M408M Learning Module Pages

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Chapter 10: Parametric Equations and Polar Coordinates

Chapter 12: Vectors and the Geometry of Space


Chapter 13: Vector Functions


Chapter 14: Partial Derivatives


Chapter 15: Multiple Integrals


Learning module LM 15.1: Multiple integrals

Learning module LM 15.2: Multiple integrals over rectangles:

Learning module LM 15.3: Double integrals over general regions:

Learning module LM 15.4: Double integrals in polar coordinates:

      dA=rdrdθ
      Examples of polar integrals

Learning module LM 15.5a: Multiple integrals in physics:

Learning module LM 15.5b: Integrals in probability and statistics:

Learning module LM 15.10: Change of variables:


dr=rdrdθ

dA = r dr d theta

Conceptually, computing double integrals in polar coordinates is the same as in rectangular coordinates. After all, the idea of an integral doesn't depend on the coordinate system. If R is a region in the plane and f(x,y) is a function, then Rf(x,y)dA is what we get when we

  1. Chop R into a bunch of small pieces.
  2. Compute f(x,y)ΔA for each piece, where ΔA is the area of the piece.
  3. Add up the contributions of the pieces, and
  4. Take a limit as we chop R into smaller and smaller pieces.

The differences when working with polar coordinates are explained in the following video:


When working with rectangular coordinates, our pieces are boxes of width Δx, height Δy, and area ΔA=ΔxΔy. When working with polar coordinates, our pieces are polar rectangles. These are regions of the form θ[α,β], r[a,b]. The approximate contribution of a single box to our integral is f(ri,θj)ΔA, where ΔA is the area of the box. [Here we are thinking of f as a function of r and θ. If f is a function of x and y, then strictly speaking we should write f(rcos(θ),rsin(θ)) instead of f(r,θ).]

So what is the area of a polar rectangle? The polar rectangle is the difference of two pie wedges, one with radius b and one with radius a, and so has area ΔA=b22(βα)a22(βα)=b2a22(βα)=a+b2(ba)(βα)=rΔrΔθ,

where Δr=ba is the change in r and Δθ=βα is the change in θ.


Another way to understand this is to look at the shape of a small polar rectangle, like the shaded box in the figure above. This is almost a rectangular, only rotated and with slightly curved sides. One side has length Δr. The other had length approximately rΔθ. So the whole rectangle has approximate area rΔrΔθ.


Now we organize our boxes. Since the contribution of each box is approximately f(ri,θj)riΔrΔθ, the contribution of the boxes in the same thin pie wedge is approximately (baf(r,θj)rdr)Δθ.

Finally we put all the pie wedges together, to get a total of βα(baf(r,θ)rdr)dθ.

The infinitestimal area in rectangular coordinates is dA=dxdy. The infinitesimal area in polar coordinates is dA=rdrdθ.
Don't forget the factor of r!!

Double integrals in polar coordinates become iterated integrals f(x,y)dA = f(rcos(θ),rsin(θ))rdrdθ = f(rcos(θ),rsin(θ))rdθdr,
with appropriate limits of integration.