In the plane, Greenās theorem bridges the circulation of a vector field around a simple closed curve with the double integral of its curl over the enclosed region. If a vector field is , then for a positively oriented curve bounding a region , the theorem states
Here the left side is a line integral measuring circulation along the boundary, while the right side accumulates the scalar curl over the interior. The equality reveals deep connections between local rotation and global circulation.
A key detail is orientation. Traversing the boundary counterclockwise corresponds to a positive orientation so that the double integral matches the line integral. Swapping direction changes the sign. Our calculator uses counterclockwise orientation for the rectangle defined by the start and end points you provide.
The boundary of a rectangle consists of four straight segments. Along each segment, either or is constant. We integrate or with respect to the varying variable using Simpsonās rule. For example, the bottom edge from to gives . Summing the four edges yields the total circulation.
The integrand on the right-hand side of Greenās theorem involves the partial derivatives and . We compute them symbolically with math.js
and evaluate at the midpoint of each subrectangle. Using a grid of 10 by 10 subrectangles, we multiply the mean value of the integrand by the area element and sum.
Students often struggle to connect abstract theorems to concrete numbers. By computing both integrals numerically, this calculator demonstrates that Greenās theorem truly holds for smooth vector fields. It can also serve as a quick check of hand calculations when solving homework problems or exploring fluid flow patterns.
Suppose and . For a unit square centered at the origin, Greenās theorem predicts the line integral equals twice the enclosed area. Our calculator replicates this example numerically, offering immediate insight into why rotation links to area.
George Green formulated his theorem in the nineteenth century as part of his investigations into electricity and magnetism. His work prefigured later results by Kelvin, Stokes, and Gauss, highlighting deep relationships between local derivatives and global flux. Today, Greenās theorem is a staple in vector calculus courses and underpins many engineering applications.
Numerical integration introduces approximation error. Our method uses a fixed grid and Simpsonās rule, which performs well for smooth fields but may struggle with rapid variation. For highly oscillatory functions or extremely small rectangles, you might need more subintervals. Nonetheless, the calculator captures the essence of Greenās theorem for many typical problems.
Greenās theorem is actually a special case of the more general KelvināStokes theorem in three dimensions. Exploring these connections leads to surface integrals and differential forms. Another fruitful path is applying the divergence theorem, which complements Greenās theorem for flux rather than circulation. Practicing with different vector fields builds intuition for these powerful ideas.
Enter functions and along with the rectangle bounds. The result shows the line integral around the rectangle and the double integral of the scalar curl. With the default orientation and units, the two values should match closely, providing compelling numeric evidence of the theorem.
Feel free to change the functions and region to explore different scenarios. Notice how reversing the bounds flips the sign, reminding us again that orientation matters. By experimenting, you deepen your understanding of how local rotation influences global behavior.
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