Many integration regions can be described conveniently in polar coordinates. Recall the meaning of the polar coordinate

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Output

Relationship to Cartesian:


Polar Coordinate Examples

Here are some sketched examples of polar coordinates:

Sketch

  1. The disk
  2. The semi-annulus
  3. The disk

The circle in the third example is given by:

Expanding and Simplifying:

Using conversion and


Double Integrals in Polar Coordinates

Suppose we wish to find the volume of the solid beneath the surface and above the region , where is described in polar coordinates. We seek:

where we have made the substitution , , and represents the area element in polar coordinates. To determine the area element, we must understand what it means to integrate over a polar region. The general polar region given by , where

represents the following sector:

Sketch

If we divide into sub-intervals of width , and into n sub-intervals of width , we obtain sub-sectors (see the right-side of the above figure).

Let’s determine the area of a sub-sector:

Sketch

For very small and , the sub sector is nearly a rectangle with height and width equal to the arc length of one side of the sector. If we choose the “long” side, the arc length is

Therefore:

When we take the , the polar area element is:

Polar Area Element

Using this expression, we obtain the following:

Important

If is continuous on a “polar rectangle” given by , , then:

Observe the extra factor of r that must be included!


Examples

Example

Evaluate:

where is the semi-annulus shown at the beggining, .

Solution

We integrate in polar coordinates with respect to and , so we must determine bounds on and . From the figure at the beggining, can be described as:

We make the substitutions , , , into the integrand to obtain:

Carry out the integration:

We use the half angle identity:

Remark

The half angle identities will be useful for these problems:


The Gaussian Integral

We will now prove the famous result:

This is the so-called Gaussian Integral

Proof

Observe that:

(*)

because we can write the first integrand as a product of two functions independent of each other. The improper integrals on the right-hand side have the same value, so (*) says:

(**)

We will compute. the double integral on the left-hand side with polar coordinates.

The integration region is , , i.e., the entire xy-plane. In polar coordinates, we can describe the xy-plane by , . The Double Integral becomes:

Solving with I1 and I2

This is an improper integral of the first kind:

Using U-sub: means

Now for I2

Therefore:

Substituting into (**), We get:

Taking the square root yields the result.

Remark

We know it’s the positive square root because is a positive function.