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Course: MATH Cal I- Cal, Spring 2008
School: TN Tech
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Calculus Stewart ET 5e 0534393217;15. Multiple Integrals; 15.6 Surface Area 1. Here z= f (x,y)=2+3x+4y and D is the rectangle 0,5 surface is A(S) = D 1,4 , so by Formula 2 the area of the dA D [ f (x,y)] +[ f (x,y)] +1 dA= x y D 2 2 3 +4 +1 dA= 26 2 2 = 26 A(D)= 26 (5)(3)=15 26 2 2 2. z= f (x,y)=10 2x 5y and D is the disk x +y A(S) = D 9 , so by Formula 2 ( 2) +( 5) +1 dA= 30 D 2 2 dA= 30 A(D) =...

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Calculus Stewart ET 5e 0534393217;15. Multiple Integrals; 15.6 Surface Area 1. Here z= f (x,y)=2+3x+4y and D is the rectangle 0,5 surface is A(S) = D 1,4 , so by Formula 2 the area of the dA D [ f (x,y)] +[ f (x,y)] +1 dA= x y D 2 2 3 +4 +1 dA= 26 2 2 = 26 A(D)= 26 (5)(3)=15 26 2 2 2. z= f (x,y)=10 2x 5y and D is the disk x +y A(S) = D 9 , so by Formula 2 ( 2) +( 5) +1 dA= 30 D 2 2 dA= 30 A(D) = 30 ( 3 )=9 30 2 3. z= f (x,y)=6 3x 2y which intersects the xy plane in the line 3x+2y=6 , so D is the triangular region 3 . Thus given by ( x,y ) 0 x 2,0 y 3 x 2 { D } A(S) = = 14 ( 3) +( 2) +1 dA= 14 D 2 2 dA= 14 A(D) 1 2 3 =3 14 2 2 4. z= f (x,y)=1+3x+2y with 0 x 2y , 0 y 1 . Thus by Formula 2, A(S) = D 1 (3) +(4y) +1 dA= 0 0 2 2 2 1 2y 10+16y dxdy= 0 1 0 2 1 10+16y 2 x x=2y x=0 dy = 2y 0 2 2 10+16y dy= 2 1 2 2 3/2 (10+16y ) 32 3 2 1/2 = 1 3/2 3/2 (26 10 ) 24 5. y +z =9 42 z= 9 y . f =0 , f = y(9 y ) x y 2 A(S) = 0 0 42 0 +[ y(9 y ) 2 2 1/2 2 42 0 0 ] +1 dydx= y 3 y=2 y=0 y 2 2 +1 dydx 2 3 4 9 y dx=3 = 0 0 3 9 y 2 4 dydx=3 0 sin 1 sin 1 x 0 =12sin 1 2 3 1 Stewart Calculus ET 5e 0534393217;15. Multiple Integrals; 15.6 Surface Area 6. z= f (x,y)=4 x y and D is the projection of the paraboloid z=4 x y onto the xy plane, that is, D= (x,y)| x +y A(S) = D 2 2 2 2 2 { 2 2 4 2 } . So f = 2x , f = 2y x y 2 ( 2x) +( 2y) +1 dA= D 4(x +y )+1 dA= 0 0 2 2 2 2 2 4r +1 r dr d 2 = 0 1 2 3/2 (4r +1) 12 2 2 r=2 r=0 d = 0 2 2 1 ( 17 17 1 ) d = 6 ( 17 17 1 ) 12 7. z= f (x,y)=y x with 1 x +y A(S) = D 2 4 . Then 1+4r r dr d = 2 2 2 1+4x +4y dA= 0 1 2 0 2 2 2 d 0 1 r 1+4r dr 2 = 1 2 3/2 (1+4r ) 12 2 1 = 6 ( 17 17 5 5 ) 8. z= f (x,y)= A(S) = D 1 2 3/2 3/2 1/2 1/2 (x +y ) and D= { (x,y) 0 x 1,0 y 1 } . Then f =x , f =y and x y 3 ( x ) +( 2 y ) +1 dA= 00 y=1 2 11 x+y+1 dydx 1 0 1 0 3/2 3/2 = 0 2 3/2 (x+y+1) 3 2 dx= y=0 3 (x+2) = (x+1) dx 2 2 5/2 2 5/2 (x+2) (x+1) 3 5 5 4 5/2 7/2 = (3 2 +1) 15 = 9. z= f (x,y)=xy with 0 x +y A(S) = D 2 2 2 1 4 5/2 5/2 5/2 (3 2 2 +1) 15 1 , so f =y , f =x x y y +x +1 dA= 0 0 2 2 2 r +1 r dr d = 0 2 2 1 2 3/2 (r +1) 3 r=1 r=0 d = 0 1 2 ( 2 2 1) d = 3 3 (2 2 1) 2 Stewart Calculus ET 5e 0534393217;15. Multiple Integrals; 15.6 Surface Area 10. Given the sphere x +y +z =4 , when z=1 , we get x +y =3 so D= (x,y)| x +y z= f (x,y)= 4 x y . Thus A(S) = D 2 3 0 2 2 2 2 2 2 2 { 2 2 3 } and [( x)(4 x y ) r 2 2 2 2 1/2 2 ] +[( y)(4 x y ) 2 3 0 2 2 1/2 2 ] +1 dA = 0 2 +1 r dr d = 0 2 2r 4 r 2 dr d 4 r 2(4 r ) = 0 2 2 1/2 r= 3 r=0 d = ( 2+4)d = 2 0 2 0 =4 11. z= a x y , z = x(a x y ) x 2 2 2 2 2 1/2 , z = y(a x y ) y 2 2 2 1/2 , A(S) = D /2 acos x +y 2 2 2 2 2 +1 dA 2 2 a x y = /2 0 /2 acos r 2 +1 r dr d a r ar a r a r 2 2 2 2 = /2 /2 0 dr d r=acos r=0 = /2 a d /2 = /2 a ( a a cos 2 2 2 a d =2a ) 2 /2 0 (1 1 cos 2 )d 3 Stewart Calculus ET 5e 0534393217;15. Multiple Integrals; 15.6 Surface Area =2a 2 /2 d 0 2a 2 /2 sin 0 2 d =a 2 2a 2 /2 0 sin d =a ( 2 2) 12. To find the region D : z=x +y implies z+z =4z or z 3z=0 . Thus z=0 or z=3 are the planes where the surfaces intersect. But x +y +z =4z implies x +y +(z 2) =4 , so z=3 intersects the upper hemisphere. Thus (z 2) =4 x y or z=2+ 4 x y . Therefore D is the region inside the circle x +y +(3 2) =4 , that is, D= (x,y)| x +y A(S) = D 2 3 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 { 2 2 3 } . 2 1/2 2 1+[( x)(4 x y ) r 2 2 2 2 1/2 2 ] +[( y)(4 x y ) 2 3 0 2 ] dA 2 2 1/2 r= 3 r=0 = 0 2 0 1+ r dr d = 0 2 0 2r dr 4 r 2 d = 0 2(4 r ) d 4 r = ( 2+4)d = 2 0 =4 x y 2 2 13. z= f (x,y)=e A(S)= x +y 2 2 x y 2 2 , f = 2xe x x y 2 2 2 , f = 2ye y x y 2 2 2 x y 2 2 . Then 4(x +y )e 2 2 2(x +y ) 2 2 ( 2xe 4 ) +( 2ye ) +1 dA= x +y 2 2 +1 dA . 4 Converting to polar coordinates we have 2 2 A(S) = 0 0 2 4r e 2 2 2r 2 2 2 +1 r dr d = 0 2 d 0 r 4r e 2 2r 2 +1 dr =2 0 r 4r e 2r +1 dr 13.9783 using a calculator. 14. z= f (x,y)=cos (x +y ) , f = 2xsin (x +y ) , f = 2ysin (x +y ) . x y 2 2 2 2 2 2 A(S) = = 4x sin (x +y )+4y sin (x +y )+1 dA 2 2 2 2 2 2 2 2 2 2 x +y 1 4(x +y )sin (x +y )+1 dA 2 2 2 2 2 2 2 x +y 1 4 Stewart Calculus ET 5e 0534393217;15. Multiple Integrals; 15.6 Surface Area Converting polar to coordinates gives 2 1 A(S) = 0 0 1 4r sin (r )+1 r dr d = 0 2 2 2 2 2 2 2 1 d 0 r 4r sin (r )+1 dr 2 2 2 =2 0 r 4r sin (r )+1 dr 4.1073 using a calculator. 15. (a) The midpoints of the four squares are Here f (x,y)=x +y , so the Midpoint Rule gives A(S) = D 2 2 1 1 , 4 4 2 , 1 3 , 4 4 2 , 3 1 , 4 4 , and 3 3 , 4 4 . [ f (x,y)] +[ f (x,y)] +1 dA= x y D 2 2 2 (2x) +(2y) +1 dA 2 1 4 + = 1 4 2 2 3 +2 2 1 4 3 4 2 + 2 + 2 7 + 2 11 2 1 4 1 4 2 +1 + +1 + 1.8279 2 2 1 4 3 4 2 2 + 2 + 2 3 4 3 4 2 2 +1 +1 (b) A CAS estimates the integral to be A(S)= D 1+(2x) +(2y) dA= 0 0 2 2 1 1 1+4x +4y dydx 1.8616 . 2 2 This agrees with the Midpoint estimate only in the first decimal place. 16. (a) With m=n=2 we have four squares with midpoints 3 3 , 2 2 A(S) = D 1 1 , 2 2 , 1 3 , 2 2 , 3 1 , 2 2 , and . Since z=xy+x +y , the Midpoint Rule gives [ f (x,y)] +[ f (x,y)] +1 dA= x y D 2 2 2 2 (y+2x) +(x+2y) +1 dA 5 2 2 2 2 1 = 3 2 2 + 3 2 2 +1 + + 7 2 2 +1 + 7 2 2 + 5 2 2 +1 + 9 2 2 + 9 2 22 78 78 166 + + + 2 2 2 2 17.619 5 Stewart Calculus ET 5e 0534393217;15. Multiple Integrals; 15.6 Surface Area (b) Using a CAS, we have A(S)= D (y+2x) +(x+2y) +1 dA= 00 2 2 22 1+(y+2x) +(x+2y) dydx 17.7165 . This is within about 0.1 2 2 of the Midpoint Rule estimate. 17. z=1+2x+3y+4y , so A(S) = D 41 2 1+ z x 2 + 2 z y 2 41 dA= 1 0 1+4+(3+8y) dydx 2 = 1 0 14+48y+64y dydx . Using a CAS, we have 41 1 0 14+48y+64y dydx= or 45 8 14 + 2 45 8 14 + 15 15 ln ( 11 5+3 14 5 ) ln ( 3 5+ 14 5 ) 16 16 11 5+3 70 15 ln . 16 3 5+ 70 2 18. f ( x,y ) =1+x+y+x 1 1 f =1+2x , f =1 . We use a CAS to calculate the integral x y 1 1 2 1 A(S)= 2 1 f + f +1 dydx= x y 1 2 2 (1+2x) +2 dydx=2 2 2 1 4x +4x+3 dx and find that 2 A(S)=3 11 +2sinh 3 2 2 or A ( S ) =3 11 +ln ( 10+3 11 ) . 19. f (x,y)=1+x y 1 1 x 2 2 2 f =2xy , f =2x y . We use a CAS (with precision reduced to five significant x y 1 1 1 x 2 2 2 digits, to speed up the calculation) to estimate the integral A(S)= 1 1 x 2 f + f +1 dydx= x y 1 x 2 2 2 4x y +4x y +1 dydx , and find that A(S) 3.3213 . 2 4 4 2 6 Stewart Calculus ET 5e 0534393217;15. Multiple Integrals; 15.6 Surface Area 20. Let f (x,y)= 1+x 2 1+y 1 1 |x| 2 . Then f = x 2 x 2 y 2x 1+y 2 , f = 1+x y ( 2 ) 2y ( 1+y ) 2 2 = 2y 1+x ( 2 ) ( 1+y ) 2 2 . We use a CAS to estimate 1 ( 1 |x| ) f + f +1 dydx 2.6959 . In order to graph only the part of the surface above y 1 x as the y range in our plot command. the square, we use ( 1 x ) 21. Here z= f (x,y)=ax+by+c , f (x,y)=a , f (x,y)=b , so x y A(S)= D a +b +1 dA= a +b +1 D 2 2 2 2 dA= a +b +1 A(D) . 2 2 22. Let S be the upper hemisphere. Then z= f (x,y)= a x y , so A(S) = D 2 2 2 [ x(a x y ) x +y D 2 2 2 2 2 2 2 2 1/2 2 ] +[ y(a x y ) 2 t 2 2 2 1/2 2 ] +1 dA = 2 t +1 dA= 0 0 r 2 2 2 +1 r dr d t 0 a x y ar a r 2 a r a =lim t a 0 0 dr d =2 lim 2 2 t a a r 2 2 =2 lim a t a a t 2 2 a =2 ( a)( a)=2 a . Thus the surface area of the entire sphere is 4 a . 23. If we project the surface onto the xz plane, then the surface lies ``above'' the disk x +z the xz plane. We have y= f (x,z)=x +z and, adapting Formula 2, the area of the surface is A(S)= x +z 2 2 2 2 2 25 in 2 2 [ f (x,z)] +[ f (x,z)] +1 dA= x z 25 x +z 2 2 2 2 4x +4z +1 dA 25 7 2 2 Stewart Calculus ET 5e 0534393217;15. Multiple Integrals; 15.6 Surface Area Converting to polar coordinates x=rcos 2 5 , z=rsin 2 1/2 we have 2 0 A(S) = 0 0 4r +1 r dr d = 0 2 2 5 d 0 r(4r +1) dr= 1 2 3/2 (4r +1) 12 5 0 = 6 ( 101 101 1 ) 24. First we find the area of the face of the surface that intersects the positive y axis. As in Exercise 23 , we can project the face onto the xz plane, so the surface lies ``above'' the disk x +z z= f (x,z)= 1 z and the area is A(S) = [ f (x,z)] +[ f (x,z)] +1 dA= 2 2 2 2 1 . Then 2 2 2 x z 0+ 2 2 z 1 z 2 2 +1 dA x +z 1 2 2 1 1 z 2 x +z 1 = x +z 1 2 2 z 1 1 z 0 2 +1 dA= 1 1 z 2 1 1 z 2 dxdz 1 z 1 1 z =4 0 dxdz [by the symmetry of the surface] 2 This integral is improper (when z=1 ), so t 1 z 0 2 A ( S ) =lim 4 t 1 0 1 2 t dxdz=lim 4 0 1 z 2 2 t dz=lim 4 dz=lim 4t=4 . t 1 t 1 0 t 1 1 z 1 z Since the complete surface consists of four congruent faces, the total surface area is 4(4)=16 . 8
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TN Tech - MATH - Cal I- Cal
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Stewart Calculus ET 5e 0534393217;15. Multiple Integrals; 15.3 Double Integrals over General Regions1.1x21 0 1 0 3(x+2y)dydx =0 0xy+y2 y=x21 0y=0dx=x(x )+(x ) 0 0 dx1 0222= (x +x )dx=41 4 1 5 x+ x 4 5=9 202.22
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TN Tech - MATH - Cal I- Cal
TN Tech - MATH - Cal I- Cal
TN Tech - MATH - Cal I- Cal
TN Tech - MATH - Cal I- Cal
TN Tech - MATH - Cal I- Cal
TN Tech - MATH - Cal I- Cal
TN Tech - MATH - Cal I- Cal
TN Tech - MATH - Cal I- Cal
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Classics 2123: The Roman Way Notes to Virgil's Aeneid, Books IX-XIISpring 2008Book IX. War finally breaks out, the full-scale battles spoken of in Book VII. The book divides into three sections: (1) Turnus and the Rutulians attack the Trojan ship
FSU - CLA - 2123
Classics 2123: The Roman Way Lecture 5. Roman Imperialism and Expansion Readings: BHR 44-67; Shelton 291-293 I. Roman Imperialism - definition of `imperialism' - older notion of `defensive imperialism': how realistic? - was Rome more warlike/aggressi
FSU - CLA - 2123
Classics 2123: The Roman Way Roman Names A Roman had three names: praenomen (first name) nomen (name of the gens or clan) cognomen (family branch) Thus for: Publius praenomen Cornelius nomen Scipio cognomenSpring 2008his given name was "Publius,"
Stevens - PEP - 111
AC CIRCUITS35.1. Model: A phasor is a vector that rotates counterclockwise around the origin at angular frequency w. Solve: (a) Refemng to the phasor in Figure Ex35.1, the phase angle isU? = 180'n rad - 30" = 150 x -= 2.618 rad180"w=2*618ra
Stevens - PEP - 111
15.1. Solve: The density of the liquid is=m 0.120 kg 0.120 kg = = = 1200 kg m 3 V 100 mL 100 10 -3 10 -3 m 3Assess: The liquid's density is more than that of water (1000 kg/m3) and is a reasonable number.15.2. Solve: The volume of the helium
Stevens - PEP - 111
16.1. Solve: The mass of lead mPb = Pb VPb = (11,300 kg m 3 )(2.0 m 3 ) = 22,600 kg . For water to have thesame mass its volume must beVwater =mwater 22,600 kg = = 22.6 m 3 water 1000 kg m 316.2. Solve: The volume of the uranium nucleus isV
Stevens - PEP - 111
17.1. Model: For a gas, the thermal energy is the total kinetic energy of the moving molecules. That is, Eth =Kmicro. Solve: The number of atoms isN=M 0.0020 kg = = 3.01 10 23 m 6.64 10 -27 kgBecause helium atoms have an atomic mass number A
Stevens - PEP - 111
18.1. Solve: We can use the ideal-gas law in the form pV = NkBT to determine the Loschmidt number (N/V):1.013 10 5 Pa N p = 2.69 10 25 m -3 = = V kB T (1.38 10 -23 J K )(273 K )()18.2. Solve: Nitrogen is a diatomic molecule, so r 1.0 10-1
Stevens - PEP - 111
19.1. Model: The heat engine follows a closed cycle, starting and ending in the original state. The cycleconsists of three individual processes. Visualize: Please refer to Figure Ex19.1. Solve: (a) The work done by the heat engine per cycle is the a
Stevens - PEP - 111
20.1. Model: This is a wave traveling at constant speed. The pulse moves 1 m to the right every second.Visualize: Please refer to Figure Ex20.1. The snapshot graph shows the wave at all points on the x-axis at t = 0 s. You can see that nothing is h