Foundations to FrontierPart VI: Calculus IIIBezhig

Module 43: Conservative fields and Green’s theorem

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

On this page
  1. A. Prerequisites and observable goals
  2. B. The central idea: some line integrals depend only on endpoints
  3. C. Potential, domain, and boundary theorems
  4. D. Why local contributions cancel inside a region
  5. E. Choose between a potential and a region integral
  6. F. Worked examples
  7. Computing bridge: Potential energy and the domain of the model
  8. G. Independent practice
  9. H. Complete solutions: Module 43
  10. I. Retention and readiness

A. Prerequisites and observable goals#

Before

Line integrals, gradients, mixed partials, and double integrals.

After

Find a potential when it exists, use endpoint evaluation for conservative work, and apply Green’s circulation or flux form with domain and orientation conditions.

B. The central idea: some line integrals depend only on endpoints#

A conservative vector field is a gradient, F=∇ϕ\vv F=\grad\phi, for a scalar potential ϕ\phi on its domain. Along a path, the chain rule makes F⋅r′\vv F\cdot\vv r' a derivative of ϕ(r(t))\phi(\vv r(t)), so the work becomes a difference of potential values. Other fields retain path information; Green’s theorem can turn a closed planar path integral into an area integral describing interior rotation or outflow.

C. Potential, domain, and boundary theorems#

For a differentiable potential and a piecewise smooth path from AA to BB,

∫C∇ϕ⋅ dr=ϕ(B)−ϕ(A).\int_C\grad\phi\cdot\dd\vv r=\phi(B)-\phi(A).

On an open connected domain with sufficient smoothness, being conservative is equivalent to path independence and to zero integral around every closed path. For a C1C^1 planar field F=(P,Q)\vv F=(P,Q), a necessary condition is Py=QxP_y=Q_x. On a simply connected open domain it is also sufficient. A domain with a hole requires additional care: equality of cross partials alone is not enough. [O3Conservative]

For a positively oriented (counterclockwise) piecewise smooth simple closed boundary CC enclosing a suitable planar region DD, and P,Q∈C1P,Q\in C^1 on an open neighborhood of DD, Green’s theorem states

∮CP dx+Q dy=∬D(Qx−Py) dA.\oint_C P\dd x+Q\dd y=\iint_D(Q_x-P_y)\dd A.

Its outward flux form is

∮CP dy−Q dx=∬D(Px+Qy) dA.\oint_C P\dd y-Q\dd x=\iint_D(P_x+Q_y)\dd A.

For a region with holes, orient the outer boundary counterclockwise and each inner boundary clockwise, keeping the region on the left as you traverse. The theorem applies when the field is smooth on the region and a neighborhood, not necessarily inside excluded holes. [O3Green]

D. Why local contributions cancel inside a region#

Partition a region into small cells. Circulation around adjacent cells cancels on shared edges because those edges are traversed in opposite directions. Only the outer boundary remains. The small-cell circulation per area approaches Qx−PyQ_x-P_y. In flux form, outward flow across one cell’s shared side is inward flow to its neighbor; again the internal contributions cancel. This cancellation explains the orientation convention and foreshadows the three-dimensional boundary theorems.

For a potential, the ordinary chain rule gives  dϕ(r(t))/ dt=∇ϕ⋅r′\dd\phi(\vv r(t))/\dd t=\grad\phi\cdot\vv r'. Integrating proves the endpoint theorem directly. A zero derivative test on a punctured domain cannot create a single-valued potential if a closed loop has nonzero work around the hole.

Why the inside cancels. Split a region into small cells and walk around each one counterclockwise. Every shared edge is walked twice, in opposite directions, so those contributions cancel, and what remains is one counterclockwise trip around the outer boundary. Green’s theorem is this bookkeeping in the limit of small cells.

E. Choose between a potential and a region integral#

For any path, first check whether finding a potential is easy. Integrate one component and include an unknown function of the other coordinates, then differentiate to match the remaining components. For a closed planar path, consider Green when the enclosed region is simpler than the boundary parameterization. Verify the field has no singularities on the required region. For holes, include every boundary component with its correct direction rather than filling a forbidden hole silently.

F. Worked examples#

Building a potential. For F=(2xy,x2+2y)\vv F=(2xy,x^2+2y), integrate ϕx=2xy\phi_x=2xy in xx to get ϕ=x2y+g(y)\phi=x^2y+g(y). Matching ϕy=x2+g′(y)=x2+2y\phi_y=x^2+g'(y)=x^2+2y gives g=y2+Cg=y^2+C. Thus work from (0,0)(0,0) to (1,2)(1,2) is (12⋅2+4)−0=6(1^2\cdot2+4)-0=6, independent of path within R2\R^2.

A hole counterexample. On R2∖{0}\R^2\setminus\{0\}, the field F=(−y/(x2+y2),x/(x2+y2))\vv F=(-y/(x^2+y^2),x/(x^2+y^2)) satisfies Py=QxP_y=Q_x but has circulation 2π2\pi around the counterclockwise unit circle. It is not globally conservative there. Green cannot be applied to the full enclosed disk because the field is undefined at its center.

Area from a boundary. Choosing P=0,Q=xP=0,Q=x makes Qx−Py=1Q_x-P_y=1, so for positive orientation, A(D)=∮Cx dyA(D)=\oint_C x\dd y. The symmetric form is A=12∮C(x dy−y dx)A=\tfrac12\oint_C(x\dd y-y\dd x). Reversing orientation changes the signed result, not the geometric area.

Computing bridge: Potential energy and the domain of the model#

A force derived from a potential can give path-independent work on the stated domain. In T05, the central force excludes the origin, and the simulation must reject a singular state rather than divide by zero. Checking a derivative identity at ordinary points does not remove a hole in a field’s domain. The practical connection is to record model restrictions alongside invariants such as energy, and not use a conservation argument where its assumptions fail.

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.

M43.01FSolution

Find a potential for F=(2xy,x2+3y2)\vv F=(2xy,x^2+3y^2) on R2\R^2.

M43.02CSolution

Use a potential to compute the work of the field in M43.01 from (1,0)(1,0) to (2,1)(2,1) along any piecewise smooth path.

M43.03CSolution

Determine whether F=(y,x+y)\vv F=(y,x+y) is conservative on R2\R^2 and find a potential if so.

M43.04TSolution

Determine whether F=(xy,x2)\vv F=(xy,x^2) is conservative on R2\R^2. Explain why equality at some individual points is insufficient.

M43.05CSolution

Use Green’s theorem to find circulation of F=(−y,x)\vv F=(-y,x) counterclockwise around x2/4+y2/9=1x^2/4+y^2/9=1.

M43.06TSolution

Find the outward flux of F=(x,y)\vv F=(x,y) across the boundary of [0,2]×[0,3][0,2]\times[0,3] using Green’s flux form.

M43.07TSolution

For the punctured-plane field in the worked example, find circulation on the positively oriented boundary of the annulus 1≤x2+y2≤41\le x^2+y^2\le4. Explain why Green applies to the annulus but not its filled-in outer disk.

M43.08SSolution

Find ∮Cy2 dx+x2 dy\oint_C y^2\dd x+x^2\dd y around the counterclockwise triangle with vertices (0,0),(2,0),(0,1)(0,0),(2,0),(0,1). Check the result by direct integration on its edges.

Optional small hints

For M43.01, the arbitrary term after integrating in xx is a function of yy. For M43.07, the inner circle is clockwise. For M43.08, Green’s integrand is 2x−2y2x-2y.

H. Complete solutions: Module 43#

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

M43.01Show solution

Match the component not used in the first integration

Integrating ϕx=2xy\phi_x=2xy gives ϕ=x2y+g(y)\phi=x^2y+g(y). Then ϕy=x2+g′(y)\phi_y=x^2+g'(y) must equal x2+3y2x^2+3y^2, so g′=3y2g'=3y^2 and g=y3+Cg=y^3+C. A potential is ϕ=x2y+y3\boxed{\phi=x^2y+y^3}, verified by taking its gradient.

Back to M43.01
M43.02Show solution

Endpoint evaluation replaces the entire path calculation

The potential from M43.01 has ϕ(2,1)=4+1=5\phi(2,1)=4+1=5 and ϕ(1,0)=0\phi(1,0)=0. Therefore work is 5\boxed5. The field is a smooth gradient on all of R2\R^2, so the endpoint theorem applies to any of the stated paths, not only a straight line.

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M43.03Show solution

Check a sufficient condition and construct the potential

Here Py=1P_y=1 and Qx=1Q_x=1 throughout the simply connected domain R2\R^2, suggesting a conservative field. Integrate ϕx=y\phi_x=y to get ϕ=xy+g(y)\phi=xy+g(y). Matching ϕy=x+g′=x+y\phi_y=x+g'=x+y gives g=y2/2g=y^2/2. Thus ϕ=xy+y2/2\boxed{\phi=xy+y^2/2} directly establishes conservativeness.

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M43.04Show solution

A local mismatch rules out a global gradient

The cross partials are Py=xP_y=x and Qx=2xQ_x=2x, unequal wherever x≠0x\ne0. Hence the smooth field cannot be conservative on R2\R^2. Equality along the line x=0x=0 does not establish the needed identity on an open domain. A potential would have matching mixed partials throughout its smooth domain.

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M43.05Show solution

Constant planar curl reduces the calculation to area

The field is smooth everywhere and the ellipse has counterclockwise orientation. Its Green integrand is Qx−Py=1−(−1)=2Q_x-P_y=1-(-1)=2. The ellipse area is π(2)(3)=6π\pi(2)(3)=6\pi, so circulation is 12π\boxed{12\pi}. Orientation reversal would negate this result.

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M43.06Show solution

Outward flux is an area integral of planar divergence

Here Px+Qy=1+1=2P_x+Q_y=1+1=2. The rectangle area is 66, so outward flux is 12\boxed{12}. The boundary is taken counterclockwise when using P dy−Q dxP\dd y-Q\dd x; this convention makes the associated normal outward.

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M43.07Show solution

The inner boundary cancels the circulation around the hole

On a radius-RR circle traversed counterclockwise, substitution gives work 2π2\pi, independent of RR. The annulus’s outer circle therefore contributes 2π2\pi and its clockwise inner circle contributes −2π-2\pi, for total 0\boxed0. The cross-partial difference is zero throughout a neighborhood of the closed annulus, so Green applies and agrees. Filling the hole would include the singular origin, violating the theorem’s smoothness condition.

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M43.08Show solution

An area calculation checked by the boundary itself

Green gives

I=∫02∫01−x/2(2x−2y) dy dx=∫02(3x−1−5x2/4) dx=2/3.I=\int_0^2\int_0^{1-x/2}(2x-2y)\dd y\dd x =\int_0^2(3x-1-5x^2/4)\dd x=\boxed{2/3}.

For a direct check, the bottom edge has y=0, dy=0y=0,\dd y=0 and contributes zero. The sloping edge from (2,0)(2,0) to (0,1)(0,1) is x=2−2t,y=tx=2-2t,y=t, 0≤t≤10\le t\le1, so its contribution is ∫01[−2t2+(2−2t)2] dt=∫01(4−8t+2t2) dt=2/3\int_0^1[-2t^2+(2-2t)^2]\dd t=\int_0^1(4-8t+2t^2)\dd t=2/3. The vertical return edge has x=0, dx=0x=0,\dd x=0 and contributes zero. Both methods agree with the specified orientation.

Back to M43.08

I. Retention and readiness#

Retrieve M36.02 and M42.05. Explain why curl-free behavior on a domain with a hole is not by itself a global potential. Advance when you can choose between potential evaluation, direct parameterization, and Green, while stating which region must be free of singularities.