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Multiple Integration: Computing Volumes in Polar and Three-Dimensional Coordinates, Study notes of Differential and Integral Calculus

This chapter explores multiple integration, which allows the computation of volumes in polar and three-dimensional coordinates. The symmetry of volumes, the adaptation of the method for more complicated regions, and the concept of triple integrals for computing volumes in three-dimensional space.

What you will learn

  • How does the method of multiple integration adapt to more complicated regions?
  • What is the significance of symmetry in multiple integration?
  • How is multiple integration used to compute volumes in polar coordinates?

Typology: Study notes

2021/2022

Uploaded on 09/12/2022

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CHAPTER 15 MULTIPLE INTEGRATION
one-eighth of the sphere. We know the formula for volume of a sphere is (4/3)πr3, so the
volume we have computed is (1/8)(4/3) π23 = (4/3) π, in agreement with our answer.
This example is much like a simple one in rectangular coordinates: the region of
interest may be described exactly by a constant range for each of the variables. As with
rectangular coordinates, we can adapt the method to deal with more complicated
regions.
We can rewrite the integral as shown because of the symmetry of the volume; this
avoids a complication during the evaluation. Proceeding:
pf3
pf4

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one-eighth of the sphere. We know the formula for volume of a sphere is (4/3)πr^3 , so the volume we have computed is (1/8)(4/3) π2^3 = (4/3) π, in agreement with our answer. This example is much like a simple one in rectangular coordinates: the region of interest may be described exactly by a constant range for each of the variables. As with rectangular coordinates, we can adapt the method to deal with more complicated regions.

We can rewrite the integral as shown because of the symmetry of the volume; this avoids a complication during the evaluation. Proceeding:

You might have learned a formula for computing areas in polar coordinates. It is possible to compute areas as volumes, so that you need only remember one technique. Consider the surface z = 1, a horizontal plane. The volume under this surface and above a region in the x-y plane is simply 1 ・ (area of the region), so computing the

volume really just computes the area of the region.