Selecting Methods & Approaches - Calculus 3

  1. When evaluating ∫CF⃗⋅dr⃗\int_C \vec{F} \cdot d\vec{r} where F⃗=⟨−y/(x2+y2),x/(x2+y2)⟩\vec{F} = \langle -y/(x^2+y^2), x/(x^2+y^2) \rangle and CC is any simple closed curve in the plane not containing the origin, which theorem provides the most direct approach?
    Answer: Green's Theorem directly, since ∂Q∂x−∂P∂y=0\frac{\partial Q}{\partial x} - \frac{\partial P}{\partial y} = 0 everywhere the field is defined Computing the partial derivatives: P=−y/(x2+y2)P = -y/(x^2+y^2) gives ∂P∂y=−(x2+y2−y(2y))/(x2+y2)2=−(x2−y2)/(x2+y2)2\frac{\partial P}{\partial y} = -(x^2+y^2-y(2y))/(x^2+y^2)^2 = -(x^2-y^2)/(x^2+y^2)^2. And Q=x/(x2+y2)Q = x/(x^2+y^2) gives ∂Q∂x=(x2+y2−x(2x))/(x2+y2)2=(y2−x2)/(x2+y2)2\frac{\partial Q}{\partial x} = (x^2+y^2-x(2x))/(x^2+y^2)^2 = (y^2-x^2)/(x^2+y^2)^2. Therefore ∂Q∂x−∂P∂y=(y2−x2)/(x2+y2)2−(−(x2−y2)/(x2+y2)2)=0\frac{\partial Q}{\partial x} - \frac{\partial P}{\partial y} = (y^2-x^2)/(x^2+y^2)^2 - (-(x^2-y^2)/(x^2+y^2)^2) = 0. Since the curve doesn't contain the origin, Green's Theorem applies and gives the integral equals zero. Choice B is incorrect because the domain is not simply connected (origin is removed). Choice C incorrectly describes the potential function. Choice D unnecessarily avoids Green's Theorem when it can be applied.
  2. To find the center of mass of a solid hemisphere of radius aa with density ρ(x,y,z)=z\rho(x,y,z) = z, which combination of coordinate system and symmetry arguments would minimize computational effort?
    Answer: Use spherical coordinates and recognize that xˉ=yˉ=0\bar{x} = \bar{y} = 0 by symmetry, then compute only zˉ\bar{z} The hemisphere has symmetry about the z-axis, and the density function ρ(x,y,z)=z\rho(x,y,z) = z preserves this symmetry (it depends only on the z-coordinate, not on x or y). Therefore, xˉ=yˉ=0\bar{x} = \bar{y} = 0 by symmetry arguments. Only zˉ\bar{z} needs to be computed. Spherical coordinates are ideal because the hemisphere boundary is ρ=a\rho = a, 0≤ϕ≤π/20 \leq \phi \leq \pi/2, and the density becomes ρcos⁡ϕ\rho\cos\phi which integrates nicely. Choice B incorrectly claims density breaks symmetry. Choice C incorrectly suggests the center of mass is at the geometric center (it's not, due to the variable density). Choice D incorrectly claims all coordinates must be computed despite the clear symmetry.
  3. When computing the circulation ∮CF⃗⋅dr⃗\oint_C \vec{F} \cdot d\vec{r} where F⃗=⟨yexy,xexy+cos⁡y⟩\vec{F} = \langle ye^{xy}, xe^{xy} + \cos y \rangle and CC is the boundary of the square [0,π]×[0,π][0,\pi] \times [0,\pi] oriented counterclockwise, which method would minimize the computational work?
    Answer: Green's Theorem, since ∂Q∂x−∂P∂y=exy(1+xy)−exy(1+xy)=0\frac{\partial Q}{\partial x} - \frac{\partial P}{\partial y} = e^{xy}(1 + xy) - e^{xy}(1 + xy) = 0 Let's compute the partial derivatives for Green's Theorem. We have P=yexyP = ye^{xy} and Q=xexy+cos⁡yQ = xe^{xy} + \cos y. Then ∂P∂y=exy+y⋅xexy=exy(1+xy)\frac{\partial P}{\partial y} = e^{xy} + y \cdot xe^{xy} = e^{xy}(1 + xy) and ∂Q∂x=exy+x⋅yexy=exy(1+xy)\frac{\partial Q}{\partial x} = e^{xy} + x \cdot ye^{xy} = e^{xy}(1 + xy). Therefore ∂Q∂x−∂P∂y=exy(1+xy)−exy(1+xy)=0\frac{\partial Q}{\partial x} - \frac{\partial P}{\partial y} = e^{xy}(1 + xy) - e^{xy}(1 + xy) = 0. By Green's Theorem, the circulation is zero. This is much easier than parameterizing four separate line segments. Choice A would require substantial computation. Choice B has the correct conclusion but shows incorrect intermediate steps. Choice D would also work (the field is indeed conservative) but finding the potential function explicitly would take longer than applying Green's Theorem.
  4. Consider the line integral ∫C(x2y dx+xy2 dy)\int_C (x^2y \, dx + xy^2 \, dy) where CC is the boundary of the region R={(x,y):0≤x≤1,x2≤y≤x}R = \{(x,y): 0 \leq x \leq 1, x^2 \leq y \leq \sqrt{x}\}, traversed counterclockwise. Which approach would be most computationally efficient?
    Answer: Apply Green's Theorem: ∬R(∂(xy2)∂x−∂(x2y)∂y)dA=∬R(y2−x2) dA\iint_R \left(\frac{\partial(xy^2)}{\partial x} - \frac{\partial(x^2y)}{\partial y}\right) dA = \iint_R (y^2 - x^2) \, dA When you encounter a line integral around a closed curve, you have three main tools: direct parameterization, checking for conservativeness, or applying Green's Theorem. The key is choosing the most efficient approach based on the vector field's properties. For F⃗=⟨x2y,xy2⟩\vec{F} = \langle x^2y, xy^2 \rangle, let's first check if it's conservative by testing if ∂P∂y=∂Q∂x\frac{\partial P}{\partial y} = \frac{\partial Q}{\partial x}. We have ∂(x2y)∂y=x2\frac{\partial(x^2y)}{\partial y} = x^2 and ∂(xy2)∂x=y2\frac{\partial(xy^2)}{\partial x} = y^2. Since x2≠y2x^2 \neq y^2 in general, the field is not conservative, eliminating option A. Green's Theorem converts the line integral to ∬R(∂Q∂x−∂P∂y)dA\iint_R \left(\frac{\partial Q}{\partial x} - \frac{\partial P}{\partial y}\right) dA. Computing the partial derivatives: ∂(xy2)∂x=y2\frac{\partial(xy^2)}{\partial x} = y^2 and ∂(x2y)∂y=x2\frac{\partial(x^2y)}{\partial y} = x^2. Therefore, the integrand is y2−x2y^2 - x^2, making option C correct. Option B would require parameterizing four separate curves (the boundary has segments along y=x2y = x^2, y=xy = \sqrt{x}, and vertical segments), which is computationally intensive. Option D makes an algebraic error, incorrectly computing the partial derivatives as 2xy2xy each, likely confusing mixed partials or chain rule applications. Study tip: Always check if a vector field is conservative first (quickest when it works), but when it's not conservative and you have a nice region, Green's Theorem typically beats direct parameterization. Double-check your partial derivative calculations—they're the most common source of errors.
  5. To evaluate the triple integral ∭E(x2+y2+z2) dV\iiint_E (x^2 + y^2 + z^2) \, dV where EE is the region bounded by x2+y2+z2≤4x^2 + y^2 + z^2 \leq 4, z≥0z \geq 0, and x2+y2≤z2x^2 + y^2 \leq z^2, which coordinate system and approach would be most efficient?
    Answer: Spherical coordinates with bounds 0≤ρ≤20 \leq \rho \leq 2, 0≤θ≤2π0 \leq \theta \leq 2\pi, 0≤ϕ≤π/40 \leq \phi \leq \pi/4 The region E is the intersection of a hemisphere (upper half of sphere radius 2) with the interior of a circular cone (x2+y2≤z2x^2 + y^2 \leq z^2 with z≥0z \geq 0). In spherical coordinates, the cone x2+y2=z2x^2 + y^2 = z^2 becomes ρ2sin⁡2ϕ=ρ2cos⁡2ϕ\rho^2\sin^2\phi = \rho^2\cos^2\phi, which simplifies to tan⁡ϕ=1\tan\phi = 1 or ϕ=π/4\phi = \pi/4. Since we want x2+y2≤z2x^2 + y^2 \leq z^2 (inside the cone), we need 0≤ϕ≤π/40 \leq \phi \leq \pi/4. The integrand x2+y2+z2=ρ2x^2 + y^2 + z^2 = \rho^2 is also simple in spherical coordinates. Choice A has incorrect bounds for a cone in cylindrical coordinates. Choice C uses Cartesian coordinates which would be computationally intensive. Choice D has the wrong range for ϕ\phi (outside the cone rather than inside).
  6. To compute ∭Ezx2+y2 dV\iiint_E z \sqrt{x^2 + y^2} \, dV where EE is the region inside the cone z2=x2+y2z^2 = x^2 + y^2 and below the plane z=4z = 4, which coordinate transformation would be optimal?
    Answer: Cylindrical coordinates with bounds 0≤r≤40 \leq r \leq 4, 0≤θ≤2π0 \leq \theta \leq 2\pi, r≤z≤4r \leq z \leq 4 The cone z2=x2+y2z^2 = x^2 + y^2 with z≥0z \geq 0 (since we're below the plane z=4z = 4) becomes z=x2+y2=rz = \sqrt{x^2 + y^2} = r in cylindrical coordinates. The region EE is inside this cone and below z=4z = 4, so for each fixed rr and θ\theta, zz ranges from the cone surface z=rz = r up to z=4z = 4. At z=4z = 4, the cone has radius r=4r = 4, so rr ranges from 00 to 44. The integrand becomes zx2+y2=zrz \sqrt{x^2 + y^2} = zr with volume element r dr dθ dzr \, dr \, d\theta \, dz. Choice A has wrong zz bounds (doesn't account for cone constraint). Choice B has rr and zz bounds reversed. Choice C uses spherical coordinates unnecessarily and with incorrect bounds.
  7. To find the volume of the region bounded by z=x2+y2z = x^2 + y^2 and z=2−x2−y2z = 2 - x^2 - y^2, which method and coordinate system combination would be most efficient?
    Answer: Cartesian coordinates with double integration: V=∬R[(2−x2−y2)−(x2+y2)] dAV = \iint_R [(2-x^2-y^2) - (x^2+y^2)] \, dA where RR is x2+y2≤1x^2+y^2 \leq 1 The surfaces intersect where x2+y2=2−x2−y2x^2 + y^2 = 2 - x^2 - y^2, giving 2(x2+y2)=22(x^2 + y^2) = 2, so x2+y2=1x^2 + y^2 = 1. The paraboloid z=x2+y2z = x^2 + y^2 opens upward, and z=2−x2−y2z = 2 - x^2 - y^2 opens downward. For x2+y2<1x^2 + y^2 < 1, we have x2+y2<2−x2−y2x^2 + y^2 < 2 - x^2 - y^2, so the downward paraboloid is above the upward one. The volume is V=∬R[(2−x2−y2)−(x2+y2)] dA=∬R(2−2x2−2y2) dAV = \iint_R [(2-x^2-y^2) - (x^2+y^2)] \, dA = \iint_R (2-2x^2-2y^2) \, dA where R:x2+y2≤1R: x^2+y^2 \leq 1. Converting to polar: V=∫02π∫01(2−2r2)r dr dθ=2π∫01(2r−2r3) dr=2π[r2−r4/2]01=2π(1−1/2)=πV = \int_0^{2\pi} \int_0^1 (2-2r^2) r \, dr \, d\theta = 2\pi \int_0^1 (2r-2r^3) \, dr = 2\pi[r^2-r^4/2]_0^1 = 2\pi(1-1/2) = \pi. Choice A uses triple integration unnecessarily. Choice C uses wrong coordinate system and bounds. Choice D has incorrect intersection radius.
  8. For the surface integral ∬SF⃗⋅dS⃗\iint_S \vec{F} \cdot d\vec{S} where F⃗=⟨x3,y3,z3⟩\vec{F} = \langle x^3, y^3, z^3 \rangle and SS is the sphere x2+y2+z2=a2x^2 + y^2 + z^2 = a^2, which approach most effectively exploits the symmetry of the problem?
    Answer: Use the Divergence Theorem with ∇⋅F⃗=3(x2+y2+z2)\nabla \cdot \vec{F} = 3(x^2 + y^2 + z^2) to get ∭V3(x2+y2+z2) dV\iiint_V 3(x^2 + y^2 + z^2) \, dV When evaluating flux integrals through closed surfaces, the Divergence Theorem is often your most powerful tool, especially when the surface has high symmetry like a sphere. The theorem converts the surface integral ∬SF⃗⋅dS⃗\iint_S \vec{F} \cdot d\vec{S} into the volume integral ∭V(∇⋅F⃗) dV\iiint_V (\nabla \cdot \vec{F}) \, dV, which can dramatically simplify calculations. For F⃗=⟨x3,y3,z3⟩\vec{F} = \langle x^3, y^3, z^3 \rangle, the divergence is ∇⋅F⃗=3x2+3y2+3z2=3(x2+y2+z2)\nabla \cdot \vec{F} = 3x^2 + 3y^2 + 3z^2 = 3(x^2 + y^2 + z^2). Using the Divergence Theorem transforms your problem into ∭V3(x2+y2+z2) dV\iiint_V 3(x^2 + y^2 + z^2) \, dV, which is perfect for spherical coordinates where x2+y2+z2=ρ2x^2 + y^2 + z^2 = \rho^2. Option A incorrectly assumes ∇⋅F⃗=3a2\nabla \cdot \vec{F} = 3a^2 everywhere on the surface, but the divergence varies with position—it only equals 3a23a^2 specifically on the sphere surface, not throughout the volume. Option B misapplies symmetry arguments; while the components have certain symmetries, this vector field doesn't have the antisymmetric properties needed to make the integral zero. Option C gives the correct normal component formula but suggests direct parameterization, which leads to a much more complex calculation involving x4+y4+z4x^4 + y^4 + z^4 that doesn't simplify easily. The key insight: when you see a flux integral through a closed surface, always check if the Divergence Theorem simplifies your work. Spherical symmetry combined with the Divergence Theorem often transforms difficult surface integrals into manageable volume integrals.

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