We study integrals over basic regions.
Double integrals
Suppose you have a function . A graph of this function is a surface in . For example:
We are interested in the “signed volume” between this surface and the -plane. This means that the space above the plane under , will have a positive volume. Space above and under the -plane will have a “negative” volume. This is similar to the notion of “signed area” used before. If we want to compute the signed volume of a surface defined by over a rectangular region, say the rectangle defined by we break into slices parallel to the -axis, and slices parallel to the -axis. This allows us to consider boxes of dimension where is a point in -rectangle:
Computing the volume of each of these boxes approximates the signed volume enclosed by the surface:
Letting the number of rectangles in the -direction and -direction go to infinity, we will have that goes to zero, and we will find the exact volume enclosed by our surface when bounded by the region . This leads to our definition of a double integral:
How do we compute a double integral with calculus? We use an iterated integral.
- Double integrals can be computed via iterated integrals.
- The order of integration can be changed, as long as the bounds are changed as well.
Now let’s work some examples:
In our next example, we will see that it is sometimes easier to apply Fubini’s Theorem and integrate with respect to one variable or the other.
Triple integrals
Using a similar technique to how we made boxes to define double integrals, we can make four-dimensional boxes to define a triple integral that computes the signed hypervolume bounded by a hypersurface and a three-dimensional region. How do we compute a triple integral with calculus? We use Fubini’s theorem again, along with iterated integrals.
Let’s do an example.
We’ve just begun our journey with integrals. Next, we’ll think about more complex regions! For some interesting extra reading check out: