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A double integral computes the accumulation of a function over a two-dimensional region :
where is the infinitesimal area element. In Cartesian coordinates ; in polar coordinates .
Common physical meanings:
The key skills are: choose coordinates, set up bounds, and evaluate as iterated single integrals using Fubini's theorem.
For a continuous over a rectangle :
Either order works, so pick the one that's easier to integrate.
Type I ( bounded by curves of ):
Type II ( bounded by curves of ):
For regions with circular symmetry, use , , :
The factor of from the Jacobian is essential — forgetting it is the most common error.
If an inner integral becomes intractable (e.g., has no elementary antiderivative), switching the order of integration often makes the problem solvable. Sketch the region first to find equivalent bounds in the other order.
Use polar when the region or integrand has circular symmetry — disks, annuli, sectors, or functions of x²+y². The Jacobian r often simplifies the integrand by canceling factors.
Fubini's theorem says that for a continuous function over a rectangle (or any region where the integral is absolutely convergent), the double integral equals an iterated integral, and the order of integration can be swapped without changing the result.
Sketch the region D. Find equivalent descriptions as Type I and Type II — that is, express the same region with x bounded by curves of y instead of y bounded by curves of x. Rewrite the integral with the new bounds.
The factor r comes from the Jacobian determinant of the transformation from (x,y) to (r,θ). Geometrically, a thin polar 'wedge' has area r·dr·dθ, not just dr·dθ.
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