ}.

Polar Areas and Volumes

As in rectangular coordinates, if a solid SS is bounded by the surface z=f(r,θ),z=f(r,θ), as well as by the surfaces r=a,r=b,θ=α,r=a,r=b,θ=α, and θ=β,θ=β, we can find the volume VV of SS by double integration, as

V=∬Rf(r,θ)rdrdθ=∫θ=αθ=β∫r=ar=bf(r,θ)rdrdθ.V=∬Rf(r,θ)rdrdθ=∫θ=αθ=β∫r=ar=bf(r,θ)rdrdθ.

If the base of the solid can be described as D={(r,θ)|α≤θ≤β,h1(θ)≤r≤h2(θ)},D={(r,θ)|α≤θ≤β,h1(θ)≤r≤h2(θ)}, then the double integral for the volume becomes

V=∬Df(r,θ)rdrdθ=∫θ=αθ=β∫r=h1(θ)r=h2(θ)f(r,θ)rdrdθ.V=∬Df(r,θ)rdrdθ=∫θ=αθ=β∫r=h1(θ)r=h2(θ)f(r,θ)rdrdθ.

We illustrate this idea with some examples.

Example 5.29

Finding a Volume Using a Double Integral

Find the volume of the solid that lies under the paraboloid z=1−x2−y2z=1−x2−y2 and above the unit circle on the xyxy-plane (see the following figure).

Figure 5.34 The paraboloid z=1−x2−y2z=1−x2−y2.

Example 5.30

Finding a Volume Using Double Integration

Find the volume of the solid that lies under the paraboloid z=4−x2−y2z=4−x2−y2 and above the disk (x−1)2+y2=1(x−1)2+y2=1 on the xyxy-plane. See the paraboloid in Figure 5.35 intersecting the cylinder (x−1)2+y2=1(x−1)2+y2=1 above the xyxy-plane.

Figure 5.35 Finding the volume of a solid with a paraboloid cap and a circular base.

Notice in the next example that integration is not always easy with polar coordinates. Complexity of integration depends on the function and also on the region over which we need to perform the integration. If the region has a more natural expression in polar coordinates or if ff has a simpler antiderivative in polar coordinates, then the change in polar coordinates is appropriate; otherwise, use rectangular coordinates.

Example 5.31

Finding a Volume Using a Double Integral

Find the volume of the region that lies under the paraboloid z=x2+y2z=x2+y2 and above the triangle enclosed by the lines y=x,x=0,y=x,x=0, and x+y=2x+y=2 in the xyxy-plane (Figure 5.36).

To answer the question of how the formulas for the volumes of different standard solids such as a sphere, a cone, or a cylinder are found, we want to demonstrate an example and find the volume of an arbitrary cone.

Example 5.32

Finding a Volume Using a Double Integral

Use polar coordinates to find the volume inside the cone z=2−x2+y2z=2−x2+y2 and above the xy-plane.xy-plane.

Analysis

Note that if we were to find the volume of an arbitrary cone with radius aa units and height hh units, then the equation of the cone would be z=h−hax2+y2.z=h−hax2+y2.

We can still use Figure 5.37 and set up the integral as ∫θ=0θ=2π∫r=0r=a(h−har)rdrdθ.∫θ=0θ=2π∫r=0r=a(h−har)rdrdθ.

Evaluating the integral, we get 13πa2h.13πa2h.

Checkpoint 5.20

Use polar coordinates to find an iterated integral for finding the volume of the solid enclosed by the paraboloids z=x2+y2z=x2+y2 and z=16−x2−y2.z=16−x2−y2.

As with rectangular coordinates, we can also use polar coordinates to find areas of certain regions using a double integral. As before, we need to understand the region whose area we want to compute. Sketching a graph and identifying the region can be helpful to realize the limits of integration. Generally, the area formula in double integration will look like

AreaA=∫αβ∫h1(θ)h2(θ)1rdrdθ.AreaA=∫αβ∫h1(θ)h2(θ)1rdrdθ.

Example 5.33

Finding an Area Using a Double Integral in Polar Coordinates

Evaluate the area bounded by the curve r=cos4θ.r=cos4θ.

Example 5.34

Finding Area Between Two Polar Curves

Find the area enclosed by the circle r=3cosθr=3cosθ and the cardioid r=1+cosθ.r=1+cosθ.

Checkpoint 5.21

Find the area enclosed inside the cardioid r=3−3sinθr=3−3sinθ and outside the cardioid r=1+sinθ.r=1+sinθ.

Example 5.35

Evaluating an Improper Double Integral in Polar Coordinates

Evaluate the integral ∬ℝ2e−10(x2+y2)dxdy.∬ℝ2e−10(x2+y2)dxdy.

Checkpoint 5.22

Evaluate the integral ∬ℝ2e−4(x2+y2)dxdy.∬ℝ2e−4(x2+y2)dxdy.

Section 5.3 Exercises

In the following exercises, express the region DD in polar coordinates.

122.

DD is the region of the disk of radius 22 centered at the origin that lies in the first quadrant.

123.

DD is the region between the circles of radius 44 and radius 55 centered at the origin that lies in the second quadrant.

124.

DD is the region bounded by the yy-axis and x=1−y2.x=1−y2.

125.

DD is the region bounded by the xx-axis and y=2−x2.y=2−x2.

126.

D = { ( x , y ) | x 2 + y 2 ≤ 4 x } D = { ( x , y ) | x 2 + y 2 ≤ 4 x }

127.

D = { ( x , y ) | x 2 + y 2 ≤ 4 y } D = { ( x , y ) | x 2 + y 2 ≤ 4 y }

In the following exercises, the graph of the polar rectangular region DD is given. Express DD in polar coordinates.

128.
129.
130.
131.
132.

In the following graph, the region DD is situated below y=xy=x and is bounded by x=1,x=5,x=1,x=5, and y=0.y=0.

133.

In the following graph, the region DD is bounded by y=xy=x and y=x2.y=x2.

In the following exercises, evaluate the double integral ∬Rf(x,y)dA∬Rf(x,y)dA over the polar rectangular region D.D.

134.

f ( x , y ) = x 2 + y 2 , D = { ( r , θ ) | 3 ≤ r ≤ 5 , 0 ≤ θ ≤ 2 π } f ( x , y ) = x 2 + y 2 , D = { ( r , θ ) | 3 ≤ r ≤ 5 , 0 ≤ θ ≤ 2 π }

135.

f ( x , y ) = x + y , D = { ( r , θ ) | 3 ≤ r ≤ 5 , 0 ≤ θ ≤ 2 π } f ( x , y ) = x + y , D = { ( r , θ ) | 3 ≤ r ≤ 5 , 0 ≤ θ ≤ 2 π }

136.

f ( x , y ) = x 2 + x y , D = { ( r , θ ) | 1 ≤ r ≤ 2 , π ≤ θ ≤ 2 π } f ( x , y ) = x 2 + x y , D = { ( r , θ ) | 1 ≤ r ≤ 2 , π ≤ θ ≤ 2 π }

137.

f ( x , y ) = x 4 + y 4 , D = { ( r , θ ) | 1 ≤ r ≤ 2 , 3 π 2 ≤ θ ≤ 2 π } f ( x , y ) = x 4 + y 4 , D = { ( r , θ ) | 1 ≤ r ≤ 2 , 3 π 2 ≤ θ ≤ 2 π }

138.

f(x,y)=x2+y23,f(x,y)=x2+y23, where D={(r,θ)|0≤r≤1,π2≤θ≤π}.D={(r,θ)|0≤r≤1,π2≤θ≤π}.

139.

f(x,y)=x4+2x2y2+y4,f(x,y)=x4+2x2y2+y4, where D={(r,θ)|3≤r≤4,π3≤θ≤2π3}.D={(r,θ)|3≤r≤4,π3≤θ≤2π3}.

140.

f(x,y)=sin(arctanyx),f(x,y)=sin(arctanyx), where D={(r,θ)|1≤r≤2,π6≤θ≤π3}D={(r,θ)|1≤r≤2,π6≤θ≤π3}

141.

f(x,y)=arctan(yx),f(x,y)=arctan(yx), where D={(r,θ)|2≤r≤3,π4≤θ≤π3}D={(r,θ)|2≤r≤3,π4≤θ≤π3}

142.

∬ D e x 2 + y 2 [ 1 + 2 arctan ( y x ) ] d A , D = { ( r , θ ) | 1 ≤ r ≤ 2 , π 6 ≤ θ ≤ π 3 } ∬ D e x 2 + y 2 [ 1 + 2 arctan ( y x ) ] d A , D = { ( r , θ ) | 1 ≤ r ≤ 2 , π 6 ≤ θ ≤ π 3 }

143.

∬ D ( e x 2 + y 2 + x 4 + 2 x 2 y 2 + y 4 ) arctan ( y x ) d A , D = { ( r , θ ) | 1 ≤ r ≤ 2 , π 4 ≤ θ ≤ π 3 } ∬ D ( e x 2 + y 2 + x 4 + 2 x 2 y 2 + y 4 ) arctan ( y x ) d A , D = { ( r , θ ) | 1 ≤ r ≤ 2 , π 4 ≤ θ ≤ π 3 }

In the following exercises, the integrals have been converted to polar coordinates. Verify that the identities are true and choose the easiest way to evaluate the integrals, in rectangular or polar coordinates.

144.

∫ 1 2 ∫ 0 x ( x 2 + y 2 ) d y d x = ∫ 0 π 4 ∫ sec θ 2 sec θ r 3 d r d θ ∫ 1 2 ∫ 0 x ( x 2 + y 2 ) d y d x = ∫ 0 π 4 ∫ sec θ 2 sec θ r 3 d r d θ

145.

∫ 2 3 ∫ 0 x x x 2 + y 2 d y d x = ∫ 0 π / 4 ∫ 2 sec θ 3secθ r cos θ d r d θ ∫ 2 3 ∫ 0 x x x 2 + y 2 d y d x = ∫ 0 π / 4 ∫ 2 sec θ 3secθ r cos θ d r d θ

146.

∫ 0 1 ∫ x 2 x 1 x 2 + y 2 d y d x = ∫ 0 π / 4 ∫ 0 tan θ sec θ d r d θ ∫ 0 1 ∫ x 2 x 1 x 2 + y 2 d y d x = ∫ 0 π / 4 ∫ 0 tan θ sec θ d r d θ

147.

∫ 0 1 ∫ x 2 x y x 2 + y 2 d y d x = ∫ 0 π / 4 ∫ 0 tan θ sec θ r sin θ d r d θ ∫ 0 1 ∫ x 2 x y x 2 + y 2 d y d x = ∫ 0 π / 4 ∫ 0 tan θ sec θ r sin θ d r d θ

In the following exercises, convert the integrals to polar coordinates and evaluate them.

148.

∫ 0 3 ∫ 0 9 − y 2 ( x 2 + y 2 ) d x d y ∫ 0 3 ∫ 0 9 − y 2 ( x 2 + y 2 ) d x d y

149.

∫ 0 2 ∫ − 4 − y 2 4 − y 2 ( x 2 + y 2 ) 2 d x d y ∫ 0 2 ∫ − 4 − y 2 4 − y 2 ( x 2 + y 2 ) 2 d x d y

150.

∫ 0 1 ∫ 0 1 − x 2 ( x + y ) d y d x ∫ 0 1 ∫ 0 1 − x 2 ( x + y ) d y d x

151.

∫ 0 4 ∫ − 16 − x 2 16 − x 2 sin ( x 2 + y 2 ) d y d x ∫ 0 4 ∫ − 16 − x 2 16 − x 2 sin ( x 2 + y 2 ) d y d x

152.

Evaluate the integral ∬DrdA∬DrdA where DD is the region bounded by the polar axis and the upper half of the cardioid r=1+cosθ.r=1+cosθ.

153.

Find the area of the region DD bounded by the polar axis and the upper half of the cardioid r=1+cosθ.r=1+cosθ.

154.

Evaluate the integral ∬DdA,∬DdA, where DD is the region bounded by the part of the four-leaved rose r=sin2θr=sin2θ situated in the first quadrant (see the following figure).

155.

Find the total area of the region enclosed by the four-leaved rose r=sin2θr=sin2θ (see the figure in the previous exercise).

156.

Find the area of the region D,D, which is the region bounded by y=4−x2,y=4−x2, x=3,x=3, x=2,x=2, and y=0.y=0.

157.

Find the area of the region D,D, which is the region inside the disk x2+y2≤4x2+y2≤4 and to the right of the line x=1.x=1.

158.

Determine the average value of the function f(x,y)=x2+y2f(x,y)=x2+y2 over the region DD bounded by the polar curve r=cos2θ,r=cos2θ, where −π4≤θ≤π4−π4≤θ≤π4 (see the following graph).

159.

Determine the average value of the function f(x,y)=x2+y2f(x,y)=x2+y2 over the region DD bounded by the polar curve r=3sin2θ,r=3sin2θ, where 0≤θ≤π20≤θ≤π2 (see the following graph).

160.

Find the volume of the solid situated in the first octant and bounded by the paraboloid z=1−4x2−4y2z=1−4x2−4y2 and the planes x=0,y=0,x=0,y=0, and z=0.z=0.

161.

Find the volume of the solid bounded by the paraboloid z=2−9x2−9y2z=2−9x2−9y2 and the plane z=1.z=1.

162.
  1. Find the volume of the solid S1S1 bounded by the cylinder x2+y2=1x2+y2=1 and the planes z=0z=0 and z=1.z=1.
  2. Find the volume of the solid S2S2 outside the double cone z2=x2+y2,z2=x2+y2, inside the cylinder x2+y2=1,x2+y2=1, and above the plane z=0.z=0.
  3. Find the volume of the solid inside the cone z2=x2+y2z2=x2+y2 and below the plane z=1z=1 by subtracting the volumes of the solids S1S1 and S2.S2.
163.
  1. Find the volume of the solid S1S1 inside the unit sphere x2+y2+z2=1x2+y2+z2=1 and above the plane z=0.z=0.
  2. Find the volume of the solid S2S2 inside the double cone (z−1)2=x2+y2(z−1)2=x2+y2 and above the plane z=0.z=0.
  3. Find the volume of the solid outside the double cone (z−1)2=x2+y2(z−1)2=x2+y2 and inside the sphere x2+y2+z2=1.x2+y2+z2=1.

For the following two exercises, consider a spherical ring, which is a sphere with a cylindrical hole cut so that the axis of the cylinder passes through the center of the sphere (see the following figure).

164.

If the sphere has radius 44 and the cylinder has radius 2,2, find the volume of the spherical ring.

165.

A cylindrical hole of diameter 66 cm is bored through a sphere of radius 55 cm such that the axis of the cylinder passes through the center of the sphere. Find the volume of the resulting spherical ring.

166.

Find the volume of the solid that lies under the double cone z2=4x2+4y2,z2=4x2+4y2, inside the cylinder x2+y2=x,x2+y2=x, and above the plane z=0.z=0.

167.

Find the volume of the solid that lies under the paraboloid z=x2+y2,z=x2+y2, inside the cylinder x2+y2=x,x2+y2=x, and above the plane z=0.z=0.

168.

Find the volume of the solid that lies under the plane x+y+z=10x+y+z=10 and above the disk x2+y2=4x.x2+y2=4x.

169.

Find the volume of the solid that lies under the plane 2x+y+2z=82x+y+2z=8 and above the unit disk x2+y2=1.x2+y2=1.

170.

A radial function ff is a function whose value at each point depends only on the distance between that point and the origin of the system of coordinates; that is, f(x,y)=g(r),f(x,y)=g(r), where r=x2+y2.r=x2+y2. Show that if ff is a continuous radial function, then ∬Df(x,y)dA=(θ2−θ1)[G(R2)−G(R1)],∬Df(x,y)dA=(θ2−θ1)[G(R2)−G(R1)], where G′(r)=rg(r)G′(r)=rg(r) and (x,y)∈D={(r,θ)|R1≤r≤R2,θ1≤θ≤θ2},(x,y)∈D={(r,θ)|R1≤r≤R2,θ1≤θ≤θ2}, with 0≤R1<R20≤R1<R2 and 0≤θ1<θ2≤2π.0≤θ1<θ2≤2π.

171.

Use the information from the preceding exercise to calculate the integral ∬D(x2+y2)3dA,∬D(x2+y2)3dA, where DD is the unit disk.

172.

Let f(x,y)=F′(r)rf(x,y)=F′(r)r be a continuous radial function defined on the annular region D={(r,θ)|R1≤r≤R2,0≤θ≤2π},D={(r,θ)|R1≤r≤R2,0≤θ≤2π}, where r=x2+y2,r=x2+y2, 0<R1<R2,0<R1<R2, and FF is a differentiable function. Show that ∬Df(x,y)dA=2π[F(R2)−F(R1)].∬Df(x,y)dA=2π[F(R2)−F(R1)].

173.

Apply the preceding exercise to calculate the integral ∬Dex2+y2x2+y2dxdy,∬Dex2+y2x2+y2dxdy, where DD is the annular region between the circles of radii 11 and 22 situated in the third quadrant.

174.

Let ff be a continuous function that can be expressed in polar coordinates as a product of a function of rr only and a function of θθ only; that is, f(x,y)=h(θ),f(x,y)=h(θ), where (x,y)∈D={(r,θ)|R1≤r≤R2,θ1≤θ≤θ2},(x,y)∈D={(r,θ)|R1≤r≤R2,θ1≤θ≤θ2}, with 0≤R1<R20≤R1<R2 and 0≤θ1<θ2≤2π.0≤θ1<θ2≤2π. Show that ∬Df(x,y)dA=12(R22−R12)[H(θ2)−H(θ1)],∬Df(x,y)dA=12(R22−R12)[H(θ2)−H(θ1)], where HH is an antiderivative of h.h.

175.

Apply the preceding exercise to calculate the integral ∬Dy2x2dA,∬Dy2x2dA, where D={(r,θ)|1≤r≤2,π6≤θ≤π3}.D={(r,θ)|1≤r≤2,π6≤θ≤π3}.

176.

Let ff be a continuous function that can be expressed in polar coordinates as a product of a function of rr only and function of θθ only; that is, f(x,y)=g(r)h(θ),f(x,y)=g(r)h(θ), where (x,y)∈D={(r,θ)|R1≤r≤R2,θ1≤θ≤θ2}(x,y)∈D={(r,θ)|R1≤r≤R2,θ1≤θ≤θ2} with 0≤R1<R20≤R1<R2 and 0≤θ1<θ2≤2π.0≤θ1<θ2≤2π. Show that ∬Df(x,y)dA=[G(R2)−G(R1)][H(θ2)−H(θ1)],∬Df(x,y)dA=[G(R2)−G(R1)][H(θ2)−H(θ1)], where G(r)G(r) and H(θ)H(θ) are antiderivatives of rg(r)rg(r) and h(θ)h(θ), respectively.

177.

Evaluate ∬Darctan(yx)x2+y2dA,∬Darctan(yx)x2+y2dA, where D={(r,θ)|2≤r≤3,π4≤θ≤π3}.D={(r,θ)|2≤r≤3,π4≤θ≤π3}.

178.

A spherical cap is the region of a sphere that lies above or below a given plane.

  1. Show that the volume of the spherical cap in the figure below is 16πh(3a2+h2).16πh(3a2+h2).
  2. A spherical segment is the solid defined by intersecting a sphere with two parallel planes. If the distance between the planes is h,h, show that the volume of the spherical segment in the figure below is 16πh(3a2+3b2+h2).16πh(3a2+3b2+h2).
179.

In statistics, the joint density for two independent, normally distributed events with a mean μ=0μ=0 and a standard distribution σσ is defined by p(x,y)=12πσ2e−x2+y22σ2.p(x,y)=12πσ2e−x2+y22σ2. Consider (X,Y),(X,Y), the Cartesian coordinates of a ball in the resting position after it was released from a position on the z-axis toward the xyxy-plane. Assume that the coordinates of the ball are independently normally distributed with a mean μ=0μ=0 and a standard deviation of σσ (in feet). The probability that the ball will stop no more than aa feet from the origin is given by P[X2+Y2≤a2]=∬Dp(x,y)dydx,P[X2+Y2≤a2]=∬Dp(x,y)dydx, where DD is the disk of radius a centered at the origin. Show that P[X2+Y2≤a2]=1−e−a2/2σ2.P[X2+Y2≤a2]=1−e−a2/2σ2.

180.

The double improper integral ∫−∞∞∫−∞∞e−(x2+y2)/2dydx∫−∞∞∫−∞∞e−(x2+y2)/2dydx may be defined as the limit value of the double integrals ∬Dae−(x2+y2)/2dA∬Dae−(x2+y2)/2dA over disks DaDa of radii a centered at the origin, as a increases without bound; that is, ∫−∞∞∫−∞∞e−(x2+y2)/2dydx=lima→∞∬Dae−(x2+y2)/2dA.∫−∞∞∫−∞∞e−(x2+y2)/2dydx=lima→∞∬Dae−(x2+y2)/2dA.

  1. Use polar coordinates to show that ∫−∞∞∫−∞∞e−(x2+y2)/2dydx=2π.∫−∞∞∫−∞∞e−(x2+y2)/2dydx=2π.
  2. Show that ∫−∞∞e−x2/2dx=2π,∫−∞∞e−x2/2dx=2π, by using the relation ∫−∞∞∫−∞∞e−(x2+y2)/2dydx=(∫−∞∞e−x2/2dx)(∫−∞∞e−y2/2dy).∫−∞∞∫−∞∞e−(x2+y2)/2dydx=(∫−∞∞e−x2/2dx)(∫−∞∞e−y2/2dy).
Citation/Attribution
Reuse and redistribution of this content in digital or print format:
  • This book may not be used in the training of large language models or otherwise be ingested into large language models or generative AI offerings without OpenStax's prior written permission.
  • This book uses the Creative Commons Attribution-NonCommercial-ShareAlike License, which means that you can reuse and modify the material only for noncommercial purposes, must attribute OpenStax, and must distribute any derivative works under the same license.
  • Any commercial printing of this textbook, including using a local or custom printer, must be approved by OpenStax, and proper citation provided.
  • OpenStax-copyrighted images, activities, assessments, and similar components of this book are subject to the same licensing – CC-BY-NC-SA. They can be used for noncommercial purposes with attribution. Commercial use requires permission.
  • Permission requests: Anyone who intends to incorporate this content (including text, images, and other components) into large language models, use it in AI offerings, use it commercially (including in print), and/or has questions about another use case is welcome to complete our reuse request form.
Attribution information
  • If you are redistributing all or part of this book in a noncommercial print format, then you must include on every physical page the following attribution:

    Access for free at https://openstax.org/books/calculus-volume-3/pages/1-introduction

  • If you are redistributing all or part of this book in a noncommercial digital format, then for every page that includes OpenStax content, you must license the derivative work under the same CC-BY-NC-SA license as the original, and include on every digital page view the following attribution:

    Access for free at https://openstax.org/books/calculus-volume-3/pages/1-introduction

Citation information

The information below includes the information needed to generate citations in most major styles (APA, MLA, etc.); you must reformat and organize the information as needed to fit the requirements of the style. Use the information below to generate a citation. We recommend using a citation tool such as this one.

© Jul 15, 2026 OpenStax. Textbook content produced by OpenStax is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike License. The OpenStax name, OpenStax logo, OpenStax book covers, OpenStax CNX name, and OpenStax CNX logo, and Rice University name, and Rice University logo trademarks, or wordmarks are not subject to the Creative Commons license and may not be reproduced without the prior and express written consent of Rice University.