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17.4 Green's Theorem

Let \(\vec{F} = \langle f, g \rangle\)

The vector quantity \(\left( \frac{\partial g}{\partial x} - \frac{\partial f}{\partial y} \right) \vec{k} = \langle 0, 0, g_x - f_y \rangle\) is called the curl of \(\vec{F}\), written as \(\text{curl } \vec{F}\).

\(|\text{curl } \vec{F}| = |g_x - f_y|\) is a measure of rotation in \(\vec{F}\).

For example, \(\vec{F} = \langle x, y \rangle\)

Vector field plot of F = <x, y> showing arrows pointing radially outward from the origin with no rotation.
showing arrows pointing radially outward from the origin with no rotation." class="mx-auto">

\(\text{curl } \vec{F} = \langle 0, 0, 0 - 0 \rangle = \vec{0}\)

\(|\text{curl } \vec{F}| = 0\)

indicating no rotation
confirmed by visual inspection

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\(\vec{F} = \langle -y, x \rangle\)

Vector field plot of F = <-y, x> showing arrows circulating counter-clockwise around the origin.
showing arrows circulating counter-clockwise around the origin." class="mx-auto">

we see rotation

\(\text{curl } \vec{F} = \langle 0, 0, g_x - f_y \rangle = \langle 0, 0, 1 - (-1) \rangle = \langle 0, 0, 2 \rangle\)

\(|\text{curl } \vec{F}| = 2 \neq 0\), indicating a rotation

From last time,

if \(\vec{F} = \langle f, g \rangle\), then \(\vec{F}\) is conservative

if \(g_x = f_y \rightarrow g_x - f_y = 0\)

this means if \(\vec{F}\) is conservative, then \(|\text{curl } \vec{F}| = 0\)

or a conservative vector field is irrotational

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Green's Theorem

If \(\vec{F} = \langle f, g \rangle\) and \(C\) is a simple closed path traversed once in the counterclockwise direction, then

\[ \oint_C \vec{F} \cdot d\vec{r} = \oint_C f dx + g dy = \iint_R \left( \frac{\partial g}{\partial x} - \frac{\partial f}{\partial y} \right) dA \]
Circle means closed path
A region R in the xy-plane bounded by a closed curve C with counterclockwise orientation arrows.

Why is this true?

\(\oint_C \vec{F} \cdot d\vec{r}\) is a line integral accumulating \(\vec{F}\) along the path.

→ circulation on the boundary

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right side: \(\iint_R (g_x - f_y) dA\)

\(| \text{curl } \vec{F} |\)

So this is accumulating rotation on region \(R\).

inside each grid there is rotation

A region in the xy-plane divided into a grid, with small red circular arrows indicating rotation in each cell.

rotations cancel on boundary of two boxes

Diagram showing four adjacent square cells with internal rotations where internal boundary arrows cancel out.

after canceling inside, ends up like

A single square boundary with net counterclockwise flow after internal cancellations.
Final region in xy-plane showing only the boundary circulation remaining.

accumulates \(\vec{F}\) along boundary → left side of theorem

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Example: Line Integral and Green's Theorem

Given the vector field:

\[ \vec{F} = \langle y+2, x^2+1 \rangle \]

And the curve \( C \): from \( (-1, 1) \) to \( (1, 1) \) along \( y = x^2 \) then back to \( (-1, 1) \) along \( y = 2 - x^2 \).

Coordinate graph showing a closed region bounded by y=x^2 (C1) and y=2-x^2 (C2) from x=-1 to x=1.

Let's do this as a line integral, then try the Green's Theorem way.

Method 1: Line Integral

  • \( C_1: \vec{r}(t) = \langle t, t^2 \rangle \) for \( -1 \le t \le 1 \)
  • \( C_2: \vec{r}(t) = \langle -t, 2-t^2 \rangle \) for \( -1 \le t \le 1 \)
\[ \int_C \vec{F} \cdot \vec{r}' dt = \underbrace{\int_{-1}^{1} \langle t^2+2, t^2+1 \rangle \cdot \langle 1, 2t \rangle dt}_{C_1} + \underbrace{\int_{-1}^{1} \langle 4-t^2, t^2+1 \rangle \cdot \langle -1, -2t \rangle dt}_{C_2} \]
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\[ = \int_{-1}^{1} (2t^3 + t^2 + 2t + 2) dt + \int_{-1}^{1} (-2t^3 + t^2 - 2t - 4) dt = \dots = \frac{14}{3} - \frac{22}{3} = \boxed{-\frac{8}{3}} \]

Method 2: Green's Theorem

Green's Theorem says we can trade a line integral for a double integral over the region \( R \):

\[ \iint_R (g_x - f_y) dA \]

\( \vec{F} = \langle y+2, x^2+1 \rangle \)

\( g_x - f_y = 2x - 1 \)

Region \( R \):

  • \( -1 \le x \le 1 \)
  • \( x^2 \le y \le 2 - x^2 \)
Graph of the region R bounded by the parabolas y=x^2 and y=2-x^2 between x=-1 and x=1.
\[ \iint_R (g_x - f_y) dA = \int_{-1}^{1} \int_{x^2}^{2-x^2} (2x - 1) dy dx \]\[ = \int_{-1}^{1} (2x - 1)(2 - 2x^2) dx = \int_{-1}^{1} (-4x^3 + 2x^2 + 4x - 2) dx \]\[ = \dots = \boxed{-\frac{8}{3}} \]
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Green's Theorem for Area

Green's Theorem can also find area of \( R \) as a line integral:

\[ \oint f dx + g dy = \iint_R (g_x - f_y) dA \]

If \( g_x - f_y = 1 \), then the right side is \( \iint_R dA = \text{area of } R \).

Now come up with a vector field \( \vec{F} = \langle f, g \rangle \) such that \( g_x - f_y = 1 \).

One possibility: \( \vec{F} = \langle -\frac{1}{2}y, \frac{1}{2}x \rangle \)

Note: Here \( f = -\frac{1}{2}y \) and \( g = \frac{1}{2}x \).

Use these on the left side:

\[ \oint f dx + g dy = \oint -\frac{1}{2}y dx + \frac{1}{2}x dy \]
\[ = \frac{1}{2} \oint x dy - y dx \]

This gives area of \( R \)

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Green's Theorem: Alternative Form

Green's Theorem \( \oint f dx + g dy = \iint_R (g_x - f_y) dA \) is based on \( \int \vec{F} \cdot \vec{T} ds \) on the left side, where \( \vec{T} \) is the unit tangent.

If we use the unit normal \( \vec{N} \) instead of unit tangent \( \vec{T} \), we end up with:

\[ \oint f dy - g dx = \iint_R (f_x + g_y) dA \]

This is called the Divergence of \( \vec{F} = \text{div } \vec{F} \).

(In "standard" Green's Theorem, the right side is \( \text{curl } \vec{F} \)).

The divergence measures the change of a small volume as it travels in the vector field, and in this alternate Green's Theorem form we get the flux.

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Illustration of Divergence

\(\vec{F} = \langle x, 0 \rangle\)

\(\text{div } \vec{F} = f_x + g_y = 1 + 0 = 1\)

\(\rightarrow\) this means the rate of increase in volume of a small box as it moves in \(\vec{F}\) is positive

Vector field plot of \vec{F} = \langle x, 0 \rangle with horizontal arrows growing longer as they move right.

Small magnitude on left than right so it ends being stretched, so volume increases (positive divergence)

A small blue box is shown being stretched into a longer rectangle by a larger vector on the right side.