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F(x,y)= 1 2 (i+ j) 1 2 y=x. F(x, y)=i+x j i+x j 1+x2 y � F(x, y)=y i+ 12 j y i+ 12 j y 2 + 1 4 x � F(x, y)=(x�y) i+x j (x�y) i+x j (x�y)2+x2 y=x 1. All vectors in this field are identical, with length and direction parallel to the line 2. The length of the vector is . Vectors are tangent to parabolas opening about the axis. 3. . The length of the vector is . Vectors are tangent to parabolas opening about the axis. 4. The length of the vector is . Vectors along the line are vertical. 1 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.1 Vector Fields F(x, y)= y i+x j x 2 +y 2 y i+x j x 2 +y 2 F(x, y)= y i�x j x 2 +y 2 F(x, y) x 2 +y 2 F(x, y, z)= j y � 1 F(x, y, z)=z j (x, y, z) F(x, y, z) |z| z>0 y � z<0 y � 5. The length of the vector is 1. 6. All the vectors are unit vectors tangent to circles centered at the origin with radius . 7. All vectors in this field are parallel to the axis and have length . 8. At each point , is a vector of length . For , all point in the direction of the positive axis while for , all are in the direction of the negative axis. 2 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.1 Vector Fields F(x, y, z)=y j F(x, y, z) |y| xz � y=0 y=b F(x, y, z)= j�i 2 xy � F(x, y)= y, x x � y � x � y � x � y � x � y � F(x, y)= 1, sin y x � x F(x, y)= x�2, x+1 y x � y � F(x, y)= y, 1/x x � y � x � y � x � y � 9. The length of is . No vectors emanate from the plane since there. In each plane , all the vectors are identical. 10. All vectors in this field have length and point in the same direction, parallel to the plane. 11. corresponds to graph II. In the first quadrant all the vectors have positive and components, in the second quadrant all vectors have positive components and negative components, in the third quadrant all vectors have negative and components, and in the fourth quadrant all vectors have negative components and positive components. In addition, the vectors get shorter as we approach the origin. 12. corresponds to graph IV since the component of each vector is constant, the vectors are independent of (vectors along horizontal lines are identical), and the vector field appears to repeat the same pattern vertically. 13. corresponds to graph I since the vectors are independent of (vectors along vertical lines are identical) and, as we move to the right, both the and the components get larger. 14. corresponds to graph III. As in Exercise 11, all the vectors in the first quadrant have positive and components, in the second quadrant all vectors have positive components and negative components, in the third quadrant all vectors have negative and components, 3 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.1 Vector Fields x � y � y � F(x, y, z)=i+2 j+3 k F(x, y, z)=i+2 j+zk xy � xy � F(x, y, z)=x i+y j+3 k xy � x i+y j z � 3 F(x, y, z)=x i+y j+zk F(x, y, z) (x, y, z) y=2x F(x, y)= 0, 0 y 2 �2xy=0 3xy�6x 2 =0 y=0 y=2x x=0 y=2x F(x, y)=0 y=2x |x|=2 F(x)=0� r(r�2)=0�r=0 2 F(x)=0 |x|=2 |x|=0 r 2 �r<0 r 2 �r>0 and in the fourth quadrant all vectors have negative components and positive components. Also, the vectors become longer as we approach the axis. 15. corresponds to graph IV, since all vectors have identical length and direction. 16. corresponds to graph I, since the horizontal vector components remain constant, but the vectors above the plane point generally upward while the vectors below the plane point generally downward. 17. corresponds to graph III; the projection of each vector onto the plane is , which points away from the origin, and the vectors point generally upward because their components are all . 18. corresponds to graph II; each vector has the same length and direction as the position vector of the point , and therefore the vectors all point directly away from the origin. 19. The vector field seems to have very short vectors near the line . For we must have and . The first equation holds if or , and the second holds if or . So both equations hold [and thus ] along the line . 20. From the graph, it appears that all of the vectors in the field lie on lines through the origin, and that the vectors have very small magnitudes near the circle and near the origin. Note that or , so as we suspected, for and for . Note that where , the vectors point towards the origin, and where , they point away from the origin. 4 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.1 Vector Fields � f (x, y)= f x (x, y)i+ f y (x, y) j= 1 x+2y i+ 2 x+2y j � f (x, y)= f x (x, y)i+ f y (x, y) j= x� (�� e�� x)+� x� �1e�� x i+0 j=(� �� x)x� �1e�� x i � f (x, y, z) = f x(x, y, z) i+ f y(x, y, z) j+ f z(x, y, z) k = x x 2 +y 2 +z 2 i+ y x 2 +y 2 +z 2 j+ z x 2 +y 2 +z 2 k � f (x, y, z) = f x(x, y, z) i+ f y(x, y, z) j+ f z(x, y, z) k = cos y z i�x sin y z 1 z j�x sin y z � y z 2 k = cos y z i� x z sin y z j+ xy z 2 sin y z k f (x, y)=xy�2x�� f (x, y)=(y�2) i+x j � f (x, y) (y�2)2+x2 � f (x, y) y=x+2 (x+y�2, x+y). f (x, y)= 14 (x+y) 2 � � f (x, y)= 12 (x+y) i+ 1 2 (x+y) j � f (x, y) 21. 22. 23. 24. 25. . The length of is and terminates on the line at the point 26. . The length of is 5 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.1 Vector Fields 1 2 (x+y) 2 = 1 2 |x+y|. y=�x y=�x � f f f � f f f f (x, y)=xy�� f (x, y)=y i+x j x � y � � f The vectors are perpendicular to the line and point away from the line, with length that increases as the distance from the line increases. 27. We graph along with a contour map of . The graph shows that the gradient vectors are perpendicular to the level curves. Also, the gradient vectors point in the direction in which is increasing and are longer where the level curves are closer together. 28. We graph along with a contour map of . The graph shows that the gradient vectors are perpendicular to the level curves. Also, the gradient vectors point in the direction in which is increasing and are longer where the level curves are closer together. 29. . In the first quadrant, both components of each vector are positive, while in the third quadrant both components are negative. However, in the second quadrant each vector’s component is positive while its component is negative (and vice versa in the fourth quadrant). Thus, is graph IV. 6 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.1 Vector Fields f (x, y)=x2�y2�� f (x, y)=2x i�2y j x � y � x � x � y � y � � f f (x, y)=x2+y2�� f (x, y)=2x i+2y j � f (x, y) (x, y) � f f (x, y)= x2+y2 �� f (x, y)= x x 2 +y 2 i+ y x 2 +y 2 j |� f (x, y)|= 1 x 2 +y 2 x 2 +y 2 =1 � f (x, y) (x,y) � f F(x, y)=x i�y j y=�1/x y=C /x x=x(t) y=y(t) (x, y) x / (t)i+y / t( ) j x / (t)i+y /(t) j=x i�y j�dx/dt=x dy/dt=�y dx/dt=x�dx/x=dt� ln |x|=t+C� x=�et +C=Aet A dy/dt=�y�dy/y=�dt� ln |y|=�t+K� y=�e�t +K=Be�t B xy=Ae t Be �t =AB= (1, 1) (1)(1)= =1� xy=1� y=1/x x>0 F(x, y)=i+x j 30. . In the first quadrant, the component of each vector is positive while the component is negative. The other three quadrants are similar, where the component of each vector has the same sign as the value of its initial point, and the component has sign opposite that of the value of the initial point. Thus, is graph III. 31. . Thus, each vector has the same direction and twice the length of the position vector of the point , so the vectorsall point directly away from the origin and their lengths increase as we move away from the origin. Hence, is graph II. 32. . Then , so all vectors are unit vectors. In addition, each vector has the same direction as the position vector of the point , so the vectors all point directly away from the origin. Hence, is graph I. 33. (a) We sketch the vector field along with several approximate flow lines.The flow lines appear to be hyperbolas with shape similar to the graph of , so we might guess that the flow lines have equations . (b) If and are parametric equations of a flow line, then the velocity vector of the flow line at the point is . Since the velocity vectors coincide with the vectors in the vector field, we have , . To solve these differential equations, we know for some constant , and for some constant . Therefore constant. If the flow line passes through then constant , . 34. (a) We sketch the vector field along with several approximate flow lines.The flow lines appear to be parabolas. 7 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.1 Vector Fields x=x(t) y=y(t) (x, y) x / (t)i+y /(t) j x / (t)i+y /(t) j=i+x j� dxdt =1 dy dt =x dy dx = dy/dt dx/dt = x 1 =x dy/dx=x y= 12 x 2 +c (0, 0) 0=0+c� c=0 y= 1 2 x 2 (b) If and are parametric equations of a flow line, then the velocity vector of the flow line at the point is . Since the velocity vectors coincide with the vectors in the vector field, we have , . Thus . (c) From part (b), . Integrating, we have . Since the particle starts at the origin, we know is on the curve, so and the path the particle follows is . 8 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.1 Vector Fields x=t 2 y=t 0� t� 2 �C y ds = � 2 0 t dx dt 2 + dy dt 2 dt=�2 0 t (2t) 2 +(1) 2 dt = �2 0 t 4t 2 +1 dt= 1 12 (4t 2 +1) 3/2 2 0 = 1 12 (17 17�1) � C y x ds =�1 1/2 t 3 t 4 (4t 3 ) 2 +(3t 2 ) 2 dt=�1 1/2 1 t 16t 6 +9t 4 dt=�1 1/2 t 16t 2 +9 dt = 1 48 (16t 2 +9) 3/2 1 1/2 = 1 48 (25 3/2 �13 3/2 )= 1 48 (125�13 13) C x=4cos t y=4sin t � � 2 � t� � 2 �Cxy 4 ds = �� /2 �� /2 (4cos t)(4sin t) 4 (�4sin t) 2 +(4cos t) 2 dt = �� /2 �� /2 4 5 cos tsin 4 t 16(sin 2 t+cos 2 t) dt = 4 5�� /2 �� /2 (sin 4 tcos t)(4)dt=(4) 6 1 5 sin 5 t � /2 �� /2 = 2 � 4 6 5 =1638.4 C x=1+3t y=2+5t 0� t� 1 �Cye x ds=�1 0 (2+5t)e 1+3t 3 2 +5 2 dt= 34�1 0 (2+5t)e 1+3t dt u=2+5t � du=5dt dv=e 1+3t � v= 1 3 e 1+3t dt �Cye x ds = 34 1 3 (2+5t)e 1+3t � 5 9 e 1+3t 1 0 = 34 7 3 � 5 9 e 4 � 2 3 � 5 9 e = 34 9 (16e 4 �e) x C x=x y=x 2 1� x� 3 1. and , , so by Formula 3 2. 3. Parametric equations for are , , . Then 4. Parametric equations for are , , . Then Integrating by parts with , gives 5. If we choose as the parameter, parametric equations for are , for and 1 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals � C (xy+ln x)dy = �3 1 (x� x 2 +ln x)2xdx=�3 1 2(x 4 +xln x)dx = 2 1 5 x 5 + 1 2 x 2 ln x� 1 4 x 2 3 1 = 2 243 5 + 9 2 ln 3� 9 4 � 1 5 + 1 4 = 464 5 +9ln 3 y x=e y y=y 0� y� 1 �cxe y dx=�1 0 e y (e y )e y dy=�1 0 e 3y dy= 1 3 e 3y 1 0 = 1 3 (e 3 �1) C=C 1 +C 2 C 1 x=x y=0�dy=0dx 0� x� 2 C 2 x=x y=2x�4�dy=2dx 2� x� 3 �Cxydx+(x�y)dy =�C1 xydx+(x�y)dy+� C2 xydx+(x�y)dy =�2 0 (0+0)dx+�3 2 dx =�3 2 (2x 2 �6x+8)dx= 17 3 C=C 1 +C 2 C 1 x=cos t�dx=�sin t dt y=sin t� (by integrating by parts in the second term) 6. Choosing as the parameter, we have , , . Then . 7. On : , , . On : , , . Then 8. On : , 2 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals dy=cos t dt 0� t�� C 2 x=�1�t�dx=�dt y=3t� dy=3dt 0� t� 1 � C sin xdx+cos ydy =�C1 sin xdx+cos ydy+� C2 sin xdx+cos ydy =�� 0 sin (cos t)(�sin t dt)+cos (sin t)cos t dt +�1 0 sin (�1�t)(�dt)+cos (3t)(3dt) = �cos (cos t)+sin (sin t) � 0 + �cos (�1�t)+sin (3t) 1 0 =�cos (cos� )+sin (sin� )+cos (cos 0)�sin (sin 0) �cos (�2)+sin (3)+cos (�1)�sin (0) =�cos (�1)+sin 0+cos (1)�sin 0�cos (�2)+sin 3+cos (�1) =�cos 1+cos 1�cos 2+sin 3+cos 1=cos 1�cos 2+sin 3 cos (�� )=cos� x=4sin t y=4cos t z=3t 0� t� � 2 � C xy 3 ds = �� /2 0 (4sin t)(4cos t) 3 dx dt 2 + dy dt 2 + dz dt 2 dt = �� /2 0 4 4 cos 3 tsin t (4cos t) 2 +(�4sin t) 2 +(3) 2 dt = �� /2 0 256cos 3 tsin t 16(cos 2 t+sin 2 t +9)dt = 1280�� /2 0 cos 3 tsin t dt= �320cos 4 t � /2 0 =320 C x=4t y=6�5t z=�1+6t 0� t� 1 � C x 2 zds = �1 0 (4t) 2 (6t�1) 4 2 +(�5) 2 +6 2 dt= 77�1 0 (96t 3 �16t 2 )dt = 77 96� t 4 4 �16� t 3 3 1 0 = 56 3 77 , . On : , , . Then where we have used the identity . 9. , , , . Then by Formula 9, 10. Parametric equations for are , , , . Then 3 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals C x=t y=2t z=3t 0� t� 1 �Cxe yz ds = �1 0 te (2t)(3t) 1 2 +2 2 +3 2 dt= 14�1 0 te 6t 2 dt = 14 1 12 e 6t 2 1 0 = 14 12 (e 6 �1) (dx/dt) 2 +(dy/dt) 2 +(dz/dt) 2 = 1 2 +(2t) 2 +(3t 2 ) 2 = 1+4t 2 +9t 4 � C (2x+9z)ds =�1 0 (2t+9t 3 ) 1+4t 2 +9t 4 dt u=1+4t 2 +9t 4 � 1 4 du=(2t+9t 3 )dt =�14 1 1 4 u du= 1 6 u 3/2 14 1 = 1 6 (14 3/2 �1) �Cx 2 y z dz=�1 0 (t 3 ) 2 (t) t 2 � 2t dt=�1 0 2t 9 dt= 1 5 t 10 1 0 = 1 5 �Czdx+xdy+ydz =� 1 0 t 2 � 2t dt+t 2 � 3t 2 dt+t 3 � 2t dt=�1 0 (2t 3 +5t 4 )dt = 1 2 t 4 +t 5 1 0 = 1 2 +1= 3 2 C 1 x=1+t�dx=dt y=3t�dy=3dt z=1 �dz=0dt 0� t� 1 C 2 x=2�dx=0dt y=3+2t� dy=2dt z=1+t�dz=dt 0� t� 1 �C (x+yz)dx+2xdy+xyzdz =� C1 (x+yz)dx+2xdy+xyzdz+� C2 (x+yz)dx+2xdy+xyzdz 11. Parametric equations for are , , , . Then 12. . Then [ let ] 13. 14. 15. On : , , , . On : , , , . Then 4 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals =�1 0 (1+t+(3t)(1))dt+2(1+t)� 3dt+(1+t)(3t)(1)� 0dt +�1 0 (2+(3+2t)(1+t))� 0dt+2(2)� 2dt+(2)(3+2t)(1+t)dt =�1 0 (10t+7)dt+�1 0 (4t 2 +10t+14)dt = 5t 2 +7t 1 0 + 4 3 t 3 +5t 2 +14t 1 0 =12+ 61 3 = 97 3 C 1 x=t�dx=dt y=2t�dy=2dt z=�t �dz=�dt 0� t� 1 C 2 x=1+2t�dx=2dt y=2� dy=0dt z=�1+t�dz=dt 0� t� 1 � C x 2 dx+y 2 dy+z 2 dz =� C1 x 2 dx+y 2 dy+z 2 dz+� C2 x 2 dx+y 2 dy+z 2 dz =�1 0 t 2 dt+(2t) 2 � 2dt+(�t) 2 (�dt)+�1 0 (1+2t) 2 � 2dt+2 2 � 0dt+(�1+t) 2 dt =�1 0 8t 2 dt+�1 0 (9t 2 +6t+3)dt= 8 3 t 3 1 0 + 3t 3 +3t 2 +3t 1 0 = 35 3 x=�3 F y � F�T � C1 F� dr=� C1 F�T ds 3 F�T � C2 F� dr=� C2 F�T ds 16. On : , , , . On : , , , . Then 17. (a) Along the line , the vectors of have positive components, so since the path goes upward, the integrand is always positive. Therefore is positive. (b) All of the (nonzero) field vectors along the circle with radius are pointed in the clockwise direction, that is, opposite the direction tothe path. So is negative, and therefore is negative. 18. Vectors starting on 5 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals C 1 C 1 F�T � C1 F� dr=� C1 F�T ds C 2 C 2 � C2 F� dr=� C2 F�T ds r(t)=t 2 i�t 3 j F(r(t))=(t 2 ) 2 (�t 3 ) 3 i�(�t 3 ) t 2 j=�t 13 i+t 4 j r / (t)=2t i�3t 2 j �CF� dr=� 1 0 F(r(t))� r / (t)dt=�1 0 (�2t 14 �3t 6 )dt= � 2 15 t 15 � 3 7 t 7 1 0 =� 59 105 F(r(t))=(t 2 )(t 3 )i+(t)(t 3 ) j+(t)(t 2 )k=t 5 i+t 4 j+t 3 k r / (t)=i+2t j+3t 2 k �CF� dr=� 2 0 F(r(t))� r / (t)dt=�2 0 (t 5 +2t 5 +3t 5 )dt= t 6 2 0 =64 �CF� dr =� 1 0 sin t 3 , cos (�t 2 ), t 4 � 3t 2 , �2t, 1 dt =�1 0 (3t 2 sin t 3 �2tcos t 2 +t 4 )dt= �cos t 3 �sin t 2 + 1 5 t 5 1 0 = 6 5 �cos 1�sin 1 �CF� d r =� � 0 cos t, sin t, �t � 1, cos t, �sin t dt=�� 0 (cos t+sin tcos t+tsin t)dt = sin t+ 1 2 sin 2 t+(sin t�tcos t) � 0 =� F(x, y)=(x�y) i+xy j C C C C F�T C C �CF� dr=�CF�T ds �CF� dr C r(t)=2cos t i+2sin t j 0� t� 3� 2 F(r(t))=(2cos t�2sin t) i+4cos tsin t j r / (t)=�2sin t i+2cos t j point in roughly the same direction as , so the tangential component is positive. Then is positive. On the other hand, no vectors starting on point in the same direction as , while some vectors point in roughly the opposite direction, so we would expect to be negative. 19. , so and . Thus . 20. , . Thus . 21. 22. 23. We graph and the curve . We see that most of the vectors starting on point in roughly the same direction as , so for these portions of the tangential component is positive. Although some vectors in the third quadrant which start on point in roughly the opposite direction, and hence give negative tangential components, it seems reasonable that the effect of these portions of is outweighed by the positive tangential components. Thus, we would expect to be positive. To verify, we evaluate . The curve can be represented by , , so and . Then 6 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals � C F� dr = �3� /2 0 F(r(t))� r / t( ) dt = �3� /2 0 �2sin t(2cos t�2sin t)+2cos t(4cos tsin t) dt = 4�3� /2 0 (sin 2 t�sin tcos t+2sin tcos 2 t)dt = 3� + 2 3 F(x, y)= x x 2 +y 2 i+ y x 2 +y 2 j C C C F�T C C F�T � C F� dr=� C F�T ds �CF� dr C r(t)=t i+(1+t 2 ) j �1� t� 1 F(r(t))= t t 2 +(1+t 2 ) 2 i+ 1+t 2 t 2 +(1+t 2 ) 2 j r / (t)=i+2t j �CF� dr = � 1 �1 F(r(t))� r / (t)dt = � 1 �1 t t 2 +(1+t 2 ) 2 + 2t (1+t 2 ) t 2 +(1+t 2 ) 2 dt [using a CAS] 24. We graph and the curve . In the first quadrant, each vector starting on points in roughly the same direction as , so the tangential component is positive. In the second quadrant, each vector starting on points in roughly the direction opposite to , so is negative. Here, it appears that the tangential components in the first and second quadrants counteract each other, so it seems reasonable to guess that is zero. To verify, we evaluate . The curve can be represented by , , so and . Then 7 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals = �1�1 t (3+2t 2 ) t 4 +3t 2 +1 dt=0 � C F� dr �1 0 e t 2 �1 , t 5 � 2t, 3t 2 dt=�1 0 2te t 2 �1 +3t 7( )dt= et2�1+ 38 t8 1 0 = 11 8 �1/e r(0)=0 F(r(0))= e �1 , 0 r 1 2 = 1 2 , 1 2 2 F r 1 2 = e �1/2 , 1 4 2 r(1)= 1, 1 F(r(1))= 1, 1 PLOT plot v1:=PLOT(CURVES( [ [0, 0], [evalf(1/exp(1)), 0] ] ) ); (0, 0) v1. display ListPlot PlotJoined � > True Show � C F� dr=�1 �1 2t, t 2 , 3t � 2, 3, �2t dt=�1 �1 (4t+3t 2 �6t 2 )dt= 2t 2 �t 3 1 �1 =�2 F(r(t))= 2t, t 2 , 3t F(r(�1))= �2, 1, �3 F r � 1 2 = �1, 1 4 , � 3 2 F r 1 2 = 1, 1 4 , 3 2 F(r(1))= 2, 1, 3 [since the integrand is an odd function] 25. (a) = (b) , ; , ; , . In order to generate the graph with Maple, we use the command (not to be confused with the command) to define each of the vectors. For example, generates the vector from the vector field at the point (but without an arrowhead) and gives it the name To show everything on the same screen, we use the command. In Mathematica, we use (with the option) to generate the vectors, and then to show everything on the same screen. 26. (a) (b) Now , so , , , and . 8 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals x=cos 3 t y=sin 3 t 0� t� � 2 dx dt =3cos 2 t (�sin t) dy dt =3sin 2 tcos t dx dt 2 + dy dt 2 = 9cos 4 tsin 2 t+9sin 4 tcos 2 t =3cos tsin t cos 2 t+sin 2 t =3cos tsin t � C x 3 y 5 ds=�� /2 0 cos 9 tsin 15 t (3cos tsin t)dt= 945 16,777,216 � (t)= 1, 2, 1 +t 6, 4, 5 � 1, 2, 1 =(1+5t)i+(2+2t) j+(1+4t)k 0� t� 1 � C F� dr =�1 0 (1+5t) 4 e 2+2t , ln (1+4t), (2+2t) 2 +(1+4t) 2 � 5, 2, 4 dt = 5235e 4 4 � 6285e 2 4 + 9 5sinh �1 14 3 25 � 9 5sinh �1 4 3 25 + 5ln 5 2 + 14 41 5 � 4 5 5 �2 = 5235e 4 4 � 6285e 2 4 � 18 5ln 3 25 + 9 5ln (14+ 205 ) 25 + 5ln 5 2 + 14 41 �4 5 5 �2 �Cxsin yds=� 2 1 ln tsin (e �t ) (1/t) 2 +(�e �t ) 2 dt�0.052 C r(t)=2cos t i+2sin t j 0� t� 2� F(r(t))= 4cos 2 t, 4cos tsin t r / (t)= �2sin t, 2cos t W =� C F� dr=�2� 0 (�8cos 2 tsin t+8cos 2 tsin t)dt=0 27. The part of the astroid that lies in the quadrant is parametrized by , , . Now and , so . Therefore . 28. We parametrize the line as r , . Using a CAS, we calculate The first answer is the one given by Maple. The two answers are equivalent by Equation 7.6.3 . 29. A calculator or CAS gives . 30. (a) We parametrize the circle as , . So , , and . (b) From the graph, we see that all of the vectors in the field are perpendicular to the path. This indicates that the field does no work on the particle, since the field never pulls the particle in the direction in 9 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals C F�T=0 �CF� dr=0 x=2cos t y=2sin t � � 2 � t� � 2 ds= dx dt 2 + dy dt 2 dt= (�2sin t) 2 +(2cos t) 2 dt=2dt m=�Ckds=2k� � /2 �� /2 dt=2k(� ) x= 1 2� k �Cxkds= 1 2� � � /2 �� /2 (2cos t)2dt= 1 2� 4sin t � /2 �� /2 = 4 � y= 1 2� k �Cykds= 1 2� � � /2 �� /2 (2sin t)2dt=0 (x,y)= 4 � ,0 x=rcos t y=rsin t 0� t� � 2 ds= dx dt 2 + dy dt 2 dt= (�rsin t) 2 +(rcos t) 2 dt=r dt m=�C(x+y)ds=� � /2 0 (rcos t+rsin t)r dt=r 2 sin t�cos t � /2 0 =2r 2 x = 1 2r 2 �Cx(x+y)ds= 1 2r 2 �� /2 0 (r 2 cos 2 t+r 2 cos tsin t)r dt= r 2 t 2 + sin 2t 4 � cos 2t 4 � /2 0 = r(� +2) 8 y = 1 2r 2 �Cy(x+y)ds= 1 2r 2 �� /2 0 (r 2 sin tcos t+r 2 sin 2 t)r dt = r 2 � cos 2t 4 + t 2 � sin 2t 4 � /2 0 = r(� +2) 8 (x, y)= r(� +2) 8 , r(� +2) 8 . x= 1 m �Cx� (x, y, z)ds y= 1 m �Cy� (x, y, z)ds z= 1 m �Cz� (x, y, z)ds m=�C� (x, y, z)ds m=�Ckds=k� 2� 0 4sin 2 t+4cos 2 t+9 dt=k 13�2� 0 dt=2� k 13 x= 1 2� k 13 �2� 0 k2 13 sin t dt=0 y= 1 2� k 13 �2� 0 k2 13 cos t dt=0 z= 1 2� k 13 �2� 0 (k 13 )(3t)dt=3 2� (2� 2 )=3� which it is going. In other words, at any point along , , and so certainly . 31. We use the parametrization , , . Then , so , , . Hence . 32. We use the parametrization , , . Then , so , , and . Therefore 33. (a) , , where . (b) , , , . Hence 10 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals (x, y, z)=(0, 0, 3� ) m =�C(x 2 +y 2 +z 2 )ds=�2� 0 (t 2 +1) (1) 2 +(�sin t) 2 +(cos t) 2 dt=�2� 0 (t 2 +1) 2 dt = 2 8 3 � 3 +2� x= 1 2 8 3 � 3 +2� �2� 0 2 (t 3 +t)dt 4� 4 +2� 2 8 3 � 3 +2� 3� (2� 2 +1) 4� 2 +3 y= 3 2 2� (4� 2 +3) �2� 0 ( 2 cos t)(t 2 +1)dt=0 z= 3 2 2� (4� 2 +3) �2� 0 ( 2sin t)(t 2 +1)dt=0 (x, y, z)= 3� (2� 2 +1) 4� 2 +3 , 0, 0 � (x, y)=k(1�y) x=cos t y=sin t ds=dt 0� t��� Ix = �Cy 2 � (x, y)ds=�� 0 sin 2 t dt=k�� 0 (sin 2 t�sin 3 t)dt = 12 k� � 0 (1�cos 2t)dt�k�� 0 (1�cos 2 t)sin t dt u=t,du=�tdt�3pt = k � 2 +� �1 1 (1�u 2 )du =k � 2 � 4 3 Iy = �Cx 2 � (x, y)ds=k�� 0 cos 2 t (1�sin t)dt= k 2 � � 0 (1+cos 2t)dt�k�� 0 cos 2 tsin t dt = k � 2 � 2 3 x=2sin t y=2cos t z=3t 0� t� 2� � (x, y, z)=k ds= (2cos t) 2 +(�2sin t) 2 +3 2 = 4(cos 2 t+sin 2 t)+9 = 13 Ix =�C(y 2 +z 2 )� (x, y, z)ds=�2� 0 (4cos 2 t+9t 2 )(k) 13 dt= 13 k 4 1 2 t+ 1 4 sin 2t +3t 3 2� 0 . 34. , = = , , and . Hence . 35. From Example 3, , , , and , [Let in the second integral] , using the same substitution as above. 36. The wire is given as , , , with . Then and 11 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals = 13 k(4� +24� 3 )=4 13� k(1+6� 2 ) Iy =�C(x 2 +z 2 )� (x, y, z)ds=�2� 0 4sin 2 t+9t 2( )(k) 13 dt= 13 k 4 12 t� 1 4 sin 2t +3t 3 2� 0 = 13 k(4� +24� 3 )=4 13� k(1+6� 2 ) Iz =�C(x 2 +y 2 )� (x, y, z)ds=�2� 0 (4sin 2 t+4cos 2 t)(k) 13 dt=4 13 k�2� 0 dt=8� 13 k W =�CF� dr=� 2� 0 t�sin t, 3�cos t � 1�cos t, sin t dt =�2� 0 (t�tcos t�sin t+sin tcos t+3sin t�sin tcos t)dt =�2� 0 (t�tcos t+2sin t)dt= 1 2 t 2 �(tsin t+cos t)�2cos t 2� 0 =2� 2 x=x y=x 2 �1� x� 2 W =�2 �1 xsin x 2 , x 2 � 1, 2x dx=�2 �1 (xsin x 2 +2x 3 )dx= � 1 2 cos x 2 + 1 2 x 4 2 �1 = 1 2 (15+cos 1�cos 4) r(t)= 1+2t, 4t, 2t 0� t� 1 W =�CF� d r=� 1 0 6t, 1+4t, 1+6t � 2, 4, 2 dt=�1 0 (12t+4(1+4t)+2(1+6t))dt =�1 0 (40t+6)dt= 20t 2 +6t 1 0 =26 r(t)=2 i+t j+5t k 0� t� 1 W = �CF� dr=� 1 0 K 2, t, 5t (4+26t 2 ) 3/2 � 0, 1, 5 dt=K�1 0 26t (4+26t 2 ) 3/2 dt 37. [by integrating by parts in the second term] 38. , , , 39. , , 40. , . Therefore 12 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals = K �(4+26t 2 ) �1/2 1 0 =K 1 2 � 1 30 F=185k x=20cos t y=20sin t z= 90 6� t= 15 � t 0� t� 6�� W = �CF� dr=� 6� 0 0, 0, 185 � �20sin t, 20cos t, 15 � dt=(185) 15 � � 6� 0 dt=(185)(90) � 1.67�10 4 ft�lb m t m=185� 9 6� t=185� 3 2� t F= 185� 3 2� t k x=20cos t y=20sin t z= 90 6� t= 15 � t 0� t� 6� W = �CF� dr=� 6� 0 0, 0, 185� 3 2� t � �20sin t, 20cos t, 15 � dt= 15 � � 6� 0 185� 3 2� t dt = 15 � 185t� 3 4� t 2 6� 0 =90 185� 9 2 �1.62�10 4 ft�lb r(t)= cos t, sin t 0� t� 2� F= a, b W =�CF� d r =� 2� 0 a, b � �sin t, cos t dt =�2� 0 (�asin t+bcos t)dt= acos t+bsin t 2� 0 =a+0�a+0=0 F(x, y)=k x= kx, ky W =�CF� d r =� 2� 0 kcos t, ksin t � �sin t, cos t dt =�2� 0 (�ksin tcos t+ksin tcos t)dt=�2� 0 0dt=0 xy � z=h(x, y) 41. Let . To parametrize the staircase, let , , , 42. This time is a function of : . So let . To parametrize the staircase, let , , , . Therefore 43. (a) , , and let . Then (b) Yes. and 44. Consider the base of the fence in the plane, centered at the origin, with the height given by . The fence can be graphed using the parametric equations 13 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals x=10cos u y=10sin u z =v 4+0.01((10cos u) 2 �(10sin u) 2 ) =v(4+cos 2 u�sin 2 u) =v(4+cos 2u) 0� u� 2� 0� v� 1 �Ch(x, y)ds C x=10cos t y=10sin t 0� t� 2� �Ch(x, y)ds = � 2� 0 4+0.01((10cos t) 2 �(10sin t) 2 ) (�10sin t) 2 +(10cos t) 2 dt = �2� 0 (4+cos 2t) 100 dt=10 4t+ 1 2 sin 2t 2� 0 = 10(8� )=80�m 2 160� 2 100 2 160� 100 =1.6��5.03 �CF� dr=�CF�T ds C 7 �s=2 F�T (x * i , y * i ) C F�T C (x * i , y * i ) �CF�T ds� 7 i =1 F(x * i , y * i )�T (x * i , y * i ) �s=[2+2+2+2+1+1+1](2)=22. B B=|B|T T C x=rcos� y=rsin� , , , , . The area of the fence is where , the base of the fence, is given by , , . Then If we paint both sides of the fence, the total surface area to cover is m , and since 1 L of paint covers m , we require L of paint. 45. The work done in moving the object is . We can approximate this integral by dividing into segments of equal length and approximating , that is, the tangential component of force, at a point on each segment. Since is composed of straight line segments, is the scalar projection of each force vector onto . If we choose to be the point on the segment closest to the origin, then the work done is Thus, we estimate the work done to be approximately 22 J. 46. Use the orientation pictured in the figure. Then since is tangent to any circle that lies in the plane perpendicular to the wire, where is the unit tangent to the circle : , . Thus 14 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals B=|B| �sin� , cos� � C B� dr=�2� 0 |B| �sin� , cos� � �rsin� , rcos� d� =�2� 0 |B|r d� =2� r |B|. |B| r � C B� dr=� 0 I. |B|= � 0 I 2� r . Then (Note that here is the magnitude of the field at a distance from the wire’s center). But by Ampere’s Law Hence . 15 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.2 Line Integrals C � f f � C � f � dr f C 50�10=40. C r(t)=(t 2 +1) i+(t 3 +t) j 0� t� 1 r / (t)=2t i+(3t 2 +1) j 3t 2 +1�0 r / (t)�0 C � f f �C� f � dr= f (r(1))� f (r(0))= f (2, 2)� f (1, 0)=9�3=6 �(6x+5y)/�y=5=�(5x+4y)/�x F R 2 � F f � f =F f x(x, y)=6x+5y f y(x, y)=5x+4y f x(x, y)=6x+5y f (x,y)=3x 2 +5xy+g(y) y f y(x, y)=5x+g / (y) 5x+4y=5x+g / (y) g / (y)=4y g(y)=2y 2 +K K f (x, y)=3x 2 +5xy+2y 2 +K F �(x 3 +4xy)/�y=4x �(4xy�y 3 )/�x=4y. F �(xe y )/�y=xe y ,�(ye x )/�x=ye x . F �(e y )/�y=e y =�(xe y )/�x F R 2 F f � f =F f x(x, y)=e y f (x, y)=xe y +g(y) f y(x, y)=xe y +g / (y) f y(x, y)=xe y g / (y)=0 g(y)=K f (x, y)=xe y +K F. �(2xcos y�ycos x)/�y=�2xsin y�cos x=�(�x 2 sin y�sin x)/�x F R 2 F f � f =F f x(x, y)=2xcos y�ycos x f (x, y)=x 2 cos y�ysin x+g(y) f y(x, y)=�x 2 sin y�sin x+g / (y) f y(x, y)=�x 2 sin y�sin x g / (y)=0 g(y)=K f (x, y)=x 2 cos y�ysin x+K F �(1+2xy+ln x)/�y=2x=�(x 2 )/�x F { (x, y) | x>0 } � F f � f =F f x(x, y)=1+2xy+ln x f (x, y)=x+x 2 y+xln x�x+g(y) f y(x, y)=x 2 +g / (y) f y(x, y)=x 2 g / (y)=0 g(y)=K f (x,y)=x 2 y+xln x+K F 1. appears to be a smooth curve, and since is continuous, we know is differentiable. Then Theorem 2 says that the valueof is simply the difference of the values of at the terminal and initial points of . From the graph, this is 2. is represented by the vector function , , so . Since , we have , thus is a smooth curve. is continuous, and hence is differentiable, so by Theorem 2 we have . 3. and the domain of is which is open and simply connected, so by Theorem 6 is conservative. Thus, there exists a function such that , that is, and . But implies and differentiating both sides of this equation with respect to gives . Thus so and where is a constant. Hence is a potential function for . 4. , Since these are not equal, is not conservative. 5. Since these are not equal, is not conservative. 6. and the domain of is . Hence is conservative so there exists a function such that . Then implies and . But so . Then is a potential function for 7. and the domain of is . Hence is conservative so there exists a function such that . Then implies and . But so . Then is a potential function for . 8. and the domain of is which is open and simply connected. Hence is conservative, so there exists a function such that . Then implies and . But so . Then is a potential function for . 1 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.3 The Fundamental Theorem for Line Integrals �(ye x +sin y)/�y=e x +cos y=�(e x +xcos y)/�x F R 2 F f � f =F f x(x, y)=ye x +sin y f (x, y)=ye x +xsin y+g(y) f y(x, y)=e x +xcos y+g / (y) f y(x, y)=e x +xcos y g(y)=K f (x, y)=ye x +xsin y+K F �(xycosh xy+sinh xy) �y =x 2 ysinh xy+xcosh xy+xcosh xy=x 2 ysinh xy+2xcosh xy= �(x 2 cosh xy) �x F R 2 F f � f =F f x(x, y)=xycosh xy+sinh xy f (x, y)=xsinh xy+g(y) f y(x, y)=x 2 cosh xy+g / (y) f y(x, y)=x 2 cosh xy g(y)=K f (x, y)=xsinh xy+K F F � � �y 2xy=2x= � �x (x 2 ) R 2 � F F �CF� dr C �CF� dr f � f =F f x(x, y)=2xy f y(x, y)=x 2 f x(x, y) x f (x, y)=x 2 y+g(y) y f y(x, y)=x 2 +g / (y) x 2 +g / (y)=x 2 g / (y)=0 g(y)=K f (x, y)=x 2 y+K (1, 2) (3, 2) � C F� dr= f (3, 2)� f (1, 2)=18�2=16 f x(x, y)=y f (x, y)=xy+g(y) f y(x, y)=x+g / (y) f y(x, y)=x+2y g / (y)=2y g(y)=y 2 +K K=0 f (x, y)=xy+y 2 �CF� dr= f (2, 1)� f (0, 1)=3�1=2 f x(x, y)=x 3 y 4 f (x, y)= 1 4 x 4 y 4 +g(y) f y(x, y)=x 4 y 3 +g / (y) f y(x, y)=x 4 y 3 g / (y)=0 g(y)=K K=0 f (x, y)= 1 4 x 4 y 4 9. and the domain of is . Hence is conservative so there exists a function such that . Then implies and . But so and is a potential function for . 10. and the domain of is . Thus is conservative, so there exists a function such that . Then implies . But so and is a potential function for . 11. (a) has continuous first order partial derivatives and on , which is open and simply connected. Thus, is conservative by Theorem 6. Then we know that the line integral of is independent of path; in particular, the value of depends only on the endpoints of . Since all three curves have the same initial and terminal points, will have the same value for each curve. (b) We first find a potential function , so that . We know and . Integrating with respect to , we have . Differentiating both sides with respect to gives , so we must have , a constant. Thus . All three curves start at and end at , so by Theorem 2, for each curve. 12. (a) implies and . But so . We can take , so . (b) . 13. (a) implies and . But so , a constant. We can take , so . 2 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.3 The Fundamental Theorem for Line Integrals C r(0)=(0, 1) r(1)=(1, 2) �CF� dr= f (1, 2)� f (0, 1)=4�0=4 f x(x, y)=y 2 /(1+x 2 ) f (x, y)=y 2 arctanx+g(y) f y(x, y)=2yarctanx+g / (y) f y(x, y)=2yarctanx g / (y)=0 g(y)=K K=0 f (x, y)=y 2 arctanx. C r(0)=(0, 0) r(1)=(1, 2) �CF� d r= f (1, 2)� f (0, 0)=4arctan1�0=4� � 4 =� f x(x, y, z)=yz f (x, y, z)=xyz+g(y, z) f y(x, y, z)=xz+gy(y, z) f y(x, y, z)=xz gy(y, z)=0 g(y, z)=h(z) f (x, y, z)=xyz+h(z) f z(x, y, z)=xy+h / (z) f z(x, y, z)=xy+2z h / (z)=2z h(z)=z 2 +K f (x, y, z)=xyz+z 2 K=0 �CF� dr= f (4, 6, 3)� f (1, 0, �2)=81�4=77 f x(x, y, z)=2xz+y 2 f (x, y, z)=x 2 z+xy 2 +g(y, z) f y(x, y, z)=2xy+gy(y, z) f y(x, y, z)=2xy gy(y, z)=0 g(y, z)=h(z) f (x, y, z)=x 2 z+xy 2 +h(z) f z(x, y, z)=x 2 +h / (z) f z(x, y, z)=x 2 +3z 2 h / (z)=3z 2 h(z)=z 3 +K f (x, y, z)=x 2 z+xy 2 +z 3 K=0 t=0 (0, 1, �1) t=1 (1, 2, 1) � C F� dr= f (1, 2, 1)� f (0, 1, �1)=6�(�1)=7 f x(x, y, z)=y 2 cos z f (x, y, z)=xy 2 cos z+g(y, z) f y(x, y, z)=2xycos z+gy(y, z) f y(x, y, z)=2xycos z gy(y, z)=0 g(y, z)=h(z) f (x, y, z)=xy 2 cos z+h(z) f z(x, y, z)=�xy 2 sin z+h / (z) f z(x, y, z)=�xy 2 sin z h / (z)=0 h(z)=K f (x, y, z)=xy 2 cos z K=0 r(0)= 0, 0, 0 r(� )= � 2 , 0,� � C F� dr= f (� 2 , 0,� )� f (0, 0, 0)=0�0=0 f x(x, y, z)=e y f (x, y, z)=xe y +g(y, z) f y(x, y, z)=xe y +gy(y, z) f y(x, y, z)=xe y gy(y, z)=0 g(y, z)=h(z) f (x, y, z)=xe y +h(z) f z(x, y, z)=0+h / (z) f z(x, y, z)=(z+1)e z (b) The initial point of is and the terminal point is , so . 14. (a) implies . But so . We can take , so (b) The initial point of is and the terminal point is , so . 15. (a) implies and so . But so . Thus and . But , so . Hence (taking ). (b) . 16. (a) implies and so . But so . Thus and . But , so . Hence (taking ). (b) corresponds to the point and corresponds to , so . 17. (a) implies and so . But so . Thus and . But , so . Hence (taking ). (b) , so . 18. (a) implies and so . But so . Thus and . But , so 3 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.3 The Fundamental Theorem for Line Integrals h / (z)=(z+1)e z h(z)=ze z +K f (x, y, z)=xe y +ze z K=0 r(0)= 0, 0, 0 r(1)= 1, 1, 1 �CF� dr= f (1, 1, 1)� f (0, 0, 0)=2e�0=2e F(x, y)=tan y i+xsec 2 y j f (x, y)=xtan y F � f =F F � C tan ydx+xsec 2 ydy=� C F� d r= f 2, � 4 � f (1, 0)=2tan � 4 �tan 0=2 F(x, y)=(1�ye �x ) i+e �x j f (x, y)=x+ye �x F � f =F F � C (1�ye �x )dx+e �x dy=� C F� d r= f (1, 2)� f (0, 1)=(1+2e �1 )�1=2/e F(x, y)=2y 3/2 i+3x y j W =�CF� d r �(2y 3/2 )/�y=3 y=�(3x y )/�x f � f =F f x(x, y)=2y 3/2 f (x, y)=2xy 3/2 +g(y) f y(x, y)=3xy 1/2 +g / (y) f y(x, y)=3x y g / (y)=0 g(y)=K K=0 f (x, y)=2xy 3/2 W =� C F� d r= f (2, 4)� f (1, 1)=2(2)(8)�2(1)=30 F(x, y)= y 2 x 2 i� 2y x j W =�CF� dr � �y y 2 x 2 = 2y x 2 = � �x � 2y x f � f =F f x=y 2 /x 2 f (x, y)=�y 2 /x+g(y) f y=�2y/x+g / (y) g / (y)=0 f (x, y)=�y 2 /x F W =�CF� dr= f (4, �2)� f (1, 1)=�[(�2) 2 /4]+(1/1)=0 F C �CF� dr=0 C C C C (using integration by parts). Hence (taking ). (b) , so . 19. Here . Then is a potential function for , that is, so is conservative and thus its line integral is independent of path. Hence . 20. Here . Then is a potential function for , that is, so is conservative and thus its line integral is independent of path. Hence . 21. , . Since , there exists a function such that . In fact, . But so or . We can take . Thus . 22. , . Since , there exists a function such that . In fact, , so we can take as a potential function for . Thus . 23. We know that if the vector field (call it ) is conservative, then around any closed path, . But take to be some circle centered at the origin, oriented counterclockwise. All of the field vectors along oppose motion along , so the integral around will be negative. Therefore the field is not conservative. 24. 4 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.3 The Fundamental Theorem for Line Integrals F � �y (2xy+sin y)=2x+cos y � �x (x 2 +xcos y)=2x+cos y F F (2, 1) �F� dr�0 � �y x�2y 1+x 2 +y 2 =(x�2y) �y (1+x 2 +y 2 ) 3/2 � 2 1+x 2 +y 2 = �2�2x 2 �xy (1+x 2 +y 2 ) 3/2 � �x x�2 1+x 2 +y 2 =(x�2) �x (1+x 2 +y 2 ) 3/2 + 1 1+x 2 +y 2 = 1+y 2 +2x (1+x 2 +y 2 ) 3/2 � f (x, y)=cos (x�2y) i�2cos (x�2y) j � C1 F� dr=� C1 � f � dr= f (r(b))� f (r(a)) C 1 t=a t=b f (0, 0)=sin 0=0 f (� ,� )=sin (� �2� )=0 C 1 (0, 0) (� ,� ) r(t)=� t i+� t j 0� t� 1 � C2 F� dr= f (r(b))� f (r(a)) f (0, 0)=sin 0=0 f � 2 ,0 =1 C 2 r(t)= � 2 t i 0� t� 1 (0, 0) � 2 , 0 From the graph, it appears that is conservative, since around all closed paths, the number and size of the field vectors pointing in directions similar to that of the path seem to be roughly the same as the number and size of the vectors pointing in the opposite direction. To check, we calculate , Thus is conservative, by Theorem 6. 25. From the graph, it appears that is not conservative. For example, any closed curve containing the point seems to have many field vectors pointing counterclockwise along it, and none pointing clockwise. So along this path the integral . To confirm our guess, we calculate , . These are not equal, so the field is not conservative, by Theorem 5. 26. (a) We use Theorem 2: where starts at and ends at . So because and , one possible curve is the straight line from to ; that is, , . (b) From (a), . So because and , one possible curve is , , the straight line from to . 5 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.3 The Fundamental Theorem for Line Integrals F f F=� f P= f x Q= f y R= f z P Q R �P/�y= f xy= f yx=�Q/�x �P/�z= f xz= f zx=�R/�x �Q/�z= f yz= f zy=�R/�y F(x, y, z)=y i+x j+xyzk �P/�z=0 �R/�x=yz F F D={ (x, y) | x>0, y>0 }= D D D D D D D � D={ (x, y) | x�0 } xy � y � D y � D D D � D={ (x, y) | 1<x 2 +y 2 <4 }= (0, 0) 1 2 D D D � x 2 +y 2 =(1.5) 2 D D D � D={ (x, y) | x 2 +y 2 � 1 4� x 2 +y 2 � 9 }= x 2 +y 2 =1 x 2 +y 2 =4 x 2 +y 2 =9 D (0, 2) D D (0, 0) (0, 2.5) D D D � x 2 +y 2 =9 D D P=� y x 2 +y 2 �P �y = y 2 �x 2 (x 2 +y 2 ) 2 Q= x x 2 +y 2 �Q �x = y 2 �x 2 (x 2 +y 2 ) 2 �P �y = �Q �x C 1 x=cos t y=sin t 0� t�� C 2 x=cos t y=sin t t=2� t=� 27. Since is conservative, there exists a function such that , that is, , , and . Since , and have continuous first order partial derivatives, Clairaut’s Theorem says that , , and . 28. Here . Then using the notation of Exercise 27, while . Since these aren’t equal, is not conservative. Thus by Theorem 4, the line integral of is not independent of path. 29. the first quadrant (excluding the axes). (a) is open because around every point in we can put a disk that lies in . (b) is connected because the straight line segment joining any two points in lies in . (c) is simply connected because it’s connected and has no holes. 30. consists of all points in the plane except for those on the axis. (a) is open. (b) Points on opposite sides of the axis cannot be joined by a path that lies in , so is not connected. (c) is not simply connected because it is not connected. 31. the annular region between the circles with center and radii and . (a) is open. (b) is connected. (c) is not simply connected. For example, is simple and closed and lies within but encloses points that are not in . (Or we can say, has a hole, so is not simply connected.) 32. or the points on or inside the circle , together with the points on or between the circles and . (a) is not open because, for instance, no disk with center lies entirely within . (b) is not connected because, for example, and lie in but cannot be joined by a path that lies entirely in . (c) is not simply connected because, for example, is a simple closed curve in but encloses points that are not in . 33. (a) , and , . Thus . (b) : , , , : , , to . Then 6 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.3 The Fundamental Theorem for Line Integrals � C1 F� dr=�� 0 (�sin t)(�sin t)+(cos t)(cos t) cos 2 t+sin 2 t dt=�� 0 dt=� � C2 F� dr=�� 2� dt=�� F � C3 F� dr=�2� 0 dt=2� C 3 x 2 +y 2 =1 F R 2 � F(r)=cr/ |r| 3 r=x i+y j+zk f (r)=�c/ |r| F � f =F F P 1 =(x 1 , y 1 , z 1 ) P 2 =(x 2 , y 2 , z 2 ) W =�CF� dr= f (P2)� f (P1)=� c (x 2 2 +y 2 2 +z 2 2 ) 1/2 + c (x 2 1 +y 2 1 +z 2 1 ) 1/2 =c 1 d 1 � 1 d 2 c=�(mMG) W = �mMG 1 1.52 10 8 � 1 1.47 10 8 = �(5.97 10 24 )(1.99 10 30 )(6.67 10 �11 )(�2.2377 10 �10 )�1.77 10 35 J c=� qQ W =� qQ 1 10 �12 � 1 5 10 �13 =(8.985 10 10 )(1)(�1.6 10 �19 )(�10 12 )�1.4 10 4 and Since these aren’t equal, the line integral of isn’t independent of path. (Or notice that where is the circle , and apply the contrapositive of Theorem 3). This doesn’t contradict Theorem 6, since the domain of , which is except the origin, isn’t simply connected. 34. (a) Here and . Then is a potential function for , that is, . (See the discussion of gradient fields in Section 17.1). Hence is conservative and its line integral is independent of path. Let and . . (b) In this case, (c) In this case, J. 7 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.3 The Fundamental Theorem for Line Integrals C 1 x=t � dx=dt y=0� dy=0dt 0� t� 2 C 2 x=2� dx=0dt y=t � dy=dt 0� t� 3 C 3 x=2�t � dx=�dt y=3� dy=0dt 0� t� 2 C 4 x=0� dx=0dt y=3�t � dy=�dt 0� t� 3 � C xy 2 dx+x 3 dy � C1+C2+C3+C4 xy 2 dx+x 3 dy =� 0 2 0dt+� 0 3 8dt+� 0 2 �9(2�t)dt+� 0 3 0dt =0+24�18+0=6 � C xy 2 dx+x 3 dy =�� D � �x (x 3 )� � �y (xy 2 ) dA=� 0 2 � 0 3 (3x 2 �2xy)dydx =� 0 2 (9x 2 �9x)dx=24�18=6 x=cos t y=sin t 0� t� 2� � C ydx�xdy=� 0 2� [sin t(�sin t)�cos t(cos t)]dt=� � 0 2� dt=�2� � C ydx�xdy=�� D � �x (�x)� � �y (y) dA=�2��D dA=�2A(D)=�2� (1) 2 =�2� 1. (a) : , , . : , , . : , , . : , , . Thus (b) 2. (a) , , . Then . (b) 3. (a) 1 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.4 Green’s Theorem C 1 x=t � dx=dt y=0� dy=0dt 0� t� 1C 1 x=t � dx=dt y=0� dy=0dt 0� t� 1 C 2 x=1� dx=0dt y=t � dy=dt 0� t� 2C 2 x=1� dx=0dt y=t � dy=dt 0� t� 2 C 3 x=1�t � dx=�dt y=2�2t � dy=�2dt 0� t� 1C 3 x=1�t � dx=�dt y=2�2t � dy=�2dt 0� t� 1 � C xydx+x 2 y 3 dy = � C1+C2+C3 xydx+x 2 y 3 dy =� 0 1 0dt+� 0 2 t 3 dt+� 0 1 �(1�t)(2�2t)�2(1�t) 2 (2�2t) 3 dt =0+ 1 4 t 4 2 0 + 2 3 (1�t) 3 + 8 3 (1�t) 6 1 0 =4� 10 3 = 2 3 � C xydx+x 2 y 3 dy =�� D � �x (x 2 y 3 )� � �y (xy) dA=�0 1 � 0 2x (2xy 3 �x)dydx =� 0 1 1 2 xy 4 �xy y=2x y=0 dx=� 0 1 (8x 5 �2x 2 )dx= 4 3 � 2 3 = 2 3 C 1 :x=0� dx=0dty=1�t� dy=�dt 0� t� 1 C 2 :x=t � dx=dt y=0� dy=0dt 0� t� 1 C 3 :x=1�t � dx=�dt y=1�(1�t) 2 =2t�t 2 � dy=(2�2t)dt 0� t� 1 : , , : , , : , , . : , , . : , , . : , , . ThusThus (b) 4. (a) , , , , , , Thus 2 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.4 Green’s Theorem � C xdx+ydy = � C1+C2+C3 xdx+ydy =� 0 1 (0dt+(1�t)(�dt))+� 0 1 (t dt+0dt)+� 0 1 ((1�t)(�dt)+(2t�t 2 )(2�2t)dt) = 1 2 t 2 �t 1 0 + 1 2 t 2 1 0 + 1 2 t 4 �2t 3 + 5 2 t 2 �t 1 0 =� 1 2 + 1 2 + 1 2 �2+ 5 2 �1 =0 � C xdx+ydy=�� D � �x (y)� � �y (x) dA=��D 0dA=0 C x=cos� y=sin� 0��� 2� � C Pdx+Qdy=� 0 2� cos 4 � sin 5 � (�sin� )d� +� 0 2� (�cos 7 � sin 6 � )cos� d� =� 29� 1024 �� D �Q �x � �P �y dA=��1 1 � � 1�x 2 1�x 2 (�7x 6 y 6 �5x 4 y 4 )dydx=� 29� 1024 y=x 2 C y=x � C Pdx+Qdy = � 0 1 x 4 sin x+x 2 sin (x 2 )(2x) dx+� 1 0 (x 2 sin x+x 2 sin x)dx = �16cos 1�23sin 1+28 (b) 5. We can parametrize as , , . Then the line integral is , according to a CAS. The double integral is , verifying Green’s Theorem in this case. 6. Since along the first part of and along the second part, the line integral is according to a CAS. The double integral is 3 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.4 Green’s Theorem �� R �Q �x � �P �y dA=�0 1 � x 2 x (2xsin y�2ysin x)dydx=�16cos 1�23sin 1+28 D C [0, 1]� [0, 1] � C e y dx+2xe y dy =�� D � �x (2xe y )� � �y (e y ) dA=� 0 1 � 0 1 (2e y �e y )dydx =� 0 1 dx� 0 1 e y dy=(1)(e 1 �e 0 )=e�1 D C { (x, y) | 0� x� 1, 3x� y� 3 } � C x 2 y 2 dx+4xy 3 dy =�� D � �x (4xy 3 )� � �y (x 2 y 2 ) dA=� 0 1 � 3x 3 (4y 3 �2x 2 y)dydx =� 0 1 y 4 �x 2 y 2 y=3 y=3xdx=�0 1 (81�9x 2 �72x 4 )dx=81�3� 72 5 = 318 5 � C (y+e x )dx+(2x+cos y 2 )dy =�� D � �x (2x+cos y 2 )� � �y (y+e x ) dA =� 0 1 � y 2 y (2�1)dxdy=� 0 1 (y 1/2 �y 2 )dy= 1 3 � C xe �2x dx+(x 4 +2x 2 y 2 )dy =�� D � �x (x 4 +2x 2 y 2 )� � �y (xe �2x ) dA=�� D (4x 3 +4xy 2 �0)dA =4�� D x(x 2 +y 2 )dA=4� 0 2� � 1 2 (rcos� )(r 2 )rdr d� =4� 0 2� cos� d� � 1 2 r 4 dr=4 sin� 2� 0 1 5 r 5 2 1 =0 7. The region enclosed by is , so 8. The region enclosed by is given by , so 9. 10. 11. 4 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.4 Green’s Theorem � C y 3 dx�x 3 dy =�� D � �x (�x 3 )� � �y (y 3 ) dA=�� D (�3x 2 �3y 2 )dA=� 0 2� � 0 2 (�3r 2 )rdr d� =�3� 0 2� d� � 0 2 r 3 dr=�3(2� )(4)=�24� � C sin ydx+xcos ydy=�� D � �x (xcos y)� � �y (sin y) dA=��D (cos y�cos y)dA=�� D 0dA=0 F(x, y)= x +y 3 , x 2 + y D C { (x, y) | 0� x�� , 0� y� sin x }.C �C � C F� dr =� � �C x +y 3( )dx+ x2+ y( )dy=��� D � �x x 2 + y( )� ��y x +y 3( ) dA =�� 0 � � 0 sin x (2x�3y 2 )dydx=�� 0 � 2xy�y 3 y=sin x y=0 dx =�� 0 � (2xsin x�sin 3 x)dx=�� 0 � (2xsin x�(1�cos 2 x)sin x)dx =� 2sin x�2xcos x+cos x� 1 3 cos 3 x � 0 =� 2� �2+ 2 3 = 4 3 �2� F(x, y)= y 2 cos x, x 2 +2ysin x D C { (x, y) | 0� x� 2, 0� y� 3x } C �C � C F� dr =� � �C (y 2 cos x)dx+(x 2 +2ysin x)dy =��� D � �x (x 2 +2ysin x)� � �y (y 2 cos x) dA =��� D (2x+2ycos x�2ycos x)dA=�� 0 2 � 0 3x 2xdydx 12. 13. and the region enclosed by is given by is traversed clockwise, so gives the positive orientation. 14. and the region enclosed by is given by . is traversed clockwise, so gives the positive orientation. 5 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.4 Green’s Theorem =�� 0 2 2x y y=3x y=0 dx=��0 2 6x 2 dx= �2x 3 2 0 =�16 F(x, y)= e x +x 2 y, e y �xy 2 D C x 2 +y 2 � 25 C �C � C F� dr =� � �C (e x +x 2 y)dx+(e y �xy 2 )dy =��� D � �x (e y �xy 2 )� � �y (e x +x 2 y) dA=��� D (�y 2 �x 2 )dA =�� D (x 2 +y 2 )dA=� 0 2� � 0 5 (r 2 )rdr d� =� 0 2� d� � 0 5 r 3 dr=2� 1 4 r 4 5 0 = 625 2 � F x, y( )= y�ln (x2+y2), 2tan �1 yx D C 1 (2, 3).C �CF� d r =� C (y�ln (x 2 +y 2 ))dx+ 2tan �1 y x dy =�� D � �x 2tan �1 y x � � �y (y�ln (x 2 +y 2 )) dA =�� D 2 �yx �2 1+(y/x) 2 � 1� 2y x 2 +y 2 dA=�� D � 2y x 2 +y 2 �1+ 2y x 2 +y 2 dA =��� D dA=�( D)=�� W =� C F� dr=� C x(x+y)dx+xy 2 dy=�� D (y 2 �x)dydx C D C W = � 0 1 � 0 1�x (y 2 �x)dydx=� 0 1 1 3 y 3 �xy y=1�x y=0 dx=� 0 1 1 3 (1�x) 3 �x(1�x) dx 15. and the region enclosed by is the disk . is traversed clockwise, so gives the positive orientation. 16. and the region enclosed by is the disk with radius centered at is oriented positively, so area of 17. By Green’s Theorem, where is the path described in the question and is the triangle bounded by . So 6 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.4 Green’s Theorem = � 1 12 (1�x) 4 � 1 2 x 2 + 1 3 x 3 1 0 = � 1 2 + 1 3 � � 1 12 =� 1 12 W =� C F� dr=� C xdx+(x 3 +3xy 2 )dy=�� D (3x 2 +3y 2 �0)dA D C W =3� 0 2 � 0 � r 2 � rd� dr=3� 1 4 r 4 2 0 =12� C 1 (0, 0) (2� , 0) 0� t� 2� C 2 (2� , 0) (0, 0) C 2 x=2� �t y=0 0� t� 2� . C=C 1 C 2 �C �C A=� � �C ydx =� C1 ydx+� C2 ydx=� 0 2� (1�cos t)(1�cos t)dt+� 0 2� 0(�dt) =� 0 2� (1�2cos t+cos 2 t)dt+0= t�2sin t+ 1 2 t+ 1 4 sin 2t 2� 0 =3� A= � C xdy=� 0 2� (5cos t�cos 5t)(5cos t�5cos 5t)dt =� 0 2� (25cos 2 t�30cos tcos 5t+5cos 2 5t)dt = 25 1 2 t+ 1 4 sin 2t �30 1 8 sin 4t+ 1 12 sin 6t +5 1 2 t+ 1 20 sin 10t 2� 0 =30� x=(1�t)x 1 +tx 2 y=(1�t)y 1 +ty 2 0� t� 1 dx=(x 2 �x 1 )dt dy=(y 2 �y 1 )dt � C xdy�ydx = � 0 1 [(1�t)x 1 +tx 2 ](y 2 �y 1 )dt+[(1�t)y 1 +ty 2 ](x 2 �x 1 )dt 18. By Green’s Theorem, , where is the semicircular region bounded by . Converting to polar coordinates, we have . 19. Let be the arch of the cycloid from to , which corresponds to , and let be the segment from to , so is given by , , Then is traversed clockwise, so is oriented positively. Thus encloses the area under one arch of the cycloid and from (5) we have 20. 21. (a) Using Equation 17.2.8 , we write parametric equations of the line segment as , , . Then and , so 7 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.4 Green’s Theorem = � 0 1 (x 1 (y 2 �y 1 )�y 1 (x 2 �x 1 )+t [(y 2 �y 1 )(x 2 �x 1 )�(x 2 �x 1 )(y 2 �y 1 )])dt = � 0 1 (x 1 y 2 �x 2 y 1 )dt=x 1 y 2 �x 2 y 1 C=C 1 C 2 � � � Cn Ci (xi, yi) (xi+1, yi+1) i=1 2 .. . n�1 Cn (xn, yn) (x1, y1) 1 2 �C xdy�ydx=�� D dA D C =A(D)=�� D dA= 1 2 �C xdy�ydx = 12 � C1 xdy�ydx+� C2 xdy�ydx+...+ � Cn�1 xdy�ydx+� Cn xdy�ydx A(D)=[(x 1 y 2 �x 2 y 1 )+(x 2 y 3 �x 3 y 2 )+...+(xn�1yn�xnyn�1)+(xny1�x1yn)]. A = 1 2 [(0� 1�2� 0)+(2� 3�1� 1)+(1� 2�0� 3)+(0� 1�(�1)� 2)+(�1� 0�0� 1)] = 1 2 (0+5+2+2)= 9 2 1 2A �C x 2 dy= 1 2A ��D 2xdA= 1 A ��D xdA=x � 1 2A �C y 2 dx=� 1 2A ��D (�2y)dA= 1 A ��D ydA=y A= 1 2 (1)(1)= 1 2 C=C1+C2+C3 C1 x=x y=0 0� x� 1 C 2 x=x y=1�x x=1 x=0 C 3 x=0 y=1 y=0 x= 1 2A �C x 2 dy=� C1 x 2 dy+� C2 x 2 dy+� C3 x 2 dy=0+� 1 0 (x 2 )(�dx)+0= 1 3 . (b) We apply Green’s Theorem to the path , where is the line segment that joins to for , , , , and is the line segment that joins to . From (5), , where is the polygon bounded by . Therefore area of polygon To evaluate these integrals we use the formula from (a) to get (c) 22. By Green’s Theorem, and . 23. Here and , where : , , ; : , , to ; and : , to . Then Similarly, 8 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.4 Green’s Theorem y=� 1 2A �C y 2 dx=� C1 y 2 dx+� C2 y 2 dx+� C3 y 2 dx=0+� 1 0 (1�x) 2 (�dx)+0= 1 3 . (x, y)= 1 3 , 1 3 . A= � a 2 2 x= 1 � a 2 � C x 2 dy y=� 1 � a 2 � C y 2 dx. x = 1 � a 2 � C1+C2 x 2 dy = 1 � a 2 0+� 0 � (a 2 cos 2 t)(acos t)dt =0 y=� 1 � a 2 � �a a 0dx+� 0 � (a 2 sin 2 t)(�asin t)dt = a � �0 � sin 3 tdt= a � �cos t+ 1 3 (cos 3 t) � 0 = 4a 3� (x, y)= 0, 4a 3� � 1 3 � �C y 3 dx=� 1 3 ���D (�3y 2 )dA=�� D y 2 �dA=Ix 1 3 � �C x 3 dy= 1 3 ���D (3x 2 )dA=�� D x 2 �dA=Iy Therefore 24. so and Orienting the semicircular region as in the figure, and . Thus . 25. By Green’s Theorem, and . 26. By symmetry the moments of inertia about any two diameters are equal. Centering the disk at the origin, the moment of inertia about a diameter equals 9 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.4 Green’s Theorem Iy = 1 3 � �C x 3 dy= 1 3 � �0 2� (a 4 cos 4 t)dt= 1 3 a 4 � � 0 2� 3 8 + 1 2 cos 2t+ 1 8 cos 4t dt = 13 a 4 � � 3(2� ) 8 = 1 4 � a 4 � C D P=�y/(x 2 +y 2 ) Q=x/(x 2 +y 2 ) D �P/�y=�Q/�x � C F� dr=�� D 0dA=0 D D={ (x, y) | f 1 (y)� x� f 2 (y), c� y� d } f 1 f 2 �� D �Q �x dA=�c d � f 1(y) f 2(y) �Q �x dxdy=�c d Q( f 2 (y), y)�Q( f 1 (y), y) dy � C Qdy= � C1+C2+C3+C4 Qdy. � C1 Qdy=� d c Q( f 1 (y), y)dy � C2 Qdy=� C4 Qdy=0 � C3 Qdy=� c d Q( f 2 (y), y)dy � C Qdy=� c d Q( f 2 (y), y)�Q( f 1 (y), y) dy=�� D (�Q/�x)dA. �� R dxdy=A(R)=� �R xdy x=g(u, v) dy= �h �u du+ �h �v dv �S �R 27. Since is a simple closed path which doesn’t pass through or enclose the origin, there exists an open region that doesn’t contain the origin but does contain . Thus and have continuous partial derivatives on this open region containing and we can apply Green’s Theorem. But by Exercise 17.3.33(a) , , so . 28. We express as a type II region: where and are continuous functions. Then by the Fundamental Theorem of Calculus. But referring to the figure, Then , , and . Hence 29. Using the first part of (5), we have that . But , and , and we orient by taking the positive direction to be that which corresponds, under the mapping, to the positive direction along , so 10 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.4 Green’s Theorem � �R xdy = � �S g(u, v) �h �u du+ �h �v dv =��S g(u, v) �h �u du+g(u, v) �h �v dv = ��S � �u g(u, v) �h �v � � �v g(u, v) �h �u dA uv � = �� S �g �u �h �v +g(u, v) � 2 h �u�v � �g �v �h �u �g(u, v) � 2 h �v�u dA = �� S �x �u �y �v � �x �v �y �u dA = ��S �(x, y) �(u, v) dudv �S A(R) �(x, y) �(u, v) A(R)=��R dxdy=�� S �(x, y) �(u, v) dudv. [using Green’s Theorem in the plane] [by the equality of mixed partials] The sign is chosen to be positive if the orientation that we gave to corresponds to the usual positive orientation, and it is negative otherwise. In either case, since is positive, the sign chosen must be the same as the sign of . Therefore 11 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.4 Green’s Theorem F =��F= i �/�x xyz j �/�y 0 k �/�z �x 2 y =(�x 2 �0) i�(�2xy�xy) j+(0�xz)k =�x 2 i+3xy j�xzk F=��F= � �x (xyz)+ � �y (0)+ � �z (�x 2 y)=yz+0+0=yz curlF =��F= i �/�x x 2 yz j �/�y xy 2 z k �/�z xyz 2 =(xz 2 �xy 2 ) i�(yz 2 �x 2 y) j+(y 2 z�x 2 z)k =x(z 2 �y 2 ) i+y(x 2 �z 2 ) j+z(y 2 �x 2 )k F=��F= � �x (x 2 yz)+ � �y (xy 2 z)+ � �z (xyz 2 )=2xyz+2xyz+2xyz=6xyz curlF =��F= i �/�x 1 j �/�y x+yz k �/�z xy� z =(x�y) i�(y�0) j+(1�0)k =(x�y) i�y j+k F=��F= � �x (1)+ � �y (x+yz)+ � �z (xy� z )=z� 1 2 z curlF =��F= i �/�x 0 j �/�y cos xz k �/�z �sin xy =(�xcos xy+xsin xz) i�(�ycos xy�0) j+(�zsin xz�0)k =x(sin xz�cos xy) i+ycos xy j�zsin xzk F=��F= � �x (0)+ � �y (cos xz)+ � �z (�sin xy)=0+0+0=0 1. (a) curl (b) div 2. (a) (b) div 3. (a) (b) div 4. (a) (b) div 1 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence F=��F= i �/�x e x sin y j �/�y e x cos y k �/�z z =(0�0)i�(0�0) j+(e x cos y�e x cos y)k=0 F=��F= � �x (e x sin y)+ � �y (e x cos y)+ � �z (z)=e x sin y�e x sin y+1=1 F =��F= i �/�x x x 2 +y 2 +z 2 j �/�y y x 2 +y 2 +z 2 k �/�z z x 2 +y 2 +z 2 = 1 (x 2 +y 2 +z 2 ) 2 [(�2yz+2yz) i�(�2xz+2xz) j+(�2xy+2xy)k]=0 F =��F= � �x x x 2 +y 2 +z 2 + � �y y x 2 +y 2 +z 2 + � �z z x 2 +y 2 +z 2 = x 2 +y 2 +z 2 �2x 2 (x 2 +y 2 +z 2 ) 2 + x 2 +y 2 +z 2 �2y 2 (x 2 +y 2 +z 2 ) 2 + x 2 +y 2 +z 2 �2z 2 (x 2 +y 2 +z 2 ) 2 = x 2 +y 2 +z 2 (x 2 +y 2 +z 2 ) 2 = 1 x 2 +y 2 +z 2 curlF =��F= i �/�x ln x j �/�y ln (xy) k �/�z ln (xyz) = xz xyz �0 i� yz xyz �0 j+ y xy �0 k = 1 y , � 1 x , 1 x F=��F= � �x (ln x)+ � �y (ln (xy))+ � �z (ln (xyz))= 1 x + x xy + xy xyz = 1 x + 1 y + 1 z 5. (a) curl (b) div 6. (a) curl (b) div 7. (a) (b) div 8. (a) 2 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence curlF =��F= i �/�x xe �y j �/�y xz k �/�z ze y =(ze y �x) i�(0�0) j+(z�xe �y (�1))k = ze y �x, 0, z+xe �y F=��F= � �x (xe �y )+ � �y (xz)+ � �z (ze y )=e �y +0+e y =e y +e �y F=P i+Q j+Rk R=0 x � F 0 P=0 �P �x = �P �y = �P �z = �R �x = �R �y = �R �z =0 Q y �Q �y <0 Q x � z � �Q �x = �Q �z =0 divF= �P �x + �Q �y + �R �z =0+ �Q �y +0<0 curlF= �R �y � �Q �z i+ �P �z � �R �x j+ �Q �x � �P �y k=(0�0) i+(0�0) j+(0�0)k=0 F=P i+Q j+Rk R=0 P Q z � �R �x = �R �y = �R �z = �P �z = �Q �z =0 x x � F y � �P �x >0 �Q �x =0y y � x � �Q �y >0 �P �y =0 divF= �P �x + �Q �y + �R �z = �P �x + �Q �y +0>0 curlF= �R �y � �Q �z i+ �P �z � �R �x j+ �Q �x � �P �y k=(0�0) i+(0�0) j+(0�0)k=0 F=P i+Q j+Rk R=0 y � F 0 Q=0 �Q �x = �Q �y = �Q �z = �R �x = �R �y = �R �z =0 P y �P �y >0 P x � z � �P �x = �P �z =0 (b) div 9. If the vector field is , then we know . In addition, the component of each vector of is , so , hence . decreases as increases, so , but doesn’t change in the or directions, so . (a) (b) 10. If the vector field is , then we know . In addition, and don’t vary in the direction, so . As increases, the component of each vector of increases while the component remains constant, so and . Similarly, as increases, the component of each vector increases while the component remains constant, so and . (a) (b) 11. If the vector field is , then we know . In addition, the component of each vector of is , so , hence . increases as increases, so , but doesn’t change in the or directions, so . 3 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence divF= �P �x + �Q �y + �R �z =0+0+0=0 curlF = �R �y � �Q �z i+ �P �z � �R �x j+ �Q �x � �P �y k =(0�0)i+(0�0) j+ 0� �P �y k=� �P �y k �P �y >0 � �P �y k z � curl f =�� f f grad f divF curl(grad f ) gradF F grad(divF) div(grad f ) grad(div f ) f curl(curlF) div(divF) divF (grad f )� (divF) divF div(curl(grad f )) F=��F= i �/�x yz j �/�y xz k �/�z xy =(x�x) i�(y�y) j+(z�z)k=0 F R 3 F f F=� f f x(x, y, z)=yz f (x, y, z)=xyz+g(y, z) f y(x, y, z)=xz+gy(y, z) f y(x, y, z)=xz g(y, z)=h(z) f (x, y, z)=xyz+h(z) f z(x, y, z)=xy+h / (z) f z(x, y, z)=xy h(z)=K F f (x, y, z)=xyz+K F=��F= i �/�x 3z 2 j �/�y cos y k �/�z 2xz =(0�0) i�(2z�6z) j+(0�0)k=4z j�0 F (a) (b) Since , is a vector pointing in the negative direction. 12. (a) is meaningless because is a scalar field. (b) is a vector field. (c) is a scalar field. (d) is a vector field. (e) is meaningless because is not a scalar field. (f) is a vector field. (g) is a scalar field. (h) is meaningless because is a scalar field. (i) is a vector field. (j) is meaningless because is a scalar field. (k) is meaningless because is a scalar field. (l) is a scalar field. 13. curl and is defined on all of with component functions which have continuous partial derivatives, so by Theorem 4, is conservative. Thus, there exists a function such that . Then implies and . But , so and . Thus but so , a constant. Hence a potential function for is . 14. curl , so is not conservative. 4 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence F=��F= i �/�x 2xy j �/�y x 2 +2yz k �/�z y 2 =(2y�2y) i�(0�0) j+(2x�2x)k=0 F R 3 F f � f =F f x(x, y, z)=2xy f (x, y, z)=x 2 y+g(y, z) f y(x, y, z)=x 2 +gy(y, z) f y(x, y, z)=x 2 +2yz g(y, z)=y 2 z+h(z) f (x, y, z)=x 2 y+y 2 z+h(z) f z(x, y, z)=y 2 +h / (z) f z(x, y, z)=y 2 h(z)=K f (x, y, z)=x 2 y+y 2 z+K F=��F= i �/�x e z j �/�y 1 k �/�z xe z =(0�0) i�(e z �e z ) j+(0�0)k=0 F R 3 F f � f =F f x(x, y, z)=e z f (x, y, z)=xe z +g(y, z)� f y(x, y, z)=gy(y, z). f y(x, y, z)=1 g(y, z)=y+h(z) f (x, y, z)=xe z +y+h(z) f z(x, y, z)=xe z +h / (z) f z(x, y, z)=xe z h(z)=K F f (x, y, z)=xe z +y+K F=��F= i �/�x ye �x j �/�y e �x k �/�z 2z =(0�0) i�(0�0) j+(�e �x �e �x )k=�2e �x k�0 F curlF =��F= i �/�x ycos xy j �/�y xcos xy k �/�z �sin z =(0�0) i�(0�0) j+[(�xysin xy+cos xy)�(�xysin xy+cos xy)]k=0 F R 3 F f � f =F f x(x, y, z)=ycos xy f (x, y, z)=sin xy+g(y, z)� f y(x, y, z)=xcos xy+gy(y, z) f y(x, y, z)=xcos xy g(y, z)=h(z) f (x, y, z)=sin xy+h(z) f z(x, y, z)=h / (z) f z(x, y, z)=�sin z h(z)=cos z+K 15. curl , is defined on all of , and the partial derivatives of the component functions are continuous, so is conservative. Thus there exists a function such that . Then implies and . But , so and . Thus but so and . 16. curl and is defined on all of with component functions that have continuous partial deriatives, so is conservative. Thus there exists a function such that . Then implies But , so and . Thus but , so , a constant. Hence a potential function for is . 17. curl , so is not conservative. 18. is defined on all of , and the partial derivatives of the component functions are continuous, so is conservative. Thus there exists a function such that . Then implies . But , so and . Thus but so and a potential 5 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence F f (x, y, z)=sin xy+cos z+K G div(curlG)=y 2 +z 2 +x 2 �0 G div(curlG)=xz�0 curlF= i �/�x f (x) j �/�y g(y) k �/�z h(z) =(0�0)i+(0�0) j+(0�0)k=0 F= f (x) i+g(y) j+h(z)k divF= �( f (y, z)) �x + �(g(x, z)) �y + �(h(x, y)) �z =0 F div(F+G) = �(P 1 +P 2 ) �x + �(Q 1 +Q 2 ) �y + �(R 1 +R 2 ) �z = �P 1 �x + �Q 1 �y + �R 1 �z + �P 2 �x + �Q 2 �y + �R 3 �z =divF+divG curlF+curlG= �R 1 �y � �Q 1 �z i+ �P 1 �z � �R 1 �x j+ �Q 1 �x � �P 1 �y k + �R 2 �y � �Q 2 �z i+ �P 2 �z � �R 2 �x j+ �Q 2 �x � �P 2 �y k = �(R 1 +R 2 ) �y � �(Q 1 +Q 2 ) �z i+ �(P 1 +P 2 ) �z � �(R 1 +R 2 ) �x j + �(Q 1 +Q 2 ) �x � �(P 1 +P 2 ) �y k=curl F+G( ) div fF( ) = �( fP 1 ) �x + �( fQ 1 ) �y + �( fR 1 ) �z = f �P 1 �x +P1 � f �x + f �Q 1 �y +Q1 � f �y + f �R 1 �z +R1 � f �z function for is . 19. No. Assume there is such a . Then , which contradicts Theorem 11. 20. No. Assume there is such a . Then which contradicts Theorem 11. 21. . Hence is irrotational. 22. so is incompressible. 23. 24. 25. 6 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence = f �P 1 �x + �Q 1 �y + �R 1 �z + P1, Q1, R1 � � f �x , � f �y , � f �z = f divF+F� � f curl fF( ) = �( fR 1 ) �y � �( fQ 1 ) �z i+ �( fP 1 ) �z � �( fR 1 ) �x j+ �( fQ 1 ) �x � �( fP 1 ) �y k = f �R 1 �y +R1 � f �y � f �Q 1 �z �Q1 � f �z i+ f �P 1 �z +P1 � f �z � f �R 1 �x �R1 � f �x j + f �Q 1 �x +Q1 � f �x � f �P 1 �y �P1 � f �y k = f �R 1 �y � �Q 1 �z i+ f �P 1 �z � �R 1 �x j+ f �Q 1 �x � �P 1 �y k + R 1 � f �y �Q1 � f �z i+ P1 � f �z �R1 � f �x j+ Q1 � f �x �P1 � f �y k = f curlF+ � f( )�F div(F)�G =�� (F�G)= �/�x P 1 P 2 �/�y Q 1 Q 2 �/�z R 1 R 2 = � �x Q 1 Q 2 R 1 R 2 � � �y P 1 P 2 R 1 R 2 + � �z P 1 P 2 Q 1 Q 2 = Q 1 �R 2 �x +R2 �Q 1 �x �Q2 �R 1 �x �R1 �Q 2 �x � P 1 �R 2 �y +R2 �P 1 �y �P2 �R 1 �y �R1 �P 2 �y + P 1 �Q 2 �z +Q2 �P 1 �z �P2 �Q 1 �z �Q1 �P 2 �z = P 2 �R 1 �y � �Q 1 �z +Q2 �P 1 �z � �R 1 �x +R2 �Q 1 �x � �P 1 �y � P 1 �R 2 �y � �Q 2 �z +Q1 �P 2 �z � �R 2 �x +R1 �Q 2 �x � �P 2 �y =G� curlF�F� curlG 26.27. 7 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence div(� f ��g)=�g� curl(� f )�� f � curl(�g)=0 curl curlF =�� (��F)= i �/�x �R 1 /�y��Q 1 /�z j �/�y �P 1 /�z��R 1 /�x k �/�z �Q 1 /�x��P 1 /�y = � 2 Q 1 �y�x � � 2 P 1 �y 2 � � 2 P 1 �z 2 + � 2 R 1 �z�x i+ � 2 R 1 �z�y � � 2 Q 1 �z 2 � � 2 Q 1 �x 2 + � 2 P 1 �x�y j + � 2 P 1 �x�z � � 2 R 1 �x 2 � � 2 R 1 �y 2 + � 2 Q 1 �y�z k graddivF�� 2 F � 2 F grad divF�� 2 F = � 2 P 1 �x 2 + � 2 Q 1 �x�y + � 2 R 1 �x�z i+ � 2 P 1 �y�x + � 2 Q 1 �y 2 + � 2 R 1 �y�z j + � 2 P 1 �z�x + � 2 Q 1 �z�y + � 2 R 1 �z 2 k � � 2 P 1 �x 2 + � 2 P 1 �y 2 + � 2 P 1 �z 2 i+ � 2 Q 1 �x 2 + � 2 Q 1 �y 2 + � 2 Q 1 �z 2 j + � 2 R 1 �x 2 + � 2 R 1 �y 2 + � 2 R 1 �z 2 k = � 2 Q 1 �x�y + � 2 R 1 �x�z � � 2 P 1 �y 2 � � 2 P 1 �z 2 i+ � 2 P 1 �y�x + � 2 R 1 �y�z � � 2 Q 1 �x 2 � � 2 Q 1 �z 2 j + � 2 P 1 �z�x + � 2 Q 1 �z�y � � 2 R 1 �x 2 � � 2 R 2 �y 2 k 28. (by Theorem 3) 29. Now let’s consider and compare with the above. (Note that is defined on page 1130). Then applying Clairaut’s Theorem to reverse the order of differentiation in the second partial derivatives as needed and comparing, we have 8 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence curl curlF=grad divF�� 2 F �� r= � �x i+ � �y j+ � �z k � (x i+y j+zk)=1+1+1=3 �� (rr) =�� x 2 +y 2 +z 2 (x i+y j+zk) = x 2 x 2 +y 2 +z 2 + x 2 +y 2 +z 2 + y 2 x 2 +y 2 +z 2 + x 2 +y 2 +z 2 + z 2 x 2 +y 2 +z 2 + x 2 +y 2 +z 2 = 1 x 2 +y 2 +z 2 (4x 2 +4y 2 +4z 2 )=4 x 2 +y 2 +z 2 =4r �� (rr)=div(rr)=rdivr+r� �r=3r+r� r r =4r � 2 r 3 =� 2 (x 2 +y 2 +z 2 ) 3/2 = � �x 3 2 (x 2 +y 2 +z 2 ) 1/2 (2x) + � �y 3 2 (x 2 +y 2 +z 2 ) 1/2 (2y) + � �z 3 2 (x 2 +y 2 +z 2 ) 1/2 (2z) =3 1 2 (x 2 +y 2 +z 2 ) �1/2 (2x)(x)+(x 2 +y 2 +z 2 ) 1/2 +3 1 2 (x 2 +y 2 +z 2 ) �1/2 (2y)(y)+(x 2 +y 2 +z 2 ) 1/2 +3 1 2 (x 2 +y 2 +z 2 ) �1/2 (2z)(z)+(x 2 +y 2 +z 2 ) 1/2 =3(x 2 +y 2 +z 2 ) �1/2 (4x 2 +4y 2 +4z 2 )=12(x 2 +y 2 +z 2 ) 1/2 =12r � �x (x 2 +y 2 +z 2 ) 3/2 =3x x 2 +y 2 +z 2 ��r 3 =3r (x i+y j+zk)=3r r � 2 r 3 =���r 3 =�� (3r r)=3(4r)=12r as desired. 30. (a) (b) Another method: By Exercise 25, . (c) Another method: , so by part (b). 9 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence �r =� x 2 +y 2 +z 2 = x x 2 +y 2 +z 2 i+ y x 2 +y 2 +z 2 j+ z x 2 +y 2 +z 2 k = x i+y j+zk x 2 +y 2 +z 2 = r r �� r = i � �x x j � �y y k � �z z = � �y (z)� � �z (y) i+ � �z (x)� � �x (z) j+ � �x (y)� � �y (x) k=0 � 1 r =� 1 x 2 +y 2 +z 2 = � 1 2 x 2 +y 2 +z 2 (2x) x 2 +y 2 +z 2 i� 1 2 x 2 +y 2 +z 2 (2y) x 2 +y 2 +z 2 j� 1 2 x 2 +y 2 +z 2 (2z) x 2 +y 2 +z 2 k =� x i+y j+zk (x 2 +y 2 +z 2 ) 3/2 =� r r 3 � ln r =� ln x 2 +y 2 +z 2( ) 1/2= 12 � ln x 2 +y 2 +z 2( ) = x x 2 +y 2 +z 2 i+ y x 2 +y 2 +z 2 j+ z x 2 +y 2 +z 2 k= x i+y j+zk x 2 +y 2 +z 2 = r r 2 r=x i+y j+zk�r=|r|= x 2 +y 2 +z 2 F= r r p = x (x 2 +y 2 +z 2 ) p/2 i+ y (x 2 +y 2 +z 2 ) p/2 j+ z (x 2 +y 2 +z 2 ) p/2 k 31. (a) (b) (c) (d) 32. , so 10 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence � �x x (x 2 +y 2 +z 2 ) p/2 = (x 2 +y 2 +z 2 )�px 2 (x 2 +y 2 +z 2 ) 1+ p/2 = r 2 �px 2 r p+2 � �y y (x 2 +y 2 +z 2 ) p/2 = r 2 �py 2 r p+2 � �z z (x 2 +y 2 +z 2 ) p/2 = r 2 �pz 2 r p+2 divF = ��F= r 2 �px 2 r p+2 + r 2 �py 2 r p+2 + r 2 �pz 2 r p+2 = 3r 2 �px 2 �py 2 �pz 2 r p+2 = 3r 2 �p(x 2 +y 2 +z 2 ) r p+2 = 3r 2 �pr 2 r p+2 = 3�p r p p=3 divF=0 C f (�g)� nds= D div ( f�g)dA= D [ f div(�g)+�g� � f ]dA div(�g)=� 2 g. D f� 2 gdA= C f (�g)� nds� D �g� � f dA. D f� 2 gdA= C f (�g)� nds� D �g� � f dA D g� 2 f dA= C g(� f )� nds� D � f � �gdA. D ( f� 2 g�g� 2 f )dA = C f (�g)� n�g(� f )� n ds+ D (� f � �g��g� � f )dA = C f�g�g� f � nds � =v/d sin� =d/r� v=d� =(sin� )r� =|w� r |. v w r v=w� r. v=w� r= i 0 x j 0 y k � z =(0� z�� y) i+(� x�0� z) j+(0� y�x� 0)k=�� y i+� x j curlv=�� v= i �/�x ��y j �/�y �x k �/�y 0 Then . Similarly, and . Thus Consequently, if we have . 33. By (13), by Exercise 25. But Hence 34. By Exercise 33, and Hence 35. (a) We know that , and from the diagram But is perpendicular to both and , so that (b) From (a), (c) 11 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence = � �y (0)� � �z (� x) i+ � �z (�� y)� � �x (0) j+ � �x (� x)� � �y (�� y) k =[� �(�� )]k=2� k=2w H= h 1 , h 2 , h 3 E= E 1 , E 2 , E 3 . �� (��E) =�� (curlE)=�� � 1 c �H �t =� 1 c i �/�x �h 1 /�t j �/�y �h 2 /�t k �/�z �h 3 /�t =� 1 c � 2 h 3 �y�t � � 2 h 2 �z�t i+ � 2 h 1 �z�t � � 2 h 3 �x�t j+ � 2 h 2 �x�t � � 2 h 1 �y�t k =� 1 c � �t �h 3 �y � �h 2 �z i+ �h 1 �z � �h 3 �x j+ �h 2 �x � �h 1 �y k =� 1 c � �t curlH=� 1 c � �t 1 c �E �t =� 1 c 2 � 2 E �t 2 �� (��H) =�� (curlH)=�� 1 c �E �t = 1 c i �/�x �E 1 /�t j �/�y �E 2 /�t k �/�z �E 3 /�t = 1 c � 2 E 3 �y�t � � 2 E 2 �z�t i+ � 2 E 1 �z�t � � 2 E 3 �x�t j+ � 2 E 2 �x�t � � 2 E 1 �y�t k = 1 c � �t �E 3 �y � �E 2 �z i+ �E 1 �z � �E 3 �x j+ �E 2 �x � �E 1 �y k = 1 c � �t curlE= 1 c � �t � 1 c �H �t =� 1 c 2 � 2 H �t 2 curl curlE=grad divE�� 2 E� 36. Let and (a) [assuming that the partial derivatives are continuous so that the order of differentiation does not matter] (b) [assuming that the partial derivatives are continuous so that the order of differentiation does not matter] (c) Using Exercise 29, we have that 12 Stewart Calculus ET 5e 0534393217;16. Vector Calculus; 16.5 Curl and Divergence � 2 E=grad divE�curl curlE=grad0+ 1 c 2 � 2 E �t 2 = 1 c 2 � 2 E �t 2 . � 2 H=grad divH�curl curlH=grad 0+ 1 c 2 � 2 H �t
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