Integrating f on R²-U: Evaluating the Integral

In summary, we need to determine if the function f(x,y) = 1/(x^2 + y^2) is integrable over the set R^2 - \overline{U}, where U is an open set in R^2 consisting of all x with a Euclidean norm of less than 1. To do so, we can use the sequence of sets A_n = {(r, \theta)| 1 < r < n, 0 < \theta < 2\pi} in the polar plane whose infinite union will equal R^2 - \overline{U}. We can then show that the integral of f over A_n is unbounded, implying that the integral over R^2 - \
  • #1
mathmonkey
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0

Homework Statement



Let U be the open set in [itex]R^2[/itex] consisting of all x with (Euclidean norm) [itex] ||x|| < 1.[/itex] Let [itex] f(x,y) = 1/(x^2 + y^2)[/itex] for [itex] (x,y) \not = 0.[/itex] Determine whether [itex] f [/itex] is integrable over [itex] R^2 - \overline{U}; [/itex] if so, evaluate it.

Homework Equations


[itex]g:R^2 \rightarrow R^2 [/itex] is the polar coordinate transformation defined by [itex] g(r, \theta ) = (r\cos \theta , r\sin \theta ). [/itex]


The Attempt at a Solution


My thought is to use the sequence of sets [itex] A_n = \{(r,\theta )| 1<r<n, 0<\theta < 2\pi \}[/itex] in the polar plane whose infinite union will equal [itex] R^2 - \overline{U} [/itex], where I can then show that [itex]\int _{A_N} f [/itex] is unbounded, implying [itex] \int _{R^2 - \overline{U}} f[/itex] does not exist. However, in order to use the polar coordinate transform, I need to show that [itex]g [/itex] is a diffeomorphism. However, I'm not sure how to show that g is bijective. If anyone has any advice, I would be very grateful. Thanks!
 
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  • #2


I don't think the integral exists first of all, because you have 1/r2 integrated against dA=rdθdr, so you are integrating (1/r)dr, which diverges near 0 (or to ∞, by the way; it's symmetrically divergent in a sense).

also, i think you meant r goes from 1/n to 1.

To get the diffeomorphism you'll need an open set, r in (1/n,1) and θ in (0,π). You could give θ a larger region, just has to be smaller than [0,2π). But it will be easier to show the diffeomorphism on a smaller region, and the integral is symmetric enough, so you could just take half the region (or smaller).

To show it is one-to-one, how about showing if cos(θ)=cos(θ'), then θ=θ' (for θ in (0,π)). To work with (0,2π), you'll need to make sure you understand what the inverse trig functions do with some care.

EDIT:

if I think about it, if sin(θ)>0 means θ is in (0,π), sin(θ)=0 means θ=π, and sin(θ)<0 means θ is in (π,2π). Then use cos to get 1-1 on each region, and stir the logic to get a neat statement.
 
  • #3


Assuming your approach will work, I'm just going to talk about the polar coordinate transformation. First off, [itex]g:R^2\rightarrow R^2[/itex] is not a diffeomorphism. Think about it; in the polar plane, you describe a point by its radius and an angle. However, to remain consistent, we throw out the point at the origin (because the origin could be assigned any angle), and we restrict our angles to being in some interval of length [itex]2\pi[/itex] (since otherwise, any point could be described by an infinite number of angles). Customarily, we choose [itex](-\pi,\pi][/itex] (or [itex](-\pi,-\pi)[/itex] if we are interested in differentiability, as we require open sets).

So really, we can make g a diffeomorphism by choosing the domain and codomain carefully. Since your set [itex]\overline{U}[/itex] contains the origin, and we are only interested in the behaviour of your function and its integral over [itex]R^2-\overline{U}[/itex], this is OK.

I claim that [itex]g:(0,\infty)\times(-\pi,\pi)\rightarrow R^2\backslash\{0\}[/itex] defined by [itex]g(r,\theta)=(r\cos\theta,r\sin\theta)[/itex] is a diffeomorphism which is continuous on [itex](0,\infty)\times(-\pi,\pi][/itex].

As for proving it is a bijection, simply find the inverse! I then leave it to you to check anything else.
 
  • #4


christoff said:
As for proving it is a bijection, simply find the inverse! I then leave it to you to check anything else.

Simply finding the inverse is not enough, for instance does the inverse imply diffeomorphism on (0,3π)? Since your proof proves something false, there must be an error. Finding the inverse may not get you to the proof any faster. Of course, it was my first thought as well, but then I worried about that larger interval business.

EDIT: Now I'm not sure we don't need the inverse, it may help with the r part. You may have to play around with it to find the most efficient/elegant proof.
 
  • #5
algebrat said:
Simply finding the inverse is not enough, for instance does the inverse imply diffeomorphism on (0,3π)?

Certainly not; can't have a diffeomorphism without a bijection, and [itex](0,3\pi)[/itex] is too big for that. I only intended on ever explaining how one could turn g into a bijection.

algebrat said:
Since your proof proves something false, there must be an error.

Not sure what you mean by false... One can define the inverse in terms of the arctan function. Once you know that, you can just check that g has no critical points, and you have a diffeomorphism. I would link to something here as a source, but I'm not at 10 posts yet :P

Edit: I'm at 10 posts now. Here's a link: http://math.bard.edu/belk/math461/MultivariableCalculus.pdf
 
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  • #6


So, I believe I need to show that given the set [itex] A_N = \{(r, \theta)| 1 < r < N, 0 < \theta < 2\pi \} [/itex] in the [itex] (r, \theta) [/itex] plane and the set [itex] U_N = \{(x,y)| 1<x^2 + y^2 < N \text{ and } x<0 \text{ when } y=0\}[/itex] in the [itex] (x,y) [/itex] plane, then [itex]g:A_N \rightarrow U_N [/itex] is a diffeomorphism.

To show that it is one-to-one, assume that [itex]g(r, \theta ) = g(s, \tau ) [/itex]. Then, [itex] (r\cos \theta , r\sin \theta ) = (s\cos \tau , s\sin \tau ), [/itex], which implies that [itex]r^2 \cos ^2 \theta + r^2 \sin ^2 \theta = s^2 \cos \theta + s^2 \sin \theta [/itex], which of course implies that [itex] r^2 = s^2[/itex], or that [itex] r = s [/itex] since both are restricted to be positive numbers. Then, we can easily show that [itex] \theta = \tau [/itex], completing the proof that [itex] g [/itex] is one-to-one.

The proof that [itex] g [/itex] is onto comes from the inverse function [itex] g^{-1}[/itex] defined as [itex] g^{-1}(x,y) = (\sqrt{x^2 + y^2}, \arctan({y/x}))[/itex].

Hence, [itex] g [/itex] is bijective, and moreover [itex] Det(Dg(r, \theta )) = r[/itex] for all [itex](r, \theta ) [/itex] which is non-zero, so [itex] g [/itex] is a diffeomorphism.

Now that [itex] g [/itex] is a diffeomorphism, I can invoke the change of variables theorem to show that [itex] \int _{U_N} f = \int _{A_N} 1/(r^2 \cos ^2 \theta + r^2 \sin ^2 \theta )r[/itex], which is unbounded as [itex] N \rightarrow \infty[/itex]. Hence, the integral does not exist.

How does this proof look? Thanks again for the help!
 
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FAQ: Integrating f on R²-U: Evaluating the Integral

What is the definition of an integral on R²-U?

An integral on R²-U is a mathematical concept used to calculate the area under a curve in a two-dimensional plane, excluding a certain set of points, known as the "excluded set" or "hole." This is denoted by the symbol ∫f(x, y)dA, where f(x, y) is the function being integrated and dA represents the area element.

How is the integral on R²-U different from a regular integral on R²?

The integral on R²-U is different from a regular integral on R² because it excludes a certain set of points, while a regular integral on R² includes all points in the given region. This exclusion of points results in a hole in the region being integrated, which requires a different approach to calculating the integral.

What is the significance of the excluded set in an integral on R²-U?

The excluded set in an integral on R²-U plays a crucial role in determining the value of the integral. It represents a hole or gap in the region being integrated, and the presence of this hole affects the calculation of the integral as it changes the bounds of integration and requires a different method of evaluation.

How do you evaluate an integral on R²-U?

Evaluating an integral on R²-U involves breaking down the integral into smaller, more manageable parts. This can be done by dividing the region being integrated into subregions, each of which can be evaluated separately. The integral can then be calculated by summing the individual subregions and taking into account the excluded set.

What are some real-life applications of integrating on R²-U?

Integrating on R²-U has various real-life applications, particularly in fields such as physics, engineering, and economics. For example, in physics, it can be used to calculate the work done by a force on an object moving in a two-dimensional plane with a hole in its path. In economics, it can be used to calculate the profit or loss of a business with certain excluded expenses. In general, it is a useful tool for determining the total value or quantity of something when a certain aspect is excluded from consideration.

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