Chapter O

Exercises O.1

  1. 1.

    When C is a curve in the plane and f is a surface defined over C, then ∫Cf⁢(s)⁢d⁡s describes the area under the spatial curve that lies on f, over C.

  2. 2.

    The evaluation is the same. The ∮ notation signifies that the curve C is a closed curve, though the evaluation is the same.

  3. 3.

    The variable s denotes the arc-length parameter, which is generally difficult to use. The Key Idea allows one to parameterize a curve using another, ideally easier-to-use, parameter.

  4. 4.

    Answers will vary.

  5. 5.

    12⁢2

  6. 6.

    41⁢10/2

  7. 7.

    40⁢π

  8. 8.

    10⁢π2

  9. 9.

    Over the first subcurve of C, the line integral has a value of 3/2; over the second subcurve, the line integral has a value of 4/3. The total value of the line integral is thus 17/6.

  10. 10.

    Over the first subcurve of C, the line integral has a value of 2⁢2/3; over the second subcurve, the line integral has a value of π−2. The total value of the line integral is thus π+2⁢2/3−2.

  11. 11.

    1/2

  12. 12.

    (ln⁡2)/2

  13. 13.

    23

  14. 14.

    4⁢π

  15. 15.

    14/5

  16. 16.

    2⁢2⁢π2

  17. 17.

    (17⁢17−5⁢5)/3

  18. 18.

    2/5

  19. 19.

    ∫01(5⁢t2+2t+2)⁢(4⁢t+1)2+1⁢d⁡t≈17.071

  20. 20.

    ∫0πt⁢1+cos2⁡t⁢d⁡t≈6.001

  21. 21.

    ∮02⁢π(10−4⁢cos2⁡t−sin2⁡t)⁢cos2⁡t+4⁢sin2⁡t⁢d⁡t≈74.986

  22. 22.

    ∫−11(3⁢t3+2⁢t+5)⁢9⁢t4+1⁢d⁡t≈15.479

  23. 23.

    7⁢26/3

  24. 24.

    2⁢π

  25. 25.

    8⁢π3

  26. 26.

    5/2

  27. 27.

    M=8⁢2⁢π2 g; center of mass is (0,−1/(2⁢π),8⁢π/3).

  28. 28.

    M≈0.237 g; center of mass is approximately (0.173,0.099,0.065).

  29. 29.

    24⁢π

  30. 30.
  31. 31.

Exercises O.2

  1. 1.

    Answers will vary. Appropriate answers include velocities of moving particles (air, water, etc.); gravitational or electromagnetic forces.

  2. 2.

    Specific answers will vary, though should relate to the idea that “more of the vector field is moving into that point than out of that point.”

  3. 3.

    Specific answers will vary, though should relate to the idea that the vector field is spinning clockwise at that point.

  4. 4.

    No; to be incompressible, the divergence needs to be 0 everywhere, not just at one point.

  5. 5.

    Correct answers should look similar to

    −22−22xy
  6. 6.

    Correct answers should look similar to

    −22−22xy
  7. 7.

    Correct answers should look similar to

    −22−22xy
  8. 8.

    Correct answers should look similar to

    −22−22xy
  9. 9.

    div⁡F→=1+2⁢y; curl⁡F→=0

  10. 10.

    div⁡F→=0; curl⁡F→=1+2⁢y

  11. 11.

    div⁡F→=x⁢cos⁡(x⁢y)−y⁢sin⁡(x⁢y); curl⁡F→=y⁢cos⁡(x⁢y)+x⁢sin⁡(x⁢y)

  12. 12.

    div⁡F→=4(x2+y2)2; curl⁡F→=0

  13. 13.

    div⁡F→=3; curl⁡F→=⟨−1,−1,−1⟩

  14. 14.

    div⁡F→=2⁢x+2⁢y+2⁢z; curl⁡F→=⟨2⁢y,2⁢z,2⁢x⟩

  15. 15.

    div⁡F→=1+2⁢y; curl⁡F→=0

  16. 16.

    div⁡F→=2⁢y; curl⁡F→=0

  17. 17.

    div⁡F→=2⁢y−sin⁡z; curl⁡F→=0→

  18. 18.

    div⁡F→=2(x2+y2+z2)2; curl⁡F→=0→

  19. 19.
  20. 20.
  21. 21.
  22. 22.
  23. 23.
  24. 24.
  25. 25.
  26. 26.

Exercises O.3

  1. 1.

    False. It is true for line integrals over scalar fields, though.

  2. 2.

    The input of F→ should be a point in the plane, not a two dimensional vector.

  3. 3.

    True.

  4. 4.

    False.

  5. 5.

    We can conclude that F→ is conservative.

  6. 6.

    By the Fundamental Theorem of Line Integrals, since F→ is conservative, ∮CF→⋅d⁡r→=f⁢(B)−f⁢(A), where f is a potential function for F→ and A and B are the initial and terminal points of C, respectively. Since C is a closed curve, A=B, and hence f⁢(B)−f⁢(A)=0.

  7. 7.

    11/6. (One parameterization for C is r→⁢(t)=⟨3⁢t,t⟩ on 0≤t≤1.)

  8. 8.

    5/3. (One parameterization for C is r→⁢(t)=⟨t,t2⟩ on 0≤t≤1.)

  9. 9.

    0. (One parameterization for C is r→⁢(t)=⟨cos⁡t,sin⁡t⟩ on 0≤t≤π.)

  10. 10.

    2/5. (One parameterization for C is r→⁢(t)=⟨t,t3⟩ on −1≤t≤1.)

  11. 11.

    12. (One parameterization for C is r→⁢(t)=⟨1,2,3⟩+t⁢⟨3,1,−1⟩ on 0≤t≤1.)

  12. 12.

    1.

  13. 13.

    1

  14. 14.

    −2⁢π

  15. 15.

    0

  16. 16.

    2⁢π

  17. 17.

    −1/30

  18. 18.

    0

  19. 19.

    1/3

  20. 20.

    −1/2; 1/2

  21. 21.

    2

  22. 22.

    2⁢π⁢(π−1)

  23. 23.

    0

  24. 24.

    67/15

  25. 25.

    0

  26. 26.

    6

  27. 27.

    5/6 joules. (One parameterization for C is r→⁢(t)=⟨t,t⟩ on 0≤t≤1.)

  28. 28.

    13/15 joules. (One parameterization for C is r→⁢(t)=⟨t,t⟩ on 0≤t≤1.)

  29. 29.

    24 ft-lbs.

  30. 30.

    24 ft-lbs.

  31. 31.

    2/3 joules

  32. 32.

    8/15 joules

  33. 33.

    No.

  34. 34.

    Yes. f⁢(x,y)=x2/2−y2/2.

  35. 35.

    No.

  36. 36.

    Yes. f⁢(x,y)=x⁢y2+x3

  37. 37.

    No.

  38. 38.

    Yes. f⁢(x,y)=4⁢x2⁢y+2⁢y2+3⁢x

  39. 39.

    No.

  40. 40.

    Yes. f⁢(x,y,z)=a⁢x+b⁢y+c⁢z.

  41. 41.

    Yes. f⁢(x,y,z)=x2/x+x⁢y+z3/3.

  42. 42.

    No

  43. 43.

    • f⁢(x,y)=x⁢y+x

      curl⁡F→=0.

      1. (One parameterization for C is r→⁢(t)=⟨t,t−1⟩ on 0≤t≤1.)

      1 (f⁢(0,1)=0 and f⁢(1,0)=1)

  44. 44.

    • f⁢(x,y)=x2+x⁢y+y2

      curl⁡F→=0.

      0.

      0 (f⁢(0,0)=0)

  45. 45.

    • f⁢(x,y)=x2⁢y⁢z

      curl⁡F→=0→.

      250.

      250 (f⁢(1,−1,0)=0 f⁢(5,5,2)=250)

  46. 46.

    • f⁢(x,y)=x2+y2+z2

      curl⁡F→=0→.

      0.

      0 (f⁢(1,0,0)=1)

  47. 47.

    • f⁢(x,y)=x⁢y2+x3/3

      curl⁡F→=0→

      0.

      0 (f⁢(1,0)=1/3)

  48. 48.

    • f⁢(x,y)=x⁢y2+x3/3

      curl⁡F→=0→

      2/3.

      2/3 (f⁢(1,0)=1/3, f⁢(−1,0)=−1/3)

  49. 49.

    • f⁢(x,y)=x2⁢y2/2

      curl⁡F→=0→

      625⁢π4/2048

      625⁢π4/2048 (f⁢(0,0)=0,
      f⁢(−5⁢π/4⁢2,−5⁢π/4⁢2)=625⁢π4/2048

  50. 50.

    • f⁢(x,y)=y2+x2⁢ey

      curl⁡F→=0→

      −1

      −1 (f⁢(1,0)=1, f⁢(0,0)=0)

  51. 51.

    Since F→ is conservative, it is the gradient of some potential function. That is, ∇f=⟨fx,fy,fz⟩=F→=⟨M,N,P⟩. In particular, M=fx, N=fy and P=fz.

    Note that curl⁡F→=⟨Py−Nz,Mz−Px,Nx−My⟩=⟨fz⁢y−fy⁢z,fx⁢z−fz⁢x,fy⁢x−fx⁢y⟩, which, by Theorem 13.3.1, is ⟨0,0,0⟩.

  52. 52.
  53. 53.
  54. 54.
  55. 55.
  56. 56.
  57. 57.

    (b) No. Hint: Think of how f is defined.

  58. 58.

    Yes. f⁢(x,y)=a⁢x⁢y+b⁢x+c⁢y+d.

  59. 59.

    0; no

  60. 60.

    7/10; 7/10; no

Exercises O.4

  1. 1.

    along, across

  2. 2.

    It is the measure of flow around the entirety of a closed curve C.

  3. 3.

    the curl of F→, or curl⁡F→

  4. 4.

    the divergence of F→, or div⁡F→

  5. 5.

    curl⁡F→

  6. 6.

    div⁡F→

  7. 7.

    12

  8. 8.

    12

  9. 9.

    −2/3

  10. 10.

    10/3

  11. 11.

    1/2

  12. 12.

    1/2

  13. 13.

    The line integral ∮CF→⋅d⁡r→, over the parabola, is 38/3; over the line, it is −10. The total line integral is thus 38/3−10=8/3. The double integral of curl⁡F→=2 over R also has value 8/3.

  14. 14.

    Both the line integral and double integral have value of 2⁢π.

  15. 15.

    Three line integrals need to be computed to compute ∮CF→⋅d⁡r→. It does not matter which corner one starts from first, but be sure to proceed around the triangle in a counterclockwise fashion.

    From (0,0) to (2,0), the line integral has a value of 0. From (2,0) to (1,1) the integral has a value of 7/3. From (1,1) to (0,0) the line integral has a value of −1/3. Total value is 2.

    The double integral of curl⁡F→ over R also has value 2.

  16. 16.

    Two line integrals need to be computed to compute ∮CF→⋅d⁡r→. Along the parabola, the line integral has value 25.5. Along the line, the line integral has value −21. Together, the total value is 4.5

    The double integral of curl⁡F→ over R also has value 4.5.

  17. 17.

    16/15

  18. 18.
  19. 19.

    −5⁢π

  20. 20.
  21. 21.

    −1/2

  22. 22.

    1/3

  23. 23.

    −π/2

  24. 24.

    −45⁢π/32

  25. 25.

    0

  26. 26.

    0

  27. 27.

    4/3

  28. 28.

    −4/3

  29. 29.

    Any choice of F→ is appropriate as long as curl⁡F→=1. When F→=⟨−y/2,x/2⟩, the integrand of the line integral is simply 6. The area of R is 12⁢π.

  30. 30.

    Any choice of F→ is appropriate as long as curl⁡F→=1. The choices of F→=⟨−y,0⟩ and ⟨0,x⟩ each lead to reasonable integrands. The area of R is 4/3.

  31. 31.

    Any choice of F→ is appropriate as long as curl⁡F→=1. The choices of F→=⟨−y,0⟩, ⟨0,x⟩ and ⟨−y/2,x/2⟩ each lead to reasonable integrands. The area of R is 16/15.

  32. 32.

    Any choice of F→ is appropriate as long as curl⁡F→=1. The choice of F→=⟨−y/2,x/2⟩ leads to a reasonable integrand after simplification. The area of R is 41⁢π/10.

  33. 33.

    The line integral ∮CF→⋅n→⁢d⁡s, over the parabola, is −22/3; over the line, it is 10. The total line integral is thus −22/3+10=8/3. The double integral of div⁡F→=2 over R also has value 8/3.

  34. 34.

    Both the line integral and double integral have value of 0.

  35. 35.

    Three line integrals need to be computed to compute ∮CF→⋅n→⁢d⁡s. It does not matter which corner one starts from first, but be sure to proceed around the triangle in a counterclockwise fashion.

    From (0,0) to (2,0), the line integral has a value of 0. From (2,0) to (1,1) the integral has a value of 1/3. From (1,1) to (0,0) the line integral has a value of 1/3. Total value is 2/3.

    The double integral of div⁡F→ over R also has value 2/3.

  36. 36.

    Two line integrals need to be computed to compute ∮CF→⋅n→⁢d⁡s. Along the parabola, the line integral has value 159/20. Along the line, the line integral has value 6. Together, the total value is 279/20.

    The double integral of div⁡F→ over R also has value 279/20.

  37. 37.

Exercises O.5

  1. 1.

    Answers will vary, though generally should meaningfully include terms like “two sided”.

  2. 2.

    Many possible answers exist; the one given by the book is the Möbius band.

  3. 3.

    • r→⁢(u,v)=⟨u,v,3⁢u2⁢v⟩ on −1≤u≤1, 0≤v≤2.

      r→(u,v)=⟨3vcosu+1,3vsinu+2,
      3(3vcosu+1)2(3vsinu+2)⟩, on 0≤u≤2⁢π, 0≤v≤1.

      r→⁢(u,v)=⟨u,v⁢(2−2⁢u),3⁢u2⁢v⁢(2−2⁢u)⟩ on 0≤u,v≤1.

      r→⁢(u,v)=⟨u,v⁢(1−u2),3⁢u2⁢v⁢(1−u2)⟩ on −1≤u≤1, 0≤v≤1.

  4. 4.

    • r→⁢(u,v)=⟨u,v,4⁢u+2⁢u2⟩ on 1≤u≤4, 5≤v≤7.

      r→⁢(u,v)=⟨4⁢v⁢cos⁡u,3⁢v⁢sin⁡u,16⁢v⁢cos⁡u+2⁢(3⁢v⁢sin⁡u)2⟩, on 0≤u≤2⁢π, 0≤v≤1.

      r→⁢(u,v)=⟨u,u+v⁢(4−2⁢u),4⁢u+2⁢(u+v⁢(4−2⁢u))2⟩ on
      0≤u≤2, 0≤v≤1.

      r→⁢(u,v)=⟨v⁢cos⁡u,v⁢sin⁡u,4⁢v⁢cos⁡u+2⁢(v⁢sin⁡u)2⟩ on 0≤u≤2⁢π, 2≤v≤5.

  5. 5.

    r→⁢(u,v)=⟨0,u,v⟩ with 0≤u≤2, 0≤v≤1.

  6. 6.

    r→⁢(u,v)=⟨u,0,1−u+v⁢u⟩ with 0≤u≤1, 0≤v≤1.

  7. 7.

    r→⁢(u,v)=⟨3⁢sin⁡u⁢cos⁡v,2⁢sin⁡u⁢sin⁡v,4⁢cos⁡u⟩ with 0≤u≤π, 0≤v≤2⁢π.

  8. 8.

    Answers may vary; one solution is

    r→⁢(u,v)=⟨v⁢cos⁡u,v,4⁢v⁢sin⁡u⟩ with 0≤u≤2⁢π, −1≤v≤5.

  9. 9.

    Answers may vary.

    For z=12⁢(3−x): r→⁢(u,v)=⟨u,v,12⁢(3−u)⟩, with 1≤u≤3 and 0≤v≤2.

    For x=1: r→⁢(u,v)=⟨1,u,v⟩, with 0≤u≤2, 0≤v≤1

    For y=0: r→⁢(u,v)=⟨u,0,v/2⁢(3−u)⟩, with 1≤u≤3, 0≤v≤1

    For y=2: r→⁢(u,v)=⟨u,2,v/2⁢(3−u)⟩, with 1≤u≤3, 0≤v≤1

    For z=0: r→⁢(u,v)=⟨u,v,0⟩, with 1≤u≤3, 0≤v≤2

  10. 10.

    Answers may vary.

    For z=2⁢x+4⁢y−4: r→⁢(u,v)=⟨u,1−u/2+u⁢v/2,2⁢u+4⁢(1−u/2+u⁢v/2)−4⟩, with 0≤u≤2, 0≤v≤1.

    For x=2: r→⁢(u,v)=⟨2,u,4⁢u⁢v⟩, with 0≤u≤1, 0≤v≤1

    For y=1: r→⁢(u,v)=⟨u,1,2⁢u⁢v⟩, with 0≤u≤2, 0≤v≤1

    For z=0: r→⁢(u,v)=⟨u,1−u/2+u⁢v/2,0⟩, with 0≤u≤2, 0≤v≤1

  11. 11.

    Answers may vary.

    For z=2⁢y:r→⁢(u,v)=⟨u,v⁢(4−u2),2⁢v⁢(4−u2)⟩ with −2≤u≤2 and 0≤v≤1.

    For y=4−x2:r→⁢(u,v)=⟨u,4−u2,2⁢v⁢(4−u2)⟩ with −2≤u≤2 and 0≤v≤1.

    For z=0: r→⁢(u,v)=⟨u,v⁢(4−u2),0⟩ with −2≤u≤2 and 0≤v≤1.

  12. 12.

    Answers may vary.

    For y=1−z2: r→⁢(u,v)=⟨u,v⁢(1−u2),1−v⁢(1−u2)⟩ with 0≤u≤1 and 0≤v≤1.

    For y=1−x2: r→⁢(u,v)=⟨u,1−u2,u⁢v⟩ with 0≤u≤1 and 0≤v≤1.

    For x=0: r→⁢(u,v)=⟨0,v⁢(1−u2),u⟩ with 0≤u≤1 and 0≤v≤1.

    For y=0: r→⁢(u,v)=⟨u,0,v⟩ with 0≤u≤1 and 0≤v≤1.

    For z=0: r→⁢(u,v)=⟨u,v⁢(1−u2),0⟩ with 0≤u≤1 and 0≤v≤1.

  13. 13.

    Answers may vary.

    For x2+y2/9=1: r→⁢(u,v)=⟨cos⁡u,3⁢sin⁡u,v⟩ with 0≤u≤2⁢π and 1≤v≤3.

    For z=1: r→⁢(u,v)=⟨v⁢cos⁡u,3⁢v⁢sin⁡u,1⟩ with 0≤u≤2⁢π and 0≤v≤1.

    For z=3: r→⁢(u,v)=⟨v⁢cos⁡u,3⁢v⁢sin⁡u,3⟩ with 0≤u≤2⁢π and 0≤v≤1.

  14. 14.

    Answers may vary.

    For x2+y2=(z−1)2: r→⁢(u,v)=⟨v⁢cos⁡u,v⁢sin⁡u,1−v⟩ with 0≤u≤2⁢π and 0≤v≤1.

    For z=0: r→⁢(u,v)=⟨v⁢cos⁡u,v⁢sin⁡u,0⟩ with 0≤u≤2⁢π and 0≤v≤1.

  15. 15.

    Answers may vary.

    For z=1−x2: r→⁢(u,v)=⟨u,v,1−u2⟩ with −1≤u≤1 and −1≤v≤2.

    For y=−1: r→⁢(u,v)=⟨u,−1,v⁢(1−u2)⟩ with −1≤u≤1 and 0≤v≤1.

    For y=2: r→⁢(u,v)=⟨u,2,v⁢(1−u2)⟩ with −1≤u≤1 and 0≤v≤1.

    For z=0: r→⁢(u,v)=⟨u,v,0⟩ with −1≤u≤1 and −1≤v≤2.

  16. 16.

    Answers may vary.

    For z=4−x2−4⁢y2: r→⁢(u,v)=⟨2⁢v⁢cos⁡u,v⁢sin⁡u,4−(2⁢v⁢cos⁡u)2−4⁢(v⁢sin⁡u)2⟩ with 0≤u≤2⁢π and 0≤v≤1.

    For z=0: r→⁢(u,v)=⟨2⁢v⁢cos⁡u,v⁢sin⁡u,0⟩ with 0≤u≤2⁢π and 0≤v≤1.

  17. 17.

    S=2⁢14.

  18. 18.

    S=6/2.

  19. 19.

    S=4⁢3⁢π.

  20. 20.

    S=3⁢3⁢π.

  21. 21.

    4⁢π⁢r2

  22. 22.

    π⁢R⁢h2+R2

  23. 23.
  24. 24.
  25. 25.

    S=∫03∫02⁢πv2+4⁢v4⁢d⁡u⁢d⁡v=(37⁢37−1)⁢π/6≈117.319.

  26. 26.

    S=∫01∫01v2+4⁢u2⁢v2+4⁢v4⁢d⁡u⁢d⁡v≈0.931.

  27. 27.

    S=∫−11∫01−v227⁢d⁡u⁢d⁡v=4⁢3≈6.928.

  28. 28.

    S=∫01∫02⁢πv2+4⁢v4⁢d⁡u⁢d⁡v=(5⁢5−1)⁢π/6≈5.330.

Exercises O.6

  1. 1.

    curve; surface

  2. 2.

    Answers will vary; in general, it means that more of the vector field passes through the surface opposite the direction of the normal vector than in the same direction of the normal vector.

  3. 3.

    outside

  4. 4.

    0

  5. 5.

    240⁢3

  6. 6.

    40⁢π

  7. 7.

    24

  8. 8.

    15

  9. 9.

    0

  10. 10.

    0

  11. 11.

    −1/2

  12. 12.

    π

  13. 13.

    0; the flux over 𝒮1 is −45⁢π and the flux over 𝒮2 is 45⁢π.

  14. 14.

    9⁢π/8; the flux over 𝒮1 is 3⁢π/4 (use r→⁢(u,v)=⟨sin⁡u⁢cos⁡v,sin⁡u⁢sin⁡v,cos⁡u⟩ on π/3≤u≤π, 0≤v≤2⁢π) and the flux over 𝒮2 is 3⁢π/8 (use r→⁢(u,v)=⟨v⁢3⁢cos⁡(u)/2,v⁢3⁢sin⁡(u)/2,1/2⟩ for 0≤u≤2⁢π, 0≤v≤1.

  15. 15.

    3

  16. 16.

    7/4

Exercises O.7

  1. 1.

    Answers will vary; in Section 15.4, the Divergence Theorem connects outward flux over a closed curve in the plane to the divergence of the vector field, whereas in this section the Divergence Theorem connects outward flux over a closed surface in space to the divergence of the vector field.

  2. 2.

    Divergence.

  3. 3.

    Curl.

  4. 4.

    Green’s Theorem.

  5. 5.

    Outward flux across the plane z=2−x/2−2⁢y/3 is 22; across the plane z=0 the outward flux is −8; across the planes x=0 and y=0 the outward flux is 0.

    Total outward flux: 14.

    ∬Ddiv⁡F→⁢d⁡V=∫04∫03−3⁢x/4∫02−x/2−2⁢y/3(2⁢x+2⁢y)⁢d⁡z⁢d⁡y⁢d⁡x=14.

  6. 6.

    Outward flux across the cylinder x2+y2=1 is 0; across the plane z=3 the outward flux is 3⁢π; across the plane z=−3 the outward flux is 3⁢π.

    Total outward flux: 6⁢π.

    ∬Ddiv⁡F→⁢d⁡V=∫02⁢π∫01∫−33r⁢d⁡z⁢d⁡r⁢d⁡θ=6⁢π.

  7. 7.

    Outward flux across the surface z=x⁢y⁢(3−x)⁢(3−y) is 252; across the plane z=0 the outward flux is −9.

    Total outward flux: 243.

    ∬Ddiv⁡F→⁢d⁡V=∫03∫03∫0x⁢y⁢(3−x)⁢(3−y)12⁢d⁡z⁢d⁡y⁢d⁡x=243.

  8. 8.

    Outward flux across the paraboloid is 112⁢π/3; across the disk the outward flux is 0.

    Total outward flux: 112⁢π/3.

    ∬Ddiv⁡F→⁢d⁡V=∫02⁢π∫02∫04−r2(2⁢z+2)⁢r⁢d⁡z⁢d⁡r⁢d⁡θ=112⁢π/3.

  9. 9.

    With an upward normal, both integrals are −3⁢π.

  10. 10.
  11. 11.

    Circulation on C: ∮CF→⋅d⁡r→=π

    ∬𝒮(curl⁡F→)⋅n→⁢d⁡S=π.

  12. 12.

    Circulation on C: ∮CF→⋅d⁡r→=π

    ∬𝒮(curl⁡F→)⋅n→⁢d⁡S=π.

  13. 13.

    Circulation on C: The flow along the line from (0,0,2) to (4,0,0) is 0; from (4,0,0) to (0,3,0) it is −6, and from (0,3,0) to (0,0,2) it is 6. The total circulation is 0+(−6)+6=0.

    ∬𝒮(curl⁡F→)⋅n→⁢d⁡S=∬𝒮0⁢d⁡S=0.

  14. 14.

    Circulation on C: The flow along the parabola is −32/15; the flow along the line is 4/3. The total circulation is 4/3−32/15=−4/5.

    ∬𝒮(curl⁡F→)⋅n→⁢d⁡S=−4/5.

  15. 15.

    216⁢π

  16. 16.

    3

  17. 17.

    12⁢π/5

  18. 18.

    0

  19. 19.

    128/225

  20. 20.

    8

  21. 21.

    8192/105≈78.019

  22. 22.

    64/3

  23. 23.

    5/3

  24. 24.

    8⁢π

  25. 25.

    23⁢π

  26. 26.

    0

  27. 27.

    Each field has a divergence of 1; by the Divergence Theorem, the total outward flux across 𝒮 is ∬D1⁢d⁡S for each field.

  28. 28.

    • curl⁡F→=1.

      curl⁡F→⋅n→=1, where n→ is a unit vector normal to 𝒮.

  29. 29.

    Answers will vary. Often the closed surface 𝒮 is composed of several smooth surfaces. To measure total outward flux, this may require evaluating multiple double integrals. Each double integral requires the parameterization of a surface and the computation of the cross product of partial derivatives. One triple integral may require less work, especially as the divergence of a vector field is generally easy to compute.

  30. 30.

    Answers will vary. Often the closed curve C is composed of several smooth curves. To measure the total circulation, one may have to evaluate line integrals along each curve. Each line integral requires the parameterization of its curve. It may be less work to evaluate one single double (i.e., surface) integral.

  31. 31.
  32. 32.
  33. 33.
  34. 34.
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