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In physics and mathematics, Green's theorem gives the relationship between a line integral around a simple closed curve C and a double integral over the plane region D bounded by C. It is the two-dimensional special case of the more general Stokes' theorem, and is named after British mathematician George Green. Let C be a positively oriented, piecewise smooth, simple closed curve in the plane R2, and let D be the region bounded by C. If L and M are functions of (x, y) defined on an open region containing D and have continuous partial derivatives there, then For positive orientation, an arrow pointing in the counterclockwise direction may be drawn in the small circle in the integral symbol. In physics, Green's theorem is mostly used to solve two-dimensional flow integrals, stating that the sum of fluid outflows at any point inside a volume is equal to the total outflow summed about an enclosing area.
[edit] Proof when D is a simple regionThe following is a proof of the theorem for the simplified area D, a type I region where C2 and C4 are vertical lines. A similar proof exists for when D is a type II region where C1 and C3 are straight lines. The general case can be deduced from this special case by approximating the domain D by a union of simple domains. If it can be shown that and are true, then Green's theorem is proven in the first case. Define the type I region D as pictured on the right by: where g1 and g2 are continuous functions on [a, b]. Compute the double integral in (1): Now compute the line integral in (1). C can be rewritten as the union of four curves: C1, C2, C3, C4. With C1, use the parametric equations: x = x, y = g1(x), a ≤ x ≤ b. Then With C3, use the parametric equations: x = x, y = g2(x), a ≤ x ≤ b. Then The integral over C3 is negated because it goes in the negative direction from b to a, as C is oriented positively (counterclockwise). On C2 and C4, x remains constant, meaning Therefore, Combining (3) with (4), we get (1). Similar computations give (2). [edit] Relationship to the Stokes theoremGreen's theorem is a special case of Stokes' theorem, when applied to a region on the xy-plane: We can augment the two-dimensional field into a three-dimensional field with a z-component that is always 0: Start with the left side of Green's theorem: Then by Stokes' Theorem: The surface S is just the region in the plane D, with the unit normals pointing up (in +z direction) to match the "positive orientation" definitions for both theorems. The expression inside the integral becomes Thus we get the right side of Green's theorem [edit] Relationship to the divergence theoremConsidering only two-dimensional vector fields, Green's theorem is equivalent to the following two-dimensional analogue of the divergence theorem: where To see this, consider the unit normal in the right side of the equation. Since Now let the components of which by Green's theorem becomes [edit] See also
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