Foundations to FrontierPart VI: Calculus IIIBezhig

Module 44: Surface area, scalar surface integrals, and flux

8 exercises, each with a complete solution. 1 figure.

On this page
  1. A. Prerequisites and observable goals
  2. B. The central idea: a surface needs two parameters and a normal
  3. C. Area elements and orientation
  4. D. Why cross products appear again
  5. E. A safe surface-integral workflow
  6. F. Worked examples
  7. G. Independent practice
  8. H. Complete solutions: Module 44
  9. I. Retention and readiness

A. Prerequisites and observable goals#

Before

Cross products, double integrals, parameterized curves, and field interpretation.

After

Parameterize a surface patch, compute its area element, choose an oriented vector area element, and distinguish an open surface from a closed boundary.

B. The central idea: a surface needs two parameters and a normal#

A curve uses one parameter; a surface patch uses two: r(u,v)\vv r(u,v). The two derivative vectors describe tangent directions. Their cross product gives a normal and an area scale. A scalar surface integral weights actual curved area. Flux additionally selects the component of a vector field passing through the oriented surface. Choosing an orientation is part of the problem, not an optional sign adjustment afterward.

C. Area elements and orientation#

For a smooth regular patch with ru×rv≠0\vv r_u\times\vv r_v\ne\vv0 and a parameter region that covers the surface once except permissible boundary seams,

 dS=∥ru×rv∥ du dv,∬Sf dS=∬Df(r(u,v))∥ru×rv∥ du dv.\dd S=\|\vv r_u\times\vv r_v\|\dd u\dd v, \qquad \iint_S f\dd S=\iint_D f(\vv r(u,v))\|\vv r_u\times\vv r_v\|\dd u\dd v.

For the orientation of ru×rv\vv r_u\times\vv r_v,

∬SF⋅n dS=∬DF(r(u,v))⋅(ru×rv) du dv.\iint_S\vv F\cdot\vv n\dd S =\iint_D\vv F(\vv r(u,v))\cdot(\vv r_u\times\vv r_v)\dd u\dd v.

The cross product already contains the area scale. Do not multiply its dot product by its norm again. Reversing orientation negates flux but does not change scalar surface area. [O3Surface]

For a graph z=g(x,y)z=g(x,y), upward vector area is ⟨−gx,−gy,1⟩ dx dy\langle-g_x,-g_y,1\rangle\dd x\dd y, and scalar area is 1+gx2+gy2 dx dy\sqrt{1+g_x^2+g_y^2}\dd x\dd y. Downward orientation reverses the vector. A closed surface encloses a solid and has a conventional outward orientation; an open patch has a boundary and must be assigned one of its normal choices explicitly.

D. Why cross products appear again#

A small parameter rectangle has tangent side vectors approximately ruΔu\vv r_u\Delta u and rvΔv\vv r_v\Delta v. Its mapped parallelogram has area ∥ru×rv∥ΔuΔv\|\vv r_u\times\vv r_v\|\Delta u\Delta v. Dividing the cross product by its length yields a unit normal, so multiplying F⋅n\vv F\cdot\vv n by scalar area cancels the normalization denominator and gives the vector-area formula.

The same geometric distinction appeared in line integrals: density times length used a norm, while work along a direction used a dot product. Here density times area uses a cross-product norm, and flow through an orientation uses a dot product with the cross product.

E. A safe surface-integral workflow#

Identify the surface equation, its boundary, and orientation. Choose a graph or a two-parameter description with a simple parameter domain. Differentiate both parameter directions, compute their cross product, and test its direction at an easy point. Reverse it if necessary. Substitute the field and integrate with either the norm or the oriented vector, depending on the requested quantity. For a closed surface made of several patches, account for every patch with outward normals; a missing disk can change flux even when it looks visually small.

F. Worked examples#

A cylinder’s side. The radius-aa cylinder is r(θ,z)=⟨acos⁡θ,asin⁡θ,z⟩\vv r(\theta,z)=\langle a\cos\theta,a\sin\theta,z\rangle. The cross product rθ×rz=⟨acos⁡θ,asin⁡θ,0⟩\vv r_\theta\times\vv r_z=\langle a\cos\theta,a\sin\theta,0\rangle points outward and has norm aa. Therefore lateral area over height HH is ∫0H∫02πa dθ dz=2πaH\int_0^H\int_0^{2\pi}a\dd\theta\dd z=2\pi aH. The top and bottom disks are not included.

A sphere’s orientation. With fixed radius RR, use r(ϕ,θ)=R⟨sin⁡ϕcos⁡θ,sin⁡ϕsin⁡θ,cos⁡ϕ⟩\vv r(\phi,\theta)=R\langle\sin\phi\cos\theta,\sin\phi\sin\theta,\cos\phi\rangle. The order rϕ×rθ\vv r_\phi\times\vv r_\theta points outward and has magnitude R2sin⁡ϕR^2\sin\phi. Swapping parameter derivative order makes the normal inward. The pole singularities are coordinate degeneracies handled by patching or limits, not geometric tears in the sphere.

Three-dimensional projection of the graph patch z=x+yz=x+y with an upward normal proportional to (−1,−1,1)(-1,-1,1). The normal is perpendicular to both coordinate tangent directions. This geometric area differs from the patch’s projection onto the xyxy-plane.

G. Independent practice#

F foundation C standard course work T transfer S optional stretch L runnable lab or project. Attempt the complete set before opening its solutions.

M44.01FSolution

Find the area of r(u,v)=⟨u,v,2u−v⟩\vv r(u,v)=\langle u,v,2u-v\rangle, 0≤u,v≤10\le u,v\le1.

M44.02CSolution

Evaluate ∬Sz dS\iint_S z\dd S on the graph z=x+yz=x+y over 0≤x≤10\le x\le1, 0≤y≤20\le y\le2.

M44.03TSolution

Find upward flux of F=(0,0,z)\vv F=(0,0,z) through z=3−x−yz=3-x-y above the triangle x,y≥0x,y\ge0, x+y≤3x+y\le3.

M44.04CSolution

Compute outward flux of F=(x,y,z)\vv F=(x,y,z) through the radius-two sphere directly as a surface integral.

M44.05TSolution

Compute outward flux of F=(x,y,0)\vv F=(x,y,0) through the lateral cylinder x2+y2=1x^2+y^2=1, 0≤z≤20\le z\le2. What do its end disks contribute if included?

M44.06TSolution

Find downward flux of F=(x,y,2)\vv F=(x,y,2) through z=x2+y2z=x^2+y^2 over the unit disk.

M44.07CSolution

Evaluate ∬Sz dS\iint_S z\dd S over the upper hemisphere of the unit sphere.

M44.08SSolution

For the constant field F=(0,0,1)\vv F=(0,0,1), compute upward/outward flux through the upper unit hemisphere and downward flux through its base disk. Explain the difference between the open and closed surface totals.

Optional small hints

For M44.03, use the upward vector area (1,1,1) dA(1,1,1)\dd A. For M44.06, downward vector area is (2x,2y,−1) dA(2x,2y,-1)\dd A. For M44.08, close the hemisphere only after including the disk with the correct outward direction for the half-ball.

H. Complete solutions: Module 44#

Compare the first step where your work differs. A corrected answer is not yet an independent success.

M44.01Show solution

The cross-product norm is constant over this planar patch

The tangent vectors are ru=(1,0,2)\vv r_u=(1,0,2) and rv=(0,1,−1)\vv r_v=(0,1,-1). Their cross product is (−2,1,1)(-2,1,1), with norm 6\sqrt6. The parameter square has area one, so surface area is 6\boxed{\sqrt6}. This also equals the parallelogram area spanned by the two edge vectors.

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M44.02Show solution

A scalar surface integral weights slanted area

For the graph, gx=gy=1g_x=g_y=1, so  dS=3 dx dy\dd S=\sqrt3\dd x\dd y. Substitute z=x+yz=x+y: ∬Sz dS=3∫01∫02(x+y) dy dx=3∫01(2x+2) dx=33\iint_Sz\dd S=\sqrt3\int_0^1\int_0^2(x+y)\dd y\dd x =\sqrt3\int_0^1(2x+2)\dd x=\boxed{3\sqrt3}. No orientation sign is involved in this scalar integral.

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M44.03Show solution

The field’s vertical component dots with vector area

The upward vector area is (1,1,1) dA(1,1,1)\dd A. After substituting z=3−x−yz=3-x-y, its dot product with (0,0,z)(0,0,z) is 3−x−y3-x-y. Thus

Φ=∫03∫03−x(3−x−y) dy dx=12∫03(3−x)2 dx=9/2.\Phi=\int_0^3\int_0^{3-x}(3-x-y)\dd y\dd x =\frac12\int_0^3(3-x)^2\dd x=\boxed{9/2}.

Multiplying by another 3\sqrt3 would wrongly add a second area scale.

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M44.04Show solution

A radial field has constant normal component on the sphere

On radius two, the outward unit normal is (x,y,z)/2(x,y,z)/2, so F⋅n=(x2+y2+z2)/2=2\vv F\cdot\vv n=(x^2+y^2+z^2)/2=2. The sphere area is 4π(2)2=16π4\pi(2)^2=16\pi, derived by integrating 4sin⁡ϕ4\sin\phi over its angular domain. Hence outward flux is 32π\boxed{32\pi}. This direct surface calculation will later provide a check on the Divergence theorem.

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M44.05Show solution

The side passes radial flow; the ends do not

Using (θ,z)(\theta,z), outward vector area is (cos⁡θ,sin⁡θ,0) dθ dz(\cos\theta,\sin\theta,0)\dd\theta\dd z. The substituted field is the same vector, so the dot product is one. Flux is ∫02∫02π1 dθ dz=4π\int_0^2\int_0^{2\pi}1\dd\theta\dd z=\boxed{4\pi}. On horizontal end disks, normals are vertical while the field has zero vertical component, so each disk contributes zero.

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M44.06Show solution

Choose downward before integrating

The graph’s downward vector area is (2x,2y,−1) dA(2x,2y,-1)\dd A. Its dot product with (x,y,2)(x,y,2) is 2x2+2y2−22x^2+2y^2-2. In polar coordinates,

Φ=∫02π∫01(2r2−2)r dr dθ=2π(1/2−1)=−π.\Phi=\int_0^{2\pi}\int_0^1(2r^2-2)r\dd r\dd\theta =2\pi(1/2-1)=\boxed{-\pi}.

The negative flux means the field has a net component opposite the chosen downward normal. Reversing to upward would give +π+\pi.

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M44.07Show solution

The hemisphere’s height and area factor are different functions

For the unit sphere, z=cos⁡ϕz=\cos\phi and  dS=sin⁡ϕ dϕ dθ\dd S=\sin\phi\dd\phi\dd\theta. The upper hemisphere uses 0≤ϕ≤π/20\le\phi\le\pi/2. Thus ∬Sz dS=∫02π∫0π/2cos⁡ϕsin⁡ϕ dϕ dθ=π\iint_Sz\dd S=\int_0^{2\pi}\int_0^{\pi/2}\cos\phi\sin\phi\dd\phi\dd\theta=\boxed\pi. This is a surface moment, not the volume moment π/4\pi/4 of the upper half-ball in Module 40.

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M44.08Show solution

Closing a surface adds a real flux contribution

On the upper unit hemisphere, the outward normal’s vertical component is cos⁡ϕ\cos\phi, so the flux is π\pi by the same angular integral as M44.07. The base disk’s outward normal for the half-ball is (0,0,−1)(0,0,-1), so its flux is −1-1 times disk area, −π-\pi. The open hemisphere flux is therefore π\boxed\pi, whereas the closed boundary total is 0\boxed0. A theorem for closed boundaries cannot be applied to the open hemisphere without accounting for its missing disk.

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I. Retention and readiness#

Retrieve M42.04 and M41.07. Explain when to use a cross-product norm and when to use its oriented vector directly. Advance when you can identify every patch of a closed surface and test each normal’s direction geometrically.