Double Integrals in Polar Coordinates

Cut a region with circles about the origin and rays from it, and each cell is a piece of a ring whose area is its middle radius times Δr times Δθ. That middle radius is the r in r dr dθ. Mark a cell in either picture and compare its area in the two planes.

Double integral in polar coordinates
The Gaussian integral
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Lesson

The theory — Double Integrals in Polar Coordinates

A double integral in polar coordinates integrates over a region described by an angle θ and a distance r from the origin, with the area element dA = r dr dθ.

What each symbol means

r, θ
the distance from the origin and the angle from the positive x-axis: x = r cos θ, y = r sin θ
r̄, Δr, Δθ
a cell's middle radius, its width in r and its width in θ

Where the formula comes from

  1. Cut the region into polar cells. A cell between the radii r₁ and r₂ and the angles θ and θ + Δθ is the difference of two sectors, and its area factors into the middle radius times Δr times Δθ.
  2. Sum and take the limit. f at each cell times the cell's area, summed, tends to an iterated integral in which r̄ has become r. The limits of r may depend on θ.
  3. Square the Gaussian. A product of two one-variable integrals is a double integral over the plane, and in polar form the r gives e^(−r²) an antiderivative with a formula.
Assumes
The region is θ between two angles and, along each ray, r between two curves r₁(θ) ≤ r₂(θ). The integral over the whole plane is improper; growing discs and growing squares give the same π, because each square lies between two discs.

Problems solved in full

  1. The area of a disc 2 steps

    Find the area of the disc of radius R as a double integral in polar coordinates, and what you get if you forget the r.

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    1. The disc is 0 ≤ r ≤ R, 0 ≤ θ ≤ 2π, and dA = r dr dθ:

    2. Without the r:

    Answer

    πR², which is 3.1416 at R = 1. Without the r, 2πR: the circumference, a length.

  2. Inside a cardioid 2 steps

    Find the area inside the cardioid r = 1 + cos θ.

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    1. For each θ in [0, 2π], r runs from 0 to 1 + cos θ, and the inner integral is half the square of that limit:

    2. Over a full turn cos θ integrates to 0 and cos² θ to π:

    Answer

    3π/2 ≈ 4.7124.

  3. From x and y to r and θ 2 steps

    Evaluate ∫01 ∫0√(1−x²) (x² + y²) dy dx.

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    1. y runs from 0 up to the circle x² + y² = 1 and x from 0 to 1: the quarter of the unit disc in the first quadrant, which is 0 ≤ r ≤ 1, 0 ≤ θ ≤ π/2. And x² + y² = r²:

    2. Integrate:

    Answer

    π/8 ≈ 0.3927.

  4. A disc that does not sit on the origin 3 steps

    Find ∬ x dA over the disc x² + y² ≤ 2x, and from it the x-coordinate of the disc's centroid.

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    1. In polar coordinates the edge is r² = 2r cos θ, so r = 2 cos θ, and r ≥ 0 needs cos θ ≥ 0. θ runs from −π/2 to π/2, once round the circle; a full turn would trace it twice and double the answer.

    2. With x = r cos θ:

    3. The disc has radius 1 and area π:

    Answer

    ∬ x dA = π ≈ 3.1416, so the centroid is at x = 1, the centre of the disc.

  5. The volume of a ball 2 steps

    Find the volume of a ball of radius R as a double integral in polar coordinates.

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    1. The upper half is the volume under z = √(R² − x² − y²) over the disc r ≤ R:

    2. Substitute u = R² − r², so du = −2r dr; the r from the area element is what makes the substitution work:

    Answer

    4πR³/3, the volume found by slices earlier in the chapter.

  6. The Gaussian over a disc 2 steps

    Evaluate ∬ e^(−(x²+y²)) dA over the disc of radius R, and find its limit as R → ∞.

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    1. In polar form the integrand is e^(−r²), and the r beside it makes the antiderivative one with a formula:

    2. The θ-integral multiplies by 2π:

    Answer

    π(1 − e^(−R²)), which is 3.0841 at R = 2 and tends to π.

  7. ∫e^(−x²) dx = √π 3 steps

    Show that the integral of e^(−x²) over the whole line is √π.

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    1. Let I(b) be the integral from −b to b. Its square is a double integral over the square |x|, |y| ≤ b:

    2. The square contains the disc of radius b and lies inside the disc of radius b√2. The integrand is positive, so by problem 6:

    3. Both bounds tend to π as b → ∞, so I(b)² does too, and I(b) is positive:

    Answer

    √π ≈ 1.7725. At b = 2 the bounds are 3.0841 and 3.1405, and I(2)² ≈ 3.1123 lies between them.

  8. The constant in the normal distribution 2 steps

    Find the integral of e^(−x²/2) over the whole line, and explain the factor 1/√(2π) in the standard normal density.

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    1. Substitute x = √2 u, so dx = √2 du:

    2. Divide by √(2π) and the total is 1:

    Answer

    √(2π). So (1/√(2π)) e^(−x²/2) has total area 1, as a probability density must.

Leave out the r and the disc's area comes out as its circumference 🖖

Press Unit disc. With the r the integral is π ≈ 3.1416; without it the same limits give 2π ≈ 6.2832, the circumference, which is a length. ∫∫ dr dθ measures the rectangle the disc becomes in the rθ-plane, 1 by 2π, and in that plane every cell has the same area Δr Δθ, while in the disc the cells near the centre are slivers and those at the rim are broad. A cell between the radii r₁ and r₂ is a difference of two sectors, ½(r₂² − r₁²)Δθ, which factors as ½(r₁ + r₂) · (r₂ − r₁) · Δθ: the middle radius times Δr times Δθ, exactly. Mark a cell at the rim and then one at the centre and compare the two cell rows in the results. Because nothing was approximated, the sum over the grid prints π for this disc even with n = 1, a single cell.

The r you might forget is what makes ∫e^(−x²) dx come out 🖖

e^(−x²) has no elementary antiderivative, none built from powers, roots, exponentials, logarithms and trigonometric functions: Liouville proved it in the 1830s, and the page on non-elementary integrals runs his test. Over the whole line its integral is still exactly √π. Call that integral I. Then I² is ∫e^(−x²) dx times ∫e^(−y²) dy, which is the integral of e^(−(x²+y²)) over the whole plane, and in polar coordinates the integrand e^(−r²) arrives with an r beside it. r e^(−r²) has one: −½e^(−r²), so the inner integral is ½, the θ-integral multiplies it by 2π, and I² = π. Press Gaussian on a disc: the inner-integral row shows that bracket. Silvanus Thompson's life of Kelvin (1910) tells how Kelvin once wrote this result on the blackboard and told his class: “A mathematician is one to whom that is as obvious as that twice two makes four is to you. Liouville was a mathematician.”

The whole plane is a limit of squares, and the discs still give the right answer 🖖

I² was defined over squares, |x|, |y| ≤ b, and computed over discs. Press Gaussian on a square. The square holds the disc of radius b and sits inside the disc of radius b√2, and e^(−(x²+y²)) is positive, so its integral over the square lies between π(1 − e^(−b²)) and π(1 − e^(−2b²)). Both close on π, so the square's value must too. At b = 2 the three numbers are 3.0841, 3.1123 and 3.1405. Press Gaussian, b = 1: 1.9859, 2.231 and 2.7164, and the corners outside the inner disc carry 11% of the square's value. That is why the argument gives the integral over the whole line and only bounds over a finite interval: ∫e^(−x²) dx from −1 to 1 is 1.4936, and the discs place it between √1.9859 ≈ 1.4092 and √2.7164 ≈ 1.6482.

Learning path

Applications of integration

References (2)