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<record version="6" id="1678">
 <title>Green's theorem</title>
 <name>GreensTheorem</name>
 <created>2002-02-02 21:51:16</created>
 <modified>2004-04-30 12:11:32</modified>
 <type>Theorem</type>
 <creator id="2727" name="mathcam"/>
 <author id="2727" name="mathcam"/>
 <author id="78" name="slider142"/>
 <classification>
	<category scheme="msc" code="26B20"/>
 </classification>
 <related>
	<object name="GaussGreenTheorem"/>
	<object name="ClassicalStokesTheorem"/>
 </related>
 <keywords>
	<term>path integrals</term>
	<term>evaluating path integrals</term>
	<term>curl of a vector field</term>
 </keywords>
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 <content>Green's theorem provides a connection between path integrals over a well-connected region in the plane and the area of the region bounded in the plane. Given a closed path $P$ bounding a region $R$ with area $A$, and a vector-valued function $\vec{F}=(f(x,y),g(x,y))$ over the plane,
$$\oint_P\vec{F}\cdot d\vec{x} = \int\!\!\!\int_{\!\!R} [g_1(x,y) - f_2(x,y)] dA$$
where $a_n$ is the derivative of $a$ with respect to the $n$th variable.
\begin{center}
\includegraphics[width=2.694444in]{greensthm}
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\paragraph{Corollary:}

The closed path integral over a gradient of a function with continuous partial derivatives is always zero. Thus, gradients are conservative vector fields. The smooth function is called the potential of the vector field.

\paragraph{Proof:}

The corollary states that

$$\oint_P\vec{\nabla}_h\cdot d\vec{x} = 0$$

We can easily prove this using Green's theorem.

$$\oint_P\vec{\nabla}_h\cdot d\vec{x} = \int\!\!\!\int_{\!\!R} [g_1(x,y) - f_2(x,y)] dA$$

But since this is a gradient...

$$\int\!\!\!\int_{\!\!R} [g_1(x,y) - f_2(x,y)] dA = \int\!\!\!\int_{\!\!R} [h_{21}(x,y) - h_{12}(x,y)] dA$$

Since $h_{12}=h_{21}$ for any function with continuous partials, the corollary is proven.</content>
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