Post on 01-Jun-2020
Triple Integrals
Triple Integrals
Just as we defined single integrals for functions of one variable and doubleintegrals for functions of two variables, so we can define triple integrals forfunctions of three variables. Let’s first deal with the simplest case where fis defined on a rectangular box:
B = {(x, y, z)|a ≤ x ≤ b, c ≤ y ≤ d, r ≤ z ≤ s}.
MAT 1002 Calculus II 1 / 36
Triple Integrals
Triple Integrals � � � � � � � � � � � � � � � �
Just as we defined single integrals for functions of one variable and double integralsfor functions of two variables, so we can define triple integrals for functions of threevariables. Let’s first deal with the simplest case where is defined on a rectangular box:
The first step is to divide B into sub-boxes. We do this by dividing the interval into l subintervals of equal width , dividing into m subintervals ofwidth , and dividing into n subintervals of width . The planes through theendpoints of these subintervals parallel to the coordinate planes divide the box into
sub-boxes
which are shown in Figure 1. Each sub-box has volume .Then we form the triple Riemann sum
where the sample point is in . By analogy with the definition of adouble integral (12.1.5), we define the triple integral as the limit of the triple Riemannsums in (2).
Definition The triple integral of over the box is
if this limit exists.
Again, the triple integral always exists if is continuous. We can choose the samplepoint to be any point in the sub-box, but if we choose it to be the point weget a simpler-looking expression for the triple integral:
Just as for double integrals, the practical method for evaluating triple integrals is toexpress them as iterated integrals as follows.
Fubini’s Theorem for Triple Integrals If is continuous on the rectangular box, then
yyyB
f �x, y, z� dV � ys
r y
d
c y
b
a f �x, y, z� dx dy dz
B � �a, b� � �c, d � � �r, s�f4
yyyB
f �x, y, z� dV � lim l, m, n l �
�l
i�1 �
m
j�1 �
n
k�1 f �xi, yj, zk � �V
�xi, yj, zk �f
yyyB
f �x, y, z� dV � lim l, m, n l �
�l
i�1 �
m
j�1 �
n
k�1 f �xi jk* , yi jk* , zi jk* � �V
Bf3
Bi jk�xi jk* , yi jk* , zi jk* �
�l
i�1 �
m
j�1 �
n
k�1 f �xijk* , yijk* , zijk* � �V2
�V � �x �y �z
Bi jk � �xi�1, xi� � �yj�1, yj� � �zk�1, zk�
lmnB
�z�r, s��y�c, d ��x�xi�1, xi �
�a, b�
B � ��x, y, z� a � x � b, c � y � d, r � z � s1
f
12.7
SECTION 12.7 TRIPLE INTEGRALS � 883
FIGURE 1
z
yx
B
z
yx
Bijk
ÎxÎy
Îz
The first step is to divide B into sub-boxes.We do this by dividing the interval [a, b] intol subintervals [xi−1, xi] of equal width ∆x,dividing [c, d] into m subintervals of width∆y, and dividing [r, s] into n subintervalsof width ∆z. The planes through the end-points of these subintervals parallel to thecoordinate planes divide the box B into lmnsub-boxes
Bijk = [xi−1, xi]× [yi−1, yi]× [zi−1, zi].
Each sub-box has volume ∆V = ∆x∆y∆z.
MAT 1002 Calculus II 2 / 36
Triple Integrals
Then we form the triple Riemann sum
l∑i=1
m∑j=1
n∑k=1
f(x∗ijk, y∗ijk, z
∗ijk)∆V
where the sample point (x∗ijk, y∗ijk, z
∗ijk) is in Bijk. By analogy with the
definition of a double integral, we define the triple integral as the limit ofthe triple Riemann sums.
Definition 1
The triple integral of f over the box B is∫∫∫Bf(x, y, z)dV = lim
l,m,n→∞
l∑i=1
m∑j=1
n∑k=1
f(x∗ijk, y∗ijk, z
∗ijk)∆V
if limit exists.
MAT 1002 Calculus II 3 / 36
Triple Integrals
Just as for double integrals, the practical method for evaluating tripleintegrals is to express them as iterated integrals as follows.
Theorem 2 (Fubini’s Theorem for Triple Integrals)
If f is continuous on the rectangular box B = [a, b]× [c, d]× [r, s], then∫∫∫Bf(x, y, z)dV =
∫ b
a
∫ d
c
∫ s
rf(x, y, z)dxdydz
MAT 1002 Calculus II 4 / 36
Triple Integrals
The iterated integral on the right side of Fubini’s Theorem means that weintegrate first with respect to x (keeping y and z fixed), then we integratewith respect to y (keeping z fixed), and finally we integrate with respectto z. There are five other possible orders in which we can integrate, all ofwhich give the same value. For instance, if we integrate with respect to y,then z, and then x, we have∫∫∫
Bf(x, y, z)dV =
∫ d
c
∫ s
r
∫ b
af(x, y, z)dydzdx
MAT 1002 Calculus II 5 / 36
Triple Integrals
Example 3
Evaluate the triple integral
∫∫∫Bxyz2dV , where B is the rectangular box
given by B = {(x, y, z)|0 ≤ x ≤ 0,−1 ≤ y ≤ 2, 0 ≤ z ≤ 3}.
Solution.
We could use any of the six possible orders of integration. If we choose tointegrate with respect to x, then y, and then z, we obtain∫∫∫
Bxyz2dV =
∫ 3
0
∫ 2
−1
∫ 1
0xyz2dxdydz =
∫ 3
0
∫ 2
−1
[x2yz2
2
]x=1
x=0
dydz
=
∫ 3
0
∫ 2
−1
[yz2
2
]dydz =
∫ 3
0
[y2z2
4
]y=2
y=−1dz
=
∫ 3
0
[3z2
4
]dz =
[z3
4
]=
27
4.
MAT 1002 Calculus II 6 / 36
Triple Integrals
Now we define the triple integral over a general bounded region E inthree-dimensional space (a solid) by much the same procedure that weused for double integrals. We enclose E in a rectangular box B. Then wedefine a function F so that it agrees with f on E but is 0 for points in Bthat are outside E. By definition,∫∫∫
Ef(x, y, z)dV =
∫∫∫Bf(x, y, z)dV.
MAT 1002 Calculus II 7 / 36
Triple Integrals
We restrict our attention to continuous functions f and to certain simpletypes of regions. A solid region E is said to be of Type 1 if it lies betweenthe graphs of two continuous functions of x and y, that is,
E = {(x, y, z)|(x, y) ∈ D,u1(x, y) ≤ z ≤ u2(x, y)}
where D is the projection of E onto the xy-plane as shown in Figure.Notice that the upper boundary of the solid E is the surface with equationz = u2(x, y), while the lower boundary is the surface z = u1(x, y).
The iterated integral on the right side of Fubini’s Theorem means that we integratefirst with respect to (keeping and fixed), then we integrate with respect to (keep-ing fixed), and finally we integrate with respect to . There are five other possibleorders in which we can integrate, all of which give the same value. For instance, if weintegrate with respect to , then , and then , we have
EXAMPLE 1 Evaluate the triple integral , where is the rectangular boxgiven by
SOLUTION We could use any of the six possible orders of integration. If we choose tointegrate with respect to , then , and then , we obtain
Now we define the triple integral over a general bounded region E in three-dimensional space (a solid) by much the same procedure that we used for double integrals (12.3.2). We enclose in a box of the type given by Equation 1. Then wedefine a function so that it agrees with on but is 0 for points in that are out-side . By definition,
This integral exists if is continuous and the boundary of is “reasonably smooth.”The triple integral has essentially the same properties as the double integral (Proper-ties 6–9 in Section 12.3).
We restrict our attention to continuous functions and to certain simple types ofregions. A solid region is said to be of type 1 if it lies between the graphs of twocontinuous functions of and , that is,
where is the projection of onto the -plane as shown in Figure 2. Notice that theupper boundary of the solid is the surface with equation , while thelower boundary is the surface .
By the same sort of argument that led to (12.3.3), it can be shown that if is a type 1 region given by Equation 5, then
yyyE
f �x, y, z� dV � yyD
yu2�x, y�
u1�x, y� f �x, y, z� dz� dA6
Ez � u1�x, y�
z � u2�x, y�ExyED
E � ��x, y, z� �x, y� � D, u1�x, y� � z � u2�x, y�5
yxE
f
Ef
yyyE
f �x, y, z� dV � yyyB
F�x, y, z� dV
EBEfF
BE
� y3
0 3z2
4 dz �
z3
4 �0
3
�27
4
� y3
0 y
2
�1 yz2
2 dy dz � y
3
0
y 2z2
4 �y��1
y�2
dz
yyyB
xyz2 dV � y3
0 y
2
�1 y
1
0 xyz2 dx dy dz � y
3
0
y2
�1
x 2yz2
2 �x�0
x�1
dy dz
zyx
B � ��x, y, z� 0 � x � 1, �1 � y � 2, 0 � z � 3
BxxxB xyz2 dV
yyyB
f �x, y, z� dV � yb
a y
s
r y
d
c f �x, y, z� dy dz dx
xzy
zzyzyx
884 � CHAPTER 12 MULTIPLE INTEGRALS
FIGURE 2A type 1 solid region
z
0
xyD
E
z=u™ (x, y)
z=u¡ (x, y)
MAT 1002 Calculus II 8 / 36
Triple Integrals
It can be shown that if E is a Type 1 region, then∫∫∫Ef(x, y, z)dV =
∫∫D
[∫ u2(x,y)
u1(x,y)f(x, y, z)dz
]dA.
The meaning of the inner integral on the right side is that x and y are heldfixed, and therefore u1(x, y) and u2(x, y) are regarded as constants, whilef(x, y, z) is integrated with respect to z.
MAT 1002 Calculus II 9 / 36
Triple Integrals
The meaning of the inner integral on the right side of Equation 6 is that and areheld fixed, and therefore and are regarded as constants, while is integrated with respect to .
In particular, if the projection of onto the -plane is a type I plane region (asin Figure 3), then
and Equation 6 becomes
If, on the other hand, is a type II plane region (as in Figure 4), then
and Equation 6 becomes
EXAMPLE 2 Evaluate , where is the solid tetrahedron bounded by the fourplanes , , , and .
SOLUTION When we set up a triple integral it’s wise to draw two diagrams: one of the solid region (see Figure 5) and one of its projection on the -plane (see Figure 6). The lower boundary of the tetrahedron is the plane and the upper boundary is the plane (or ), so we use and in Formula 7. Notice that the planes and
intersect in the line (or ) in the -plane. So the projec-tion of is the triangular region shown in Figure 6, and we have
This description of as a type 1 region enables us to evaluate the integral as follows:
� 16 y
1
0 �1 � x�3 dx �
1
6 �
�1 � x�4
4 �0
1
�1
24
� 12 y
1
0
��1 � x � y�3
3 �y�0
y�1�x
dx
� 12 y
1
0 y
1�x
0 �1 � x � y�2 dy dx
� y1
0
y1�x
0
z2
2 �z�0
z�1�x�y
dy dx yyyE
z dV � y1
0 y
1�x
0 y
1�x�y
0 z dz dy dx
E
E � ��x, y, z� 0 � x � 1, 0 � y � 1 � x, 0 � z � 1 � x � y9
Exyy � 1 � xx � y � 1z � 0
x � y � z � 1u2�x, y� � 1 � x � yu1�x, y� � 0z � 1 � x � yx � y � z � 1
z � 0xyDE
x � y � z � 1z � 0y � 0x � 0Exxx
E z dV
yyyE
f �x, y, z� dV � yd
c y
h2� y�
h1� y� y
u2�x, y�
u1�x, y� f �x, y, z� dz dx dy8
E � ��x, y, z� c � y � d, h1�y� � x � h2�y�, u1�x, y� � z � u2�x, y�
D
yyyE
f �x, y, z� dV � yb
a y
t2�x�
t1�x� y
u2�x, y�
u1�x, y� f �x, y, z� dz dy dx7
E � ��x, y, z� a � x � b, t1�x� � y � t2�x�, u1�x, y� � z � u2�x, y�
xyEDz
f �x, y, z�u2�x, y�u1�x, y�yx
SECTION 12.7 TRIPLE INTEGRALS � 885
FIGURE 3A type 1 solid region
z=u¡(x, y)
z=u™(x, y)
y=g™(x)y=g¡(x)
z
0
yx
a
D
E
b
FIGURE 4Another type 1 solid region
x
0
z
y
c d
z=u™(x, y)
x=h™(y)
x=h¡(y)
z=u¡(x, y)E
D
FIGURE 5
x
0
z
y(1, 0, 0)
(0, 1, 0)
(0, 0, 1)
E
z=1-x-y
z=0
0
y
1
x1y=0
y=1-x
D
FIGURE 6
In particular, if the projection D of E onto the xy-plane is a Type I planeregion, then
E = {(x, y, z)|a ≤ x ≤ b, g1(x) ≤ y ≤ g2(x), u1(x, y) ≤ z ≤ u2(x, y)}
and ∫∫∫Ef(x, y, z)dV =
∫ b
a
∫ g2(x)
g1(x)
∫ u2(x,y)
u1(x,y)f(x, y, z)dzdydx.
MAT 1002 Calculus II 10 / 36
Triple Integrals
Example 4
Evaluate
∫∫∫EzdV , where E is the solid tetrahedron bounded by the four
planes x = 0, y = 0, z = 0, and x+ y + z = 1.
Solution.
The meaning of the inner integral on the right side of Equation 6 is that and areheld fixed, and therefore and are regarded as constants, while is integrated with respect to .
In particular, if the projection of onto the -plane is a type I plane region (asin Figure 3), then
and Equation 6 becomes
If, on the other hand, is a type II plane region (as in Figure 4), then
and Equation 6 becomes
EXAMPLE 2 Evaluate , where is the solid tetrahedron bounded by the fourplanes , , , and .
SOLUTION When we set up a triple integral it’s wise to draw two diagrams: one of the solid region (see Figure 5) and one of its projection on the -plane (see Figure 6). The lower boundary of the tetrahedron is the plane and the upper boundary is the plane (or ), so we use and in Formula 7. Notice that the planes and
intersect in the line (or ) in the -plane. So the projec-tion of is the triangular region shown in Figure 6, and we have
This description of as a type 1 region enables us to evaluate the integral as follows:
� 16 y
1
0 �1 � x�3 dx �
1
6 �
�1 � x�4
4 �0
1
�1
24
� 12 y
1
0
��1 � x � y�3
3 �y�0
y�1�x
dx
� 12 y
1
0 y
1�x
0 �1 � x � y�2 dy dx
� y1
0
y1�x
0
z2
2 �z�0
z�1�x�y
dy dx yyyE
z dV � y1
0 y
1�x
0 y
1�x�y
0 z dz dy dx
E
E � ��x, y, z� 0 � x � 1, 0 � y � 1 � x, 0 � z � 1 � x � y9
Exyy � 1 � xx � y � 1z � 0
x � y � z � 1u2�x, y� � 1 � x � yu1�x, y� � 0z � 1 � x � yx � y � z � 1
z � 0xyDE
x � y � z � 1z � 0y � 0x � 0Exxx
E z dV
yyyE
f �x, y, z� dV � yd
c y
h2� y�
h1� y� y
u2�x, y�
u1�x, y� f �x, y, z� dz dx dy8
E � ��x, y, z� c � y � d, h1�y� � x � h2�y�, u1�x, y� � z � u2�x, y�
D
yyyE
f �x, y, z� dV � yb
a y
t2�x�
t1�x� y
u2�x, y�
u1�x, y� f �x, y, z� dz dy dx7
E � ��x, y, z� a � x � b, t1�x� � y � t2�x�, u1�x, y� � z � u2�x, y�
xyEDz
f �x, y, z�u2�x, y�u1�x, y�yx
SECTION 12.7 TRIPLE INTEGRALS � 885
FIGURE 3A type 1 solid region
z=u¡(x, y)
z=u™(x, y)
y=g™(x)y=g¡(x)
z
0
yx
a
D
E
b
FIGURE 4Another type 1 solid region
x
0
z
y
c d
z=u™(x, y)
x=h™(y)
x=h¡(y)
z=u¡(x, y)E
D
FIGURE 5
x
0
z
y(1, 0, 0)
(0, 1, 0)
(0, 0, 1)
E
z=1-x-y
z=0
0
y
1
x1y=0
y=1-x
D
FIGURE 6
When we set up a triple integral it’s wise todraw two diagrams: one of the solid region Eand one of its projection D on the xy-plane.The lower boundary of the tetrahedron is theplane z = 0 and the upper boundary is theplane x+ y + z = 1, so we use u1(x, y) = 0and u2(x, y) = 1− x− y.
MAT 1002 Calculus II 11 / 36
Triple Integrals
Solution.
Notice that the planes x+ y + z = 1 and z = 0 intersect in the linex+ y = 1 in the xy-plane. So the projection of E is the triangular regionshown in Figure, and we have
E = {(x, y, z)|0 ≤ x ≤ 1, 0 ≤ y ≤ 1− x, 0 ≤ z ≤ 1− x− y} .
The meaning of the inner integral on the right side of Equation 6 is that and areheld fixed, and therefore and are regarded as constants, while is integrated with respect to .
In particular, if the projection of onto the -plane is a type I plane region (asin Figure 3), then
and Equation 6 becomes
If, on the other hand, is a type II plane region (as in Figure 4), then
and Equation 6 becomes
EXAMPLE 2 Evaluate , where is the solid tetrahedron bounded by the fourplanes , , , and .
SOLUTION When we set up a triple integral it’s wise to draw two diagrams: one of the solid region (see Figure 5) and one of its projection on the -plane (see Figure 6). The lower boundary of the tetrahedron is the plane and the upper boundary is the plane (or ), so we use and in Formula 7. Notice that the planes and
intersect in the line (or ) in the -plane. So the projec-tion of is the triangular region shown in Figure 6, and we have
This description of as a type 1 region enables us to evaluate the integral as follows:
� 16 y
1
0 �1 � x�3 dx �
1
6 �
�1 � x�4
4 �0
1
�1
24
� 12 y
1
0
��1 � x � y�3
3 �y�0
y�1�x
dx
� 12 y
1
0 y
1�x
0 �1 � x � y�2 dy dx
� y1
0
y1�x
0
z2
2 �z�0
z�1�x�y
dy dx yyyE
z dV � y1
0 y
1�x
0 y
1�x�y
0 z dz dy dx
E
E � ��x, y, z� 0 � x � 1, 0 � y � 1 � x, 0 � z � 1 � x � y9
Exyy � 1 � xx � y � 1z � 0
x � y � z � 1u2�x, y� � 1 � x � yu1�x, y� � 0z � 1 � x � yx � y � z � 1
z � 0xyDE
x � y � z � 1z � 0y � 0x � 0Exxx
E z dV
yyyE
f �x, y, z� dV � yd
c y
h2� y�
h1� y� y
u2�x, y�
u1�x, y� f �x, y, z� dz dx dy8
E � ��x, y, z� c � y � d, h1�y� � x � h2�y�, u1�x, y� � z � u2�x, y�
D
yyyE
f �x, y, z� dV � yb
a y
t2�x�
t1�x� y
u2�x, y�
u1�x, y� f �x, y, z� dz dy dx7
E � ��x, y, z� a � x � b, t1�x� � y � t2�x�, u1�x, y� � z � u2�x, y�
xyEDz
f �x, y, z�u2�x, y�u1�x, y�yx
SECTION 12.7 TRIPLE INTEGRALS � 885
FIGURE 3A type 1 solid region
z=u¡(x, y)
z=u™(x, y)
y=g™(x)y=g¡(x)
z
0
yx
a
D
E
b
FIGURE 4Another type 1 solid region
x
0
z
y
c d
z=u™(x, y)
x=h™(y)
x=h¡(y)
z=u¡(x, y)E
D
FIGURE 5
x
0
z
y(1, 0, 0)
(0, 1, 0)
(0, 0, 1)
E
z=1-x-y
z=0
0
y
1
x1y=0
y=1-x
D
FIGURE 6
This description of E as a Type 1 region enables us toevaluate the integral as follows:∫∫∫
Ef(x, y, z)dV =
∫ 1
0
∫ 1−x
0
∫ 1−x−y
0zdzdydx
=1
2
∫ 1
0
∫ 1−x
0(1− x− y)2dydx
=1
6
∫ 1
0(1− x)3dx =
1
24.
MAT 1002 Calculus II 12 / 36
Triple Integrals
A solid region E is of Type 2 if it is of the form
E = {(x, y, z)|(y, z) ∈ D,u1(y, z) ≤ x ≤ u2(y, z)}where, this time, D is the projection of E onto the yz-plane. The backsurface is x = u1(y, z), the front surface is x = u2(y, z), and we have∫∫∫
Ef(x, y, z)dV =
∫∫D
[∫ u2(y,z)
u1(y,z)f(x, y, z)dx
]dA.
A solid region is of type 2 if it is of the form
where, this time, is the projection of onto the -plane (see Figure 7). The backsurface is , the front surface is , and we have
Finally, a type 3 region is of the form
where is the projection of onto the -plane, is the left surface, andis the right surface (see Figure 8). For this type of region we have
In each of Equations 10 and 11 there may be two possible expressions for the inte-gral depending on whether is a type I or type II plane region (and corresponding toEquations 7 and 8).
EXAMPLE 3 Evaluate , where is the region bounded by the parab-oloid and the plane .
SOLUTION The solid is shown in Figure 9. If we regard it as a type 1 region, then weneed to consider its projection onto the -plane, which is the parabolic region inFigure 10. (The trace of in the plane is the parabola .)
From we obtain , so the lower boundary surface of is and the upper surface is . Therefore, the descriptionof as a type 1 region is
and so we obtain
yyyE
sx 2 � z 2 dV � y2
�2 y
4
x2 y
sy�x 2
�sy�x2 sx 2 � z 2 dz dy dx
E � {�x, y, z� �2 � x � 2, x 2 � y � 4, �sy � x 2 � z � sy � x 2}
Ez � sy � x 2z � �sy � x 2
Ez � �sy � x 2y � x 2 � z2
x0
y
y=4
y=≈
D¡
FIGURE 10Projection on xy-plane
FIGURE 9Region of integration
x
0
z
y4
y=≈+z@
E
y � x 2z � 0y � x 2 � z2xyD1
E
y � 4y � x 2 � z2ExxxE sx 2 � z 2 dV
D
yyyE
f �x, y, z� dV � yyD
yu2�x, z�
u1�x, z� f �x, y, z� dy� dA11
y � u2�x, z�y � u1�x, z�xzED
E � ��x, y, z� �x, z� � D, u1�x, z� � y � u2�x, z�
yyyE
f �x, y, z� dV � yyD
yu2� y, z�
u1� y, z� f �x, y, z� dx� dA10
x � u2�y, z�x � u1�y, z�yzED
E � ��x, y, z� �y, z� � D, u1�y, z� � x � u2�y, z�
E
886 � CHAPTER 12 MULTIPLE INTEGRALS
0
z
yx E
D
x=u¡(y, z)
x=u™(y, z)
FIGURE 7A type 2 region
FIGURE 8A type 3 region
x
0
z
yy=u¡(x, z)
DE
y=u™(x, z)
MAT 1002 Calculus II 13 / 36
Triple Integrals
Finally Type 3 region is of the form
E = {(x, y, z)|(x, z) ∈ D,u1(x, z) ≤ y ≤ u2(x, z)}where, this time, D is the projection of E onto the xz-plane. The leftsurface is y = u1(x, z), the right surface is y = u2(x, z), and we have∫∫∫
Ef(x, y, z)dV =
∫∫D
[∫ u2(x,z)
u1(x,z)f(x, y, z)dy
]dA.
A solid region is of type 2 if it is of the form
where, this time, is the projection of onto the -plane (see Figure 7). The backsurface is , the front surface is , and we have
Finally, a type 3 region is of the form
where is the projection of onto the -plane, is the left surface, andis the right surface (see Figure 8). For this type of region we have
In each of Equations 10 and 11 there may be two possible expressions for the inte-gral depending on whether is a type I or type II plane region (and corresponding toEquations 7 and 8).
EXAMPLE 3 Evaluate , where is the region bounded by the parab-oloid and the plane .
SOLUTION The solid is shown in Figure 9. If we regard it as a type 1 region, then weneed to consider its projection onto the -plane, which is the parabolic region inFigure 10. (The trace of in the plane is the parabola .)
From we obtain , so the lower boundary surface of is and the upper surface is . Therefore, the descriptionof as a type 1 region is
and so we obtain
yyyE
sx 2 � z 2 dV � y2
�2 y
4
x2 y
sy�x 2
�sy�x2 sx 2 � z 2 dz dy dx
E � {�x, y, z� �2 � x � 2, x 2 � y � 4, �sy � x 2 � z � sy � x 2}
Ez � sy � x 2z � �sy � x 2
Ez � �sy � x 2y � x 2 � z2
x0
y
y=4
y=≈
D¡
FIGURE 10Projection on xy-plane
FIGURE 9Region of integration
x
0
z
y4
y=≈+z@
E
y � x 2z � 0y � x 2 � z2xyD1
E
y � 4y � x 2 � z2ExxxE sx 2 � z 2 dV
D
yyyE
f �x, y, z� dV � yyD
yu2�x, z�
u1�x, z� f �x, y, z� dy� dA11
y � u2�x, z�y � u1�x, z�xzED
E � ��x, y, z� �x, z� � D, u1�x, z� � y � u2�x, z�
yyyE
f �x, y, z� dV � yyD
yu2� y, z�
u1� y, z� f �x, y, z� dx� dA10
x � u2�y, z�x � u1�y, z�yzED
E � ��x, y, z� �y, z� � D, u1�y, z� � x � u2�y, z�
E
886 � CHAPTER 12 MULTIPLE INTEGRALS
0
z
yx E
D
x=u¡(y, z)
x=u™(y, z)
FIGURE 7A type 2 region
FIGURE 8A type 3 region
x
0
z
yy=u¡(x, z)
DE
y=u™(x, z)
MAT 1002 Calculus II 14 / 36
Triple Integrals
Example 5
Evaluate
∫∫∫E
√x2 + z2dV , where E is the region bounded by the
paraboloid y = x2 + z2 and the plane y = 4.
Solution.
If we regard the solid E as a Type 1 region, then we need to consider itsprojection D1 onto the xy-plane, which is the parabolic region in theFigure.
A solid region is of type 2 if it is of the form
where, this time, is the projection of onto the -plane (see Figure 7). The backsurface is , the front surface is , and we have
Finally, a type 3 region is of the form
where is the projection of onto the -plane, is the left surface, andis the right surface (see Figure 8). For this type of region we have
In each of Equations 10 and 11 there may be two possible expressions for the inte-gral depending on whether is a type I or type II plane region (and corresponding toEquations 7 and 8).
EXAMPLE 3 Evaluate , where is the region bounded by the parab-oloid and the plane .
SOLUTION The solid is shown in Figure 9. If we regard it as a type 1 region, then weneed to consider its projection onto the -plane, which is the parabolic region inFigure 10. (The trace of in the plane is the parabola .)
From we obtain , so the lower boundary surface of is and the upper surface is . Therefore, the descriptionof as a type 1 region is
and so we obtain
yyyE
sx 2 � z 2 dV � y2
�2 y
4
x2 y
sy�x 2
�sy�x2 sx 2 � z 2 dz dy dx
E � {�x, y, z� �2 � x � 2, x 2 � y � 4, �sy � x 2 � z � sy � x 2}
Ez � sy � x 2z � �sy � x 2
Ez � �sy � x 2y � x 2 � z2
x0
y
y=4
y=≈
D¡
FIGURE 10Projection on xy-plane
FIGURE 9Region of integration
x
0
z
y4
y=≈+z@
E
y � x 2z � 0y � x 2 � z2xyD1
E
y � 4y � x 2 � z2Exxx
E sx 2 � z 2 dV
D
yyyE
f �x, y, z� dV � yyD
yu2�x, z�
u1�x, z� f �x, y, z� dy� dA11
y � u2�x, z�y � u1�x, z�xzED
E � ��x, y, z� �x, z� � D, u1�x, z� � y � u2�x, z�
yyyE
f �x, y, z� dV � yyD
yu2� y, z�
u1� y, z� f �x, y, z� dx� dA10
x � u2�y, z�x � u1�y, z�yzED
E � ��x, y, z� �y, z� � D, u1�y, z� � x � u2�y, z�
E
886 � CHAPTER 12 MULTIPLE INTEGRALS
0
z
yx E
D
x=u¡(y, z)
x=u™(y, z)
FIGURE 7A type 2 region
FIGURE 8A type 3 region
x
0
z
yy=u¡(x, z)
DE
y=u™(x, z)
A solid region is of type 2 if it is of the form
where, this time, is the projection of onto the -plane (see Figure 7). The backsurface is , the front surface is , and we have
Finally, a type 3 region is of the form
where is the projection of onto the -plane, is the left surface, andis the right surface (see Figure 8). For this type of region we have
In each of Equations 10 and 11 there may be two possible expressions for the inte-gral depending on whether is a type I or type II plane region (and corresponding toEquations 7 and 8).
EXAMPLE 3 Evaluate , where is the region bounded by the parab-oloid and the plane .
SOLUTION The solid is shown in Figure 9. If we regard it as a type 1 region, then weneed to consider its projection onto the -plane, which is the parabolic region inFigure 10. (The trace of in the plane is the parabola .)
From we obtain , so the lower boundary surface of is and the upper surface is . Therefore, the descriptionof as a type 1 region is
and so we obtain
yyyE
sx 2 � z 2 dV � y2
�2 y
4
x2 y
sy�x 2
�sy�x2 sx 2 � z 2 dz dy dx
E � {�x, y, z� �2 � x � 2, x 2 � y � 4, �sy � x 2 � z � sy � x 2}
Ez � sy � x 2z � �sy � x 2
Ez � �sy � x 2y � x 2 � z2
x0
y
y=4
y=≈
D¡
FIGURE 10Projection on xy-plane
FIGURE 9Region of integration
x
0
z
y4
y=≈+z@
E
y � x 2z � 0y � x 2 � z2xyD1
E
y � 4y � x 2 � z2Exxx
E sx 2 � z 2 dV
D
yyyE
f �x, y, z� dV � yyD
yu2�x, z�
u1�x, z� f �x, y, z� dy� dA11
y � u2�x, z�y � u1�x, z�xzED
E � ��x, y, z� �x, z� � D, u1�x, z� � y � u2�x, z�
yyyE
f �x, y, z� dV � yyD
yu2� y, z�
u1� y, z� f �x, y, z� dx� dA10
x � u2�y, z�x � u1�y, z�yzED
E � ��x, y, z� �y, z� � D, u1�y, z� � x � u2�y, z�
E
886 � CHAPTER 12 MULTIPLE INTEGRALS
0
z
yx E
D
x=u¡(y, z)
x=u™(y, z)
FIGURE 7A type 2 region
FIGURE 8A type 3 region
x
0
z
yy=u¡(x, z)
DE
y=u™(x, z)
MAT 1002 Calculus II 15 / 36
Triple Integrals
Solution (cont.)
From y = x2 + z2 we obtain z = ∓√y − x2, so the lower boundary
surface of E is z = −√y − x2 and the upper surface is z =
√y − x2.
Therefore, the description of E as a Type 1 region is
E ={
(x, y, z)| − 2 ≤ x ≤ 2, x2 ≤ y ≤ 4,−√y − x2 ≤ z ≤
√y − x2
}and so we obtain∫∫∫
E
√x2 + z2dV =
∫ 2
−2
∫ 4
x2
∫ √y−x2−√y−x2
√x2 + z2dzdydx.
Although this expression is correct, it is extremely difficult to evaluate.
MAT 1002 Calculus II 16 / 36
Triple Integrals
Solution (cont.)Although this expression is correct, it is extremely difficult to evaluate. So let’s
instead consider as a type 3 region. As such, its projection onto the -plane isthe disk shown in Figure 11.
Then the left boundary of is the paraboloid and the right boundaryis the plane , so taking and in Equation 11, wehave
Although this integral could be written as
it’s easier to convert to polar coordinates in the -plane: , .This gives
Applications of Triple Integrals
Recall that if , then the single integral represents the area under thecurve from to , and if , then the double integral represents the volume under the surface and above . The correspondinginterpretation of a triple integral , where , is not veryuseful because it would be the “hypervolume” of a four-dimensional object and, ofcourse, that is very difficult to visualize. (Remember that is just the domain of thefunction ; the graph of lies in four-dimensional space.) Nonetheless, the triple inte-gral can be interpreted in different ways in different physical situa-tions, depending on the physical interpretations of , , and .
Let’s begin with the special case where for all points in . Then thetriple integral does represent the volume of :
For example, you can see this in the case of a type 1 region by putting in Formula 6:
yyyE
1 dV � yyD
yu2�x, y�
u1�x, y� dz� dA � yy
D
�u2�x, y� � u1�x, y�� dA
f �x, y, z� � 1
V�E � � yyyE
dV12
EEf �x, y, z� � 1
f �x, y, z�zyxxxx
E f �x, y, z� dV
ffE
f �x, y, z� � 0xxxE f �x, y, z� dVDz � f �x, y�
xxD f �x, y� dAf �x, y� � 0bay � f �x�x
ba f �x� dxf �x� � 0
� 2� 4r 3
3�
r 5
5 �0
2
�128�
15
� y2�
0 y
2
0 �4 � r 2 �r r dr d� � y
2�
0 d� y
2
0 �4r 2 � r 4 � dr
yyyE
sx 2 � z 2 dV � yyD3
�4 � x 2 � z 2 �sx 2 � z 2 dA
z � r sin �x � r cos �xz
y2
�2 y
s4�x2
�s4�x2 �4 � x 2 � z2 �sx 2 � z 2 dz dx
� yyD3
�4 � x 2 � z 2 �sx 2 � z 2 dA
yyyE
sx 2 � z 2 dV � yyD3
y4
x2�z2 sx 2 � z 2 dy� dA
u2�x, z� � 4u1�x, z� � x 2 � z2y � 4y � x 2 � z2E
x 2 � z2 � 4xzD3E
SECTION 12.7 TRIPLE INTEGRALS � 887
FIGURE 11Projection on xz-plane
x0
z
≈+z@=4
_2 2
D£
| The most difficult step in evaluating atriple integral is setting up an expressionfor the region of integration (such asEquation 9 in Example 2). Rememberthat the limits of integration in the innerintegral contain at most two variables,the limits of integration in the middle integral contain at most one variable,and the limits of integration in the outerintegral must be constants.
Let’s instead consider E as a Type 3 region. As such,its projection D3 onto xz-plane is the disk x2+z2 ≤4 shown in Figure. Then the left boundary of E isthe paraboloid y = x2 + z2 and the right boundaryis the plane y = 4, so taking u1(x, z) = x2 + z2 andu2(x, z) = 4, we have∫∫∫
E
√x2 + z2dV =
∫∫D3
[∫ 4
x2+z2
√x2 + z2dy
]dA
=
∫∫D3
(4− x2 − z2)√x2 + z2dA.
Although this integral could be written as∫ 2
−2
∫ 4−x2
−√4−x2
(4− x2 − z2)√x2 + z2dzdx
MAT 1002 Calculus II 17 / 36
Triple Integrals
Solution (cont.)
it’s easier to convert to polar coordinates in the xz-plane: x = r cos θ,z = r sin θ. This gives∫∫∫
E
√x2 + z2dV =
∫∫D3
(4− x2 − z2)√x2 + z2dA
=
∫ 2π
0
∫ 2
0(4− r2)rrdrdθ
=
∫ 2π
0
∫ 2
0(4r2 − r4)drdθ
=128π
15.
MAT 1002 Calculus II 18 / 36
Triple Integrals Applications of Triple Integrals
Applications of Triple Integrals
Recall that if f(x) ≥ 0, then the single integral∫ ba f(x)dx represents the
area under the curve y = f(x) from a to b, and if f(x, y) ≥ 0, then thedouble integral
∫∫D f(x, y)dA represents the volume under the surface
z = f(x, y) and above D.
The corresponding interpretation of a triple integral∫∫∫
E f(x, y, z)dV ,where f(x, y, z) ≥ 0, is not very useful because it would be the“hypervolume” of a four-dimensional object and, of course, that is verydifficult to visualize. (Remember that E is just the domain of the functionf ; the graph of f lies in four-dimensional space.)
MAT 1002 Calculus II 19 / 36
Triple Integrals Applications of Triple Integrals
Let’s begin with the special case where f(x, y, z) = 1 for all points in E.Then the triple integral does represent the volume of E:∫∫∫
EdV.
For example, you can see this in the case of a Type 1 region by puttingf(x, y, z) = 1 in a triple integral:∫∫∫
E1dV =
∫∫D
[∫ u2(x,y)
u1(x,y)dz
]dA =
∫∫D
[u2(x, y)− u1(x, y)]dA
and from the previous sections we know this represents the volume thatlies between the surfaces z = u1(x, y) and z = u2(x, y).
MAT 1002 Calculus II 20 / 36
Triple Integrals Applications of Triple Integrals
Example 6
Use a triple integral to find the volume of the tetrahedron T bounded bythe planes x+ 2y + z = 2, x = 2y, x = 0, and z = 0.
Solution.
and from Section 12.3 we know this represents the volume that lies between the sur-faces and .
EXAMPLE 4 Use a triple integral to find the volume of the tetrahedron bounded bythe planes , , , and .
SOLUTION The tetrahedron and its projection on the -plane are shown in Figures 12 and 13. The lower boundary of is the plane and the upper boundary is the plane , that is, . Therefore, we have
by the same calculation as in Example 4 in Section 12.3.
(Notice that it is not necessary to use triple integrals to compute volumes. Theysimply give an alternative method for setting up the calculation.)
All the applications of double integrals in Section 12.5 can be immediately ex-tended to triple integrals. For example, if the density function of a solid object thatoccupies the region is , in units of mass per unit volume, at any given point
, then its mass is
and its moments about the three coordinate planes are
Mxy � yyyE
z��x, y, z� dV
Mxz � yyyE
y��x, y, z� dVMyz � yyyE
x��x, y, z� dV14
m � yyyE
��x, y, z� dV13
�x, y, z���x, y, z�E
FIGURE 12 FIGURE 13
y= x2
”1, ’12
x+2y=2 ”or y=1- ’x2
D
y
0
1
x1
(0, 1, 0)
(0, 0, 2)
y
x
0
z
x+2y+z=2x=2y
”1, , 0’12
T
� y1
0 y
1�x�2
x�2 �2 � x � 2y� dy dx � 1
3
V�T� � yyyT
dV � y1
0 y
1�x�2
x�2 y
2�x�2y
0 dz dy dx
z � 2 � x � 2yx � 2y � z � 2z � 0T
xyDT
z � 0x � 0x � 2yx � 2y � z � 2T
z � u2�x, y�z � u1�x, y�
888 � CHAPTER 12 MULTIPLE INTEGRALS
and from Section 12.3 we know this represents the volume that lies between the sur-faces and .
EXAMPLE 4 Use a triple integral to find the volume of the tetrahedron bounded bythe planes , , , and .
SOLUTION The tetrahedron and its projection on the -plane are shown in Figures 12 and 13. The lower boundary of is the plane and the upper boundary is the plane , that is, . Therefore, we have
by the same calculation as in Example 4 in Section 12.3.
(Notice that it is not necessary to use triple integrals to compute volumes. Theysimply give an alternative method for setting up the calculation.)
All the applications of double integrals in Section 12.5 can be immediately ex-tended to triple integrals. For example, if the density function of a solid object thatoccupies the region is , in units of mass per unit volume, at any given point
, then its mass is
and its moments about the three coordinate planes are
Mxy � yyyE
z��x, y, z� dV
Mxz � yyyE
y��x, y, z� dVMyz � yyyE
x��x, y, z� dV14
m � yyyE
��x, y, z� dV13
�x, y, z���x, y, z�E
FIGURE 12 FIGURE 13
y= x2
”1, ’12
x+2y=2 ”or y=1- ’x2
D
y
0
1
x1
(0, 1, 0)
(0, 0, 2)
y
x
0
z
x+2y+z=2x=2y
”1, , 0’12
T
� y1
0 y
1�x�2
x�2 �2 � x � 2y� dy dx � 1
3
V�T� � yyyT
dV � y1
0 y
1�x�2
x�2 y
2�x�2y
0 dz dy dx
z � 2 � x � 2yx � 2y � z � 2z � 0T
xyDT
z � 0x � 0x � 2yx � 2y � z � 2T
z � u2�x, y�z � u1�x, y�
888 � CHAPTER 12 MULTIPLE INTEGRALS
MAT 1002 Calculus II 21 / 36
Triple Integrals Applications of Triple Integrals
Solution (cont.)
The lower boundary of T is the plane z = 0 and upper boundary is theplane x+ 2y + z = 2, that is, z = 2− x− 2y. Therefore, we have
V (T ) =
∫∫∫TdV =
∫ 1
0
∫ 1−x/2
x/2
∫ 2−x−2y
0dzdydx
=
∫ 1
0
∫ 1−x/2
x/2(2− x− 2y)dydx =
1
3.
Notice that it is not necessary to use triple integrals to compute volumes.They simply give an alternative method for setting up the calculation.
MAT 1002 Calculus II 22 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Cylindrical Coordinates
Triple Integrals in Cylindrical and Spherical CoordinatesCylindrical Coordinates
In the cylindrical coordinate system, a point P in three-dimensionalspace is represented by the ordered triple (r, θ, z), where r and θ are polarcoordinates of the projection of P onto xy-plane and z is the directeddistance from the xy-plane to P .
Triple Integrals in Cylindrical and Spherical Coordinates � � � �
We saw in Section 12.4 that some double integrals are easier to evaluate using polarcoordinates. In this section we see that some triple integrals are easier to evaluateusing cylindrical or spherical coordinates.
Cylindrical Coordinates
Recall from Section 9.7 that the cylindrical coordinates of a point are , where, , and are shown in Figure 1. Suppose that is a type 1 region whose projection
on the -plane is conveniently described in polar coordinates (see Figure 2). In par-ticular, suppose that is continuous and
where is given in polar coordinates by
FIGURE 2
0
z
x
yD
r=h¡(¨)
r=h™(¨)
z=u™(x, y)
z=u¡(x, y)
D � ��r, �� � � � � , h1��� � r � h2���
D
E � ��x, y, z� �x, y� � D, u1�x, y� � z � u2�x, y�
fxyD
Ez�r�r, �, z�P
12.8
SECTION 12.8 TRIPLE INTEGRALS IN CYLINDRICAL AND SPHERICAL COORDINATES � 893
Volumes of Hyperspheres
In this project we find formulas for the volume enclosed by a hypersphere in -dimensionalspace.
1. Use a double integral and the trigonometric substitution , together with Formula 64 in the Table of Integrals, to find the area of a circle with radius .
2. Use a triple integral and trigonometric substitution to find the volume of a sphere with radius .
3. Use a quadruple integral to find the hypervolume enclosed by the hyperspherein . (Use only trigonometric substitution and the reduction
formulas for or .)
4. Use an -tuple integral to find the volume enclosed by a hypersphere of radius in -dimensional space . [Hint: The formulas are different for even and odd.]nn�nn
rn
x cosnx dxx sinnx dx�4x 2 � y 2 � z 2 � w 2 � r 2
r
ry � r sin �
n
DiscoveryProject
FIGURE 1
z
0
x
y
P(r, ̈ , z)
r
z¨
To convert from cylindrical to rectangular co-ordinates we use the equations
x = r cos θ y = r sin θ z = z
whereas to convert from rectangular to cylin-drical coordinates we use
r2 = x2 + y2 tan θ =y
xz = z.
MAT 1002 Calculus II 23 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Cylindrical Coordinates
Suppose that E is a Type 1 region whose projection D on the xy-plane isconveniently described in polar coordinates. In particular, suppose that fis continuous and
E = {(x, y, z)|(x, y) ∈ D,u1(x, y) ≤ z ≤ u2(x, y)}where D is given in polar coordinates by
D = {(x, y)|α ≤ θ ≤ β, h1(θ) ≤ r ≤ h2(θ)}.
Triple Integrals in Cylindrical and Spherical Coordinates � � � �
We saw in Section 12.4 that some double integrals are easier to evaluate using polarcoordinates. In this section we see that some triple integrals are easier to evaluateusing cylindrical or spherical coordinates.
Cylindrical Coordinates
Recall from Section 9.7 that the cylindrical coordinates of a point are , where, , and are shown in Figure 1. Suppose that is a type 1 region whose projection
on the -plane is conveniently described in polar coordinates (see Figure 2). In par-ticular, suppose that is continuous and
where is given in polar coordinates by
FIGURE 2
0
z
x
yD
r=h¡(¨)
r=h™(¨)
z=u™(x, y)
z=u¡(x, y)
D � ��r, �� � � � � , h1��� � r � h2���
D
E � ��x, y, z� �x, y� � D, u1�x, y� � z � u2�x, y�
fxyD
Ez�r�r, �, z�P
12.8
SECTION 12.8 TRIPLE INTEGRALS IN CYLINDRICAL AND SPHERICAL COORDINATES � 893
Volumes of Hyperspheres
In this project we find formulas for the volume enclosed by a hypersphere in -dimensionalspace.
1. Use a double integral and the trigonometric substitution , together with Formula 64 in the Table of Integrals, to find the area of a circle with radius .
2. Use a triple integral and trigonometric substitution to find the volume of a sphere with radius .
3. Use a quadruple integral to find the hypervolume enclosed by the hyperspherein . (Use only trigonometric substitution and the reduction
formulas for or .)
4. Use an -tuple integral to find the volume enclosed by a hypersphere of radius in -dimensional space . [Hint: The formulas are different for even and odd.]nn�nn
rn
x cosnx dxx sinnx dx�4x 2 � y 2 � z 2 � w 2 � r 2
r
ry � r sin �
n
DiscoveryProject
FIGURE 1
z
0
x
y
P(r, ̈ , z)
r
z¨
MAT 1002 Calculus II 24 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Cylindrical Coordinates
Then, the formula for triple integration in cylindrical coordinates isgiven by∫∫∫
Ef(x, y, z)dV =
∫ β
α
∫ h2(θ)
h1(θ)
∫ u2(r sin θ)
u1(r cos θ)f(r cos θ, r sin θ, z)rdzdrdθ.
It is worthwhile to use this formula when E is a solid region easilydescribed in cylindrical coordinates, and especially when the functionf(x, y, z) involves the expression x2 + y2.
MAT 1002 Calculus II 25 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Cylindrical Coordinates
Example 7
A solid E lies within the cylinder x2 + y2 = 1, below the plane z = 4, andabove the paraboloid z = 1− x2 − y2. Then, evaluate the integral∫∫∫
E
√x2 + y2dV .
Solution.
We know from Equation 12.7.6 that
But we also know how to evaluate double integrals in polar coordinates. In fact, com-bining Equation 1 with Equation 12.4.3, we obtain
Formula 2 is the formula for triple integration in cylindrical coordinates. It saysthat we convert a triple integral from rectangular to cylindrical coordinates by writing
, , leaving as it is, using the appropriate limits of integrationfor , , and , and replacing by . (Figure 3 shows how to remember this.)It is worthwhile to use this formula when is a solid region easily described in cylin-drical coordinates, and especially when the function involves the expression
.
EXAMPLE 1 A solid lies within the cylinder , below the plane ,and above the paraboloid . (See Figure 4.) The density at any pointis proportional to its distance from the axis of the cylinder. Find the mass of .
SOLUTION In cylindrical coordinates the cylinder is and the paraboloid is, so we can write
Since the density at is proportional to the distance from the -axis, the den-sity function is
where is the proportionality constant. Therefore, from Formula 12.7.13, the massof is
EXAMPLE 2 Evaluate .
SOLUTION This iterated integral is a triple integral over the solid region
E � {�x, y, z� �2 � x � 2, �s4 � x 2 � y � s4 � x 2, sx 2 � y 2 � z � 2}
y2
�2 y
s4�x2
�s4�x2 y
2
sx2�y2 �x 2 � y 2 � dz dy dx
� 2�K r 3 �r 5
5 �0
1
�12�K
5
� y2�
0 y
1
0 Kr 2 �4 � �1 � r 2 �� dr d� � K y
2�
0 d� y
1
0 �3r 2 � r 4 � dr
m � yyyE
Ksx 2 � y 2 dV � y2�
0 y
1
0 y
4
1�r2 �Kr� r dz dr d�
EK
f �x, y, z� � Ksx 2 � y 2 � Kr
z�x, y, z�
E � ��r, �, z� 0 � � � 2�, 0 � r � 1, 1 � r 2 � z � 4
z � 1 � r 2r � 1
Ez � 1 � x 2 � y 2
z � 4x 2 � y 2 � 1E
x 2 � y2f �x, y, z�
Er dz dr d�dV�rz
zy � r sin �x � r cos �
yyyE
f �x, y, z� dV � y
� y
h2���
h1��� y
u2�r cos �, r sin ��
u1�r cos �, r sin �� f �r cos �, r sin �, z� r dz dr d�2
yyyE
f �x, y, z� dV � yyD
yu2�x, y�
u1�x, y� f �x, y, z� dz� dA1
894 � CHAPTER 12 MULTIPLE INTEGRALS
z
dz
drr d¨
d¨
r
z
0
(1, 0, 0)
(0, 0, 1)
(0, 0, 4)
z=4
x
y
z=1-r@
FIGURE 3Volume element in cylindricalcoordinates: dV=r dz dr d¨
FIGURE 4
In cylindrical coordinates the cylinder is r = 1 and theparaboloid is z = 1− r2, so we can write
E = {(x, y, z)|0 ≤ θ ≤ 2π, 0 ≤ r ≤ 1, 1−r2 ≤ z ≤ 4}
Therefore,∫∫∫E
√x2 + y2dV =
∫ 2π
0
∫ 1
0
∫ 4
1−r2rrdzdrdθ
=12π
5
MAT 1002 Calculus II 26 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Cylindrical Coordinates
Example 8
Evaluate
∫ 2
−2
∫ √4−x2−√4−x2
∫ 2
√x2+y2
(x2 + y2)dzdydx.
Solution.
This iterated integral is a triple integral over the solid region
E ={
(x, y, z)| − 2 ≤ x ≤ 2,−√
4− x2 ≤ y ≤√
4− x2,√x2 + y2 ≤ z ≤ 2
}and the projection of E onto the xy-plane is the disk x2 + y2 ≤ 4. The
lower surface of E is the cone z =√x2 + y2 and its upper surface is the
plane z = 2.
MAT 1002 Calculus II 27 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Cylindrical Coordinates
Solution (cont.)
This region has a much simpler description in cylindrical coordinates:
E = {(r, θ, z)|0 ≤ θ ≤ 2π, 0 ≤ r ≤ 2, r ≤ z ≤ 2} .
and the projection of onto the -plane is the disk . The lower sur-face of is the cone and its upper surface is the plane . (SeeFigure 5.) This region has a much simpler description in cylindrical coordinates:
Therefore, we have
Spherical Coordinates
In Section 9.7 we defined the spherical coordinates of a point (see Figure 6)and we demonstrated the following relationships between rectangular coordinates andspherical coordinates:
In this coordinate system the counterpart of a rectangular box is a spherical wedge
where , , and . Although we defined triple integrals bydividing solids into small boxes, it can be shown that dividing a solid into small spher-ical wedges always gives the same result. So we divide into smaller spherical wedges
by means of equally spaced spheres , half-planes , and half-cones. Figure 7 shows that is approximately a rectangular box with dimensions
, (arc of a circle with radius angle ), and (arc of a circlewith radius angle ). So an approximation to the volume of is given by
FIGURE 7
z
0
x
yri=∏i sin ˙k
ri Ψ=∏i sin ˙k Ψ
∏i Î˙
∏i sin ˙k Ψ Î∏
Î˙˙k
Ψ
���� � �� i ��� � �� i sin �k ��� � � i2 sin �k �� �� ��
Eijk��� i sin �k,� i sin �k ����� i,� i ����
Eijk� � �k
� � � j� � � iEijk
E
d � c � � � � � 2�a � 0
E � ���, �, �� a � � � b, � � � � , c � � � d
z � � cos �y � � sin � sin �x � � sin � cos �3
��, �, ��
� 2� [ 12 r 4 �
15 r 5 ]0
2�
16�
5
� y2�
0 d� y
2
0 r 3�2 � r� dr
� y2�
0 y
2
0 y
2
r r 2 r dz dr d�
y2
�2 y
s4�x2
�s4�x2 y
2
sx2�y2 �x 2 � y 2 � dz dy dx � yyy
E
�x 2 � y 2 � dV
E � ��r, �, z� 0 � � � 2�, 0 � r � 2, r � z � 2
z � 2z � sx 2 � y 2Ex 2 � y 2 � 4xyE
SECTION 12.8 TRIPLE INTEGRALS IN CYLINDRICAL AND SPHERICAL COORDINATES � 895
FIGURE 5
z=œ„„„„„≈+¥
z
x 2 y2
z=2
2
z
0
x
y
P(∏, ̈ , ̇ )∏
˙
¨
FIGURE 6Spherical coordinates of P
Therefore, we have∫ 2
−2
∫ √4−x2−√4−x2
∫ 2
√x2+y2
(x2 + y2)dzdydx
=
∫ 2π
0
∫ 2
0
∫ 2
rr2rdzdrdθ
=16π
5.
MAT 1002 Calculus II 28 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Spherical Coordinates
Spherical Coordinates
The spherical coordinates (ρ, θ, φ) of a point P in space are shown inFigure, where ρ = |OP | is the distance from the origin to P , θ is the sameangle as in cylindrical coordinates, and φ is the angle between the positivez-axis and the line segment OP . Note that ρ ≥ 0 and 0 ≤ φ ≤ π.
Spherical Coordinates
The spherical coordinates of a point in space are shown in Figure 5,where is the distance from the origin to , is the same angle as in cylin-drical coordinates, and is the angle between the positive -axis and the line segment
. Note that
The spherical coordinate system is especially useful in problems where there is sym-metry about a point, and the origin is placed at this point. For example, the sphere withcenter the origin and radius has the simple equation (see Figure 6); this is thereason for the name “spherical” coordinates. The graph of the equation is a ver-tical half-plane (see Figure 7), and the equation represents a half-cone with the-axis as its axis (see Figure 8).
The relationship between rectangular and spherical coordinates can be seen fromFigure 9. From triangles and we have
But and , so to convert from spherical to rectangular coordi-nates, we use the equations
Also, the distance formula shows that
We use this equation in converting from rectangular to spherical coordinates.
�2 � x 2 � y 2 � z24
z � � cos �y � � sin � sin x � � sin � cos 3
y � r sin x � r cos
r � � sin �z � � cos �
OPP�OPQ
z� � c
� c� � cc
0 � � � �� � 0
OPz�
P� � � OP �P��, , ��
696 � CHAPTER 9 VECTORS AND THE GEOMETRY OF SPACE
0
z
x
y
FIGURE 6 ∏=c, a sphere FIGURE 8 ˙=c, a half-cone
0
z
c
π/2<c<π
y
x
0
z
c
0<c<π/2
y
x
0
z
c
FIGURE 7 ¨=c, a half-plane
x
y
FIGURE 9
P(x, y, z)P(∏, ¨, ˙)
P ª(x, y, 0)
O
x
y¨
z
y
x
z
˙ ˙
r
∏
Q
FIGURE 5The spherical coordinates of a point
P(∏, ¨, ˙)
O
z
∏
¨
˙
x y
The relationship between rectangular andspherical coordinates can be seen from Figure.From triangles OPQ and OPP ′ we have
z = ρ cosφ r = ρ sinφ.
But, x = r cos θ and y = r sin θ.
MAT 1002 Calculus II 29 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Spherical Coordinates
So to convert from spherical to rectangular coordinates, we use theequations
x = ρ sinφ cos θ y = ρ sinφ sin θ z = ρ cosφ.
Also, the distance formula shows that
ρ2 = x2 + y2 + z2.
We use this equation in converting from rectangular to sphericalcoordinates.
MAT 1002 Calculus II 30 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Spherical Coordinates
In this coordinate system the counterpart of a rectangular box is aspherical wedge
E = {(ρ, θ, φ)|a ≤ ρ ≤ b, α ≤ θ ≤ β, c ≤ φ ≤ d}
where a ≥ 0, β − α ≤ 2π, and d− c ≤ π.
Then, the formula for triple integration in spherical coordinates is given by∫∫∫Ef(x, y, z)dV
=
∫ d
c
∫ β
α
∫ b
af(ρ sinφ cos θ, ρ sinφ sin θ, ρ cosφ)ρ2 sinφdρdθdφ.
MAT 1002 Calculus II 31 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Spherical Coordinates
Example 9
Evaluate
∫∫∫Be(x
2+y2+z2)3/2dV , where B is the unit ball
B = {(x, y, z)|x2 + y2 + z2 ≤ 1}.
Solution.
Since the boundary of B is a sphere, we use spherical coordinates:
B = {(ρ, θ, φ)|0 ≤ ρ ≤ 1, 0 ≤ θ ≤ 2π, 0 ≤ φ ≤ π}.
In addition, spherical coordinates are appropriate becausex2 + y2 + z2 = ρ2. Thus,∫∫∫
Be(x
2+y2+z2)3/2dV =
∫ π
0
∫ 2π
0
∫ 1
0e(ρ
2)3/2ρ2 sinφdρdθdφ
=4π
3(e− 1).
MAT 1002 Calculus II 32 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Spherical Coordinates
Note
It would have been extremely awkward to evaluate the integral in previousExample without spherical coordinates. In rectangular coordinates theiterated integral would have been∫ 1
−1
∫ √1−x2−√1−x2
∫ √1−x2−y2
−√
1−x2−y2e(x
2+y2+z2)3/2dzdydx.
MAT 1002 Calculus II 33 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Spherical Coordinates
Example 10
Use spherical coordinates to find the volume of the solid that lies abovethe cone z =
√x2 + y2 and below the sphere x2 + y2 + z2 = z.
Solution.
SOLUTION Since the boundary of is a sphere, we use spherical coordinates:
In addition, spherical coordinates are appropriate because
Thus, (4) gives
NOTE � It would have been extremely awkward to evaluate the integral in Example 3without spherical coordinates. In rectangular coordinates the iterated integral wouldhave been
EXAMPLE 4 Use spherical coordinates to find the volume of the solid that lies abovethe cone and below the sphere . (See Figure 9.)
SOLUTION Notice that the sphere passes through the origin and has center . Wewrite the equation of the sphere in spherical coordinates as
The equation of the cone can be written as
This gives , or . Therefore, the description of the solid inspherical coordinates is
E � ���, �, �� 0 � � � 2�, 0 � � � ��4, 0 � � � cos �
E� � ��4sin � � cos �
� cos � � s�2 sin2� cos2� � �2 sin 2� sin2� � � sin �
� � cos �or�2 � � cos �
(0, 0, 12 )
yx
z(0, 0, 1)
≈+¥+z@=z
z=œ„„„„„≈+¥π4
FIGURE 9
x 2 � y 2 � z2 � zz � sx 2 � y 2
y1
�1 y
s1�x2
�s1�x2 y
s1�x2�y2
�s1�x2�y2 e �x2�y2�z2�3�2
dz dy dx
� [�cos �]0� �2�� [ 1
3e�3 ]0
1�
4�
3 �e � 1�
� y�
0 sin � d� y
2�
0 d� y
1
0 �2e �3 d�
yyyB
e �x2�y2�z2�3�2
dV � y�
0 y
2�
0 y
1
0 e��2�3�2
�2 sin � d� d� d�
x 2 � y 2 � z2 � �2
B � ���, �, �� 0 � � � 1, 0 � � � 2�, 0 � � � �
B
SECTION 12.8 TRIPLE INTEGRALS IN CYLINDRICAL AND SPHERICAL COORDINATES � 897
FIGURE 10
� Figure 10 gives another look (this time drawn by Maple) at the solid ofExample 4.
Notice that the sphere passes through theorigin and has center (0, 0, 12). We write theequation of the sphere in spherical coordi-nates as
ρ2 = ρ cosφ or ρ = cosφ.
The equation of the cone can be written as
ρ cosφ =
√ρ2 sin2 φ cos2 θ + ρ2 sin2 φ sin2 θ = ρ sinφ.
MAT 1002 Calculus II 34 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Spherical Coordinates
Solution (cont.)
This gives sinφ = cosφ, or φ = π/4. Therefore, the description of thesolid E in spherical coordinates is
E = {(ρ, θ, φ)|0 ≤ θ ≤ 2π, 0 ≤ φ ≤ π/4, 0 ≤ ρ ≤ cosφ}.
6.
� � � � � � � � � � � � �
7–14 � Use cylindrical coordinates.
7. Evaluate , where is the region that liesinside the cylinder and between the planes
and .
8. Evaluate , where is the solid in the firstoctant that lies beneath the paraboloid .
9. Evaluate , where is the solid that lies between the cylinders and , above the
-plane, and below the plane .z � x � 2xyx 2 � y 2 � 4x 2 � y 2 � 1
ExxxE y dV
z � 1 � x 2 � y 2Exxx
E �x 3 � xy 2 � dV
z � 4z � �5x 2 � y 2 � 16
ExxxE sx 2 � y 2 dV
z
x y21
1–4 � Sketch the solid whose volume is given by the integraland evaluate the integral.
1. 2.
3.
4.
� � � � � � � � � � � � �
5–6 � Set up the triple integral of an arbitrary continuous func-tion in cylindrical or spherical coordinates over thesolid shown.
5. z
xy
3
2
f �x, y, z�
y2�
0 y
�
��2 y
2
1 �2 sin � d� d� d�
y��6
0 y
��2
0 y
3
0 �2 sin � d� d� d�
y��2
0 y
2
0 y
9�r 2
0 r dz dr d�y
4
0 y
2�
0 y
4
r r dz d� dr
898 � CHAPTER 12 MULTIPLE INTEGRALS
Exercises � � � � � � � � � � � � � � � � � � � � � � � � � �12.8
Figure 11 shows how E is swept out if we integrate first with respect to , then ,and then . The volume of E is
FIGURE 11¨ varies from 0 to 2π.∏ varies from 0 to cos ˙ while
˙ and ¨ are constant.˙ varies from 0 to π/4 while¨ is constant.
z
yx
z
yx
z
yx
�2�
3 y
��4
0 sin � cos3� d� �
2�
3 �
cos4�
4 �0
��4
��
8
� y2�
0 d� y
��4
0 sin � �3
3 ���0
��cos �
d�
V�E� � yyyE
dV � y2�
0 y
��4
0 y
cos �
0 �2 sin � d� d� d�
���
6.
� � � � � � � � � � � � �
7–14 � Use cylindrical coordinates.
7. Evaluate , where is the region that liesinside the cylinder and between the planes
and .
8. Evaluate , where is the solid in the firstoctant that lies beneath the paraboloid .
9. Evaluate , where is the solid that lies between the cylinders and , above the
-plane, and below the plane .z � x � 2xyx 2 � y 2 � 4x 2 � y 2 � 1
ExxxE y dV
z � 1 � x 2 � y 2Exxx
E �x 3 � xy 2 � dV
z � 4z � �5x 2 � y 2 � 16
ExxxE sx 2 � y 2 dV
z
x y21
1–4 � Sketch the solid whose volume is given by the integraland evaluate the integral.
1. 2.
3.
4.
� � � � � � � � � � � � �
5–6 � Set up the triple integral of an arbitrary continuous func-tion in cylindrical or spherical coordinates over thesolid shown.
5. z
xy
3
2
f �x, y, z�
y2�
0 y
�
��2 y
2
1 �2 sin � d� d� d�
y��6
0 y
��2
0 y
3
0 �2 sin � d� d� d�
y��2
0 y
2
0 y
9�r 2
0 r dz dr d�y
4
0 y
2�
0 y
4
r r dz d� dr
898 � CHAPTER 12 MULTIPLE INTEGRALS
Exercises � � � � � � � � � � � � � � � � � � � � � � � � � �12.8
Figure 11 shows how E is swept out if we integrate first with respect to , then ,and then . The volume of E is
FIGURE 11¨ varies from 0 to 2π.∏ varies from 0 to cos ˙ while
˙ and ¨ are constant.˙ varies from 0 to π/4 while¨ is constant.
z
yx
z
yx
z
yx
�2�
3 y
��4
0 sin � cos3� d� �
2�
3 �
cos4�
4 �0
��4
��
8
� y2�
0 d� y
��4
0 sin � �3
3 ���0
��cos �
d�
V�E� � yyyE
dV � y2�
0 y
��4
0 y
cos �
0 �2 sin � d� d� d�
���
6.
� � � � � � � � � � � � �
7–14 � Use cylindrical coordinates.
7. Evaluate , where is the region that liesinside the cylinder and between the planes
and .
8. Evaluate , where is the solid in the firstoctant that lies beneath the paraboloid .
9. Evaluate , where is the solid that lies between the cylinders and , above the
-plane, and below the plane .z � x � 2xyx 2 � y 2 � 4x 2 � y 2 � 1
ExxxE y dV
z � 1 � x 2 � y 2Exxx
E �x 3 � xy 2 � dV
z � 4z � �5x 2 � y 2 � 16
ExxxE sx 2 � y 2 dV
z
x y21
1–4 � Sketch the solid whose volume is given by the integraland evaluate the integral.
1. 2.
3.
4.
� � � � � � � � � � � � �
5–6 � Set up the triple integral of an arbitrary continuous func-tion in cylindrical or spherical coordinates over thesolid shown.
5. z
xy
3
2
f �x, y, z�
y2�
0 y
�
��2 y
2
1 �2 sin � d� d� d�
y��6
0 y
��2
0 y
3
0 �2 sin � d� d� d�
y��2
0 y
2
0 y
9�r 2
0 r dz dr d�y
4
0 y
2�
0 y
4
r r dz d� dr
898 � CHAPTER 12 MULTIPLE INTEGRALS
Exercises � � � � � � � � � � � � � � � � � � � � � � � � � �12.8
Figure 11 shows how E is swept out if we integrate first with respect to , then ,and then . The volume of E is
FIGURE 11¨ varies from 0 to 2π.∏ varies from 0 to cos ˙ while
˙ and ¨ are constant.˙ varies from 0 to π/4 while¨ is constant.
z
yx
z
yx
z
yx
�2�
3 y
��4
0 sin � cos3� d� �
2�
3 �
cos4�
4 �0
��4
��
8
� y2�
0 d� y
��4
0 sin � �3
3 ���0
��cos �
d�
V�E� � yyyE
dV � y2�
0 y
��4
0 y
cos �
0 �2 sin � d� d� d�
���
ρ varies from 0 to cosφ φ varies from 0 to π/4 θ varies from 0 to 2π
MAT 1002 Calculus II 35 / 36
Triple Integrals in Cylindrical and Spherical Coordinates Spherical Coordinates
Solution (cont.)
The volume of E is
V (E) =
∫∫∫EdV =
∫ 2π
0
∫ π/4
0
∫ cosφ
0ρ2 sinφdρdφdθ
=
∫ 2π
0dθ
∫ π/4
0sinφ
[ρ3
3
]ρ=cosφ
ρ=0
dφ
=2π
3
∫ π/4
0sinφ cos3 φdφ
=π
8.
MAT 1002 Calculus II 36 / 36