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16 MULTIPLE INTEGRALS

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<strong>16</strong>.7 TRIPLE <strong>INTEGRALS</strong> IN CYLINDRICAL COORDINATES<br />

TRANSPARENCY AVAILABLE<br />

#52 (Figure 7)<br />

SUGGESTED TIME AND EMPHASIS<br />

1<br />

2<br />

–1 class Essential material<br />

POINTS TO STRESS<br />

1. The cylindrical coordinate system as an extension of polar coordinates in R 2 .<br />

2. The basic shapes of cylindrical solids.<br />

3. The idea that the cylindrical coordinate system can be used to simplify equations and volume integrals of<br />

certain three-dimensional surfaces and solids.<br />

QUIZ QUESTIONS<br />

• Text Question: Does the region of Example 3 have an axis of symmetry? If so, what does it say about<br />

the choice of using cylindrical coordinates?<br />

Answer: The solid is symmetric about the z-axis, which implies that cylindrical coordinates should be<br />

considered.<br />

• Drill Question: Describe in your own words the surface given by the equation r = θ, 0≤ θ ≤ 6π in<br />

cylindrical coordinates.<br />

Answer: It looks something like a rolled-up piece of paper.<br />

MATERIALS FOR LECTURE<br />

• Compute the intersection of the surfaces z = x 2 + y 2 and z = x, first in rectangular coordinates, then in<br />

cylindrical coordinates. (Here is a case where the rectangular coordinates are the easiest to visualize, even<br />

though there is an x 2 + y 2 term.)<br />

• Point out that while<br />

lim<br />

(x,y)→(0,0)<br />

this, use cylindrical coordinates to get<br />

approaches 0, as seen in Section 14.2.<br />

xy<br />

x 2 does not exist,<br />

+ y2 lim<br />

(x,y,z)→(0,0,0)<br />

xyz<br />

x 2 + y 2 does exist. To see<br />

+ z2 xyz<br />

x 2 + y 2 + z 2 = r2 z sin θ cos θ<br />

r 2 + z 2 , and compare to<br />

r 2 z<br />

r 2 + z 2 ,which<br />

• Convert a typical cylindrical volume integral of a solid S computed using double integrals into a triple<br />

integral:<br />

V = ∫∫ R f (r, θ) rdrdθ = ∫ β∫ h2 (θ)<br />

α h 1 (θ) f (r, θ) rdrdθ = ∫ β∫ h2 (θ) ∫ f (r,θ)<br />

α h 1 (θ) 0<br />

rdzdrdθ<br />

912

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