Iterated Integration
over a rectangle is two ordinary integrals nested: inner in (holding ), then outer in — and Fubini says the order does not matter for continuous . Over non-rectangles, the INNER limits depend on the outer variable: covers the triangle under .
Why nesting works: with fixed, the inner integral is the area of the slice of the solid under standing above the line at — a cross-sectional area . The outer integral then adds up the slices, the way a loaf's volume is the sum of its slices. Fubini's theorem says slicing the other way gives the same volume. For the triangle under on , the slice at runs from up to , and those are the inner limits.
On disks and rings, switch to , — but the area element becomes . That extra (a small polar rectangle is wide, not ) is the single most-forgotten factor in the course. It is also the magic that evaluates .
Why the : the circles const and the rays const cut the plane into cells whose size depends on how far out they are. A cell at radius spanning an angle is wide along the arc and deep, so its area is about : cells far from the origin are bigger, and the factor records it. For the disk of radius , , the correct area; dropping the gives .
— when the integrand factors and the region is a rectangle, the double integral is a product of singles.
Why it factors: in the inner integral , is a constant and comes out, leaving . The outer integral is then . This shortcut needs both conditions: an integrand of the form and constant limits. Over the triangle below , the same does not split, because the inner limit ties the two integrals together.
A double integral is how you total anything spread over a region: mass from density, rainfall from intensity maps, probability from joint densities. The average value of over a region is divided by the area — centroids and centers of mass are just coordinate-weighted versions of that same computation.
Find the average value of over the rectangle .
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The average is the integral divided by the area. The integrand does not involve , so the double integral factors: . The area is , so the average is . Sanity check: is spread evenly from to , so its average must be the midpoint .
Regions Between Curves, and Reversing the Order
A region between two graphs, for , is integrated in columns: . A region between for is integrated in rows: . To reverse the order, redraw the region and read the new limits off lines in the other direction.
Why redraw: the limits encode the shape, and describing a shape column by column uses different formulas from describing it row by row. The inner limits are the curves a line crosses as it passes through the region, so they change when the lines change direction; the outer limits are the extreme positions of those lines. Swapping the symbols without looking at the region almost never produces the same region.
Compute , where lies between and . The curves meet where , at and . In columns, for a vertical line enters at the parabola and leaves at the line: .
That is . In rows: for , a horizontal line enters at the line and leaves at the parabola , so the integral is . Note that the curve that was the lower limit in columns is the right-hand limit in rows.
Evaluate . The inner integral has no elementary antiderivative, so the order as given is stuck. Read the region instead: and , which is the set to the right of the parabola — the region under for .
In columns, the line at runs from to , so the integral is . The inner integration produced the factor , which is exactly what the substitution needs: the integral is .
Swapping the limits as symbols. is the area under , which is . Rewriting it as describes — the part of the unit square to the left of the parabola — and gives , the complementary piece (). The correct reversal is .
Evaluate by reversing the order of integration.
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The region is , : above the curve (that is, ) and below . In rows, runs from to and, at height , runs from to . So the integral is . The inner integration supplied the that the substitution needs.
Polar Regions
A region described by and has
The -limits are the directions of the rays that meet the region; the -limits are where each ray enters and leaves it.
Why this handles off-centre shapes: a boundary given as is crossed once by each ray, so rays play the part vertical lines played before. The circle , for instance, becomes , that is : a circle through the origin, traced once as runs from to .
Compute over the disk , which is . The rays with enter at the origin and leave at , and , so the integral is .
So the integral is . Check: the disk has area and centre , so the average value of over it is , and . The area itself comes out the same way: .
Compute over the quarter ring , . In polar form , and with the area element the integrand is .
All four limits are constants, so the integral splits: . Rings and sectors are the rectangles of polar coordinates.
Letting run over a full turn for . For , , and the curve retraces the same circle with negative . So counts the disk twice. The rays that actually meet the disk are those with .
Evaluate over the quarter disk , , .
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In polar coordinates the region is , , and the integrand is . With the area element it becomes : . Forgetting the area element would give , half the true value.
Proofs & Why It Matters
A small polar cell between radii and and angles and is nearly a rectangle: its radial side has length , and its circular side is an arc of radius subtending , of length .
So its area is (exactly , and the second term vanishes in the limit). Summing cells gives .
Let . Then over the plane — switch to polar: . The extra makes the inner integral elementary (): it equals , so and . No one-variable method ever evaluates this integral — the plane does.
Going Deeper: Explanations & Worked Problems
A double integral over a non-rectangle succeeds or fails at the limits. The procedure: (1) sketch the region; (2) choose an order, say inner , outer ; (3) for the OUTER variable record the full interval of values the region occupies; (4) for the INNER variable, freeze , draw the vertical line through the region, and record where it enters and exits — those (usually -dependent) heights are the inner limits. For the triangle with vertices (below the line ): runs to ; the vertical line at enters at and exits at , so . Reversing the order re-derives, never guesses: a horizontal line at height enters at and exits at , so the same integral is . Fubini guarantees the two agree — and when one order is hard (or impossible, as with ), swapping is the standard rescue.
Compute over the triangle below on .
Order 1 (inner ):
Step 1 — inner: .
Step 2 — outer: .
Order 2 (inner ):
Step 1 — inner: (the integrand is constant in , so multiply by the interval length).
Step 2 — outer: . Both orders give — Fubini in action, and a complete template: inner antiderivative, evaluate at the -dependent limits, then an ordinary outer integral.
Compute over the disk of radius .
Step 1 — translate to polar: and , so the integrand becomes .
Step 2 — limits: the full disk is , .
Step 3 — inner integral: .
Step 4 — outer: .
Step 5 — the cautionary rerun: forgetting the extra gives instead of — a wrong answer with no warning sign attached. Writing "" before computing anything is the habit that prevents it.