Why Does the Area Element Vanish at the Origin in Polar Coordinates?

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Discussion Overview

The discussion revolves around the behavior of the area element in polar coordinates, particularly at the origin. Participants explore the implications of the vanishing area element at \( r = 0 \) within the context of mappings from the unit disk to polar coordinates, examining both theoretical and practical aspects of coordinate systems.

Discussion Character

  • Exploratory
  • Debate/contested
  • Technical explanation
  • Conceptual clarification

Main Points Raised

  • Some participants note that the area element \( dx \wedge dy \) vanishes at \( r = 0 \) and question the implications of this singularity in polar coordinates.
  • There is a suggestion that the mapping from the unit disk to polar coordinates is not one-to-one at the origin, leading to potential inconsistencies.
  • Participants discuss whether the point \( (0,0) \) should be removed from the disk to avoid inconsistencies in equations involving the area element.
  • Some argue that removing the origin is problematic as it affects functions defined on the disk, suggesting instead to change the coordinate system based on the task at hand.
  • Concerns are raised about the mapping \( [0,1] \times (0,2\pi] \) not being open, questioning its validity as a chart at \( r = 0 \).
  • There is a discussion about the necessity of using valid charts for coordinate expressions, particularly at points where the coordinate system is not defined.
  • Some participants express a preference for Cartesian coordinates over polar coordinates, citing a lack of familiarity with the latter.
  • One participant mentions that the area element is non-zero in charts that cover the origin, contrasting with the polar coordinate system's limitations.

Areas of Agreement / Disagreement

Participants express differing views on whether the origin should be excluded from the disk and the implications of the vanishing area element. There is no consensus on the best approach to address the issues raised regarding the coordinate system and its validity at the origin.

Contextual Notes

Participants highlight limitations in the polar coordinate mapping, particularly at \( r = 0 \), and the necessity for a valid chart to interpret coordinate expressions accurately. The discussion reflects a range of perspectives on how to handle singularities in coordinate systems.

davidge
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Consider the mapping ##f: \mathbb{D}^1 \longrightarrow [0,1] \times (0,2 \pi]## where ##\mathbb{D}^1## is the unit disk. This is the familiar polar coordinate system.

The area element is ##dx \wedge dy## in ##\mathbb{D}^1## and ##r dr \wedge d\theta## in ##[0,1] \times (0,2 \pi]##*. Now at ##r = 0## this vanishes. But ##dx \wedge dy = r dr \wedge d\theta## and that means ##dx \wedge dy = 0## as well.

We know that the polar system is singular at ##r = 0## because there cannot be a bijection: for every ##\theta \in (0,2 \pi]## we have the point ##(0,0)## in ##\mathbb{D}^1##.

But what is the meaning of the vanishing area element ##dx \wedge dy##?

*I know this is two dimensional and the area element as defined in vector calculus as the vector product of two vector requires a third vector, which means a third dimension. But I think this is not relevant here.
 
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davidge said:
Consider the mapping ##f: \mathbb{D}^1 \longrightarrow [0,1] \times (0,2 \pi]## where ##\mathbb{D}^1## is the unit disk. This is the familiar polar coordinate system.

The area element is ##dx \wedge dy## in ##\mathbb{D}^1## and ##r dr \wedge d\theta## in ##[0,1] \times (0,2 \pi]##*. Now at ##r = 0## this vanishes. But ##dx \wedge dy = r dr \wedge d\theta## and that means ##dx \wedge dy = 0## as well.

We know that the polar system is singular at ##r = 0## because there cannot be a bijection: for every ##\theta \in (0,2 \pi]## we have the point ##(0,0)## in ##\mathbb{D}^1##.

But what is the meaning of the vanishing area element ##dx \wedge dy##?

*I know this is two dimensional and the area element as defined in vector calculus as the vector product of two vector requires a third vector, which means a third dimension. But I think this is not relevant here.
It means that you have allowed the RHS to be multiplied by zero and the LHS not. The equations doesn't hold for ##r=0\,##.
 
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fresh_42 said:
The equations doesn't hold for ##r=0\,##.
Does it mean we have to remove the point ##(0,0)## from the disk?
 
davidge said:
Does it mean we have to remove the point ##(0,0)## from the disk?
In order to do what? I consider ##(dx,dy)## as Cartesian coordinates. If we give them coefficients, zero shouldn't be a problem. To me it is as if you asked, whether the origin of the plane should be removed, because the standard basis vectors aren't zero, whereas the radius can be zero.
 
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fresh_42 said:
To me it is as if you asked, whether the origin of the plane should be removed, because the standard basis vectors aren't zero, whereas the radius can be zero.
Yes, this is what I was asking you
fresh_42 said:
I consider ##(dx,dy)## as Cartesian coordinates.
Me too
fresh_42 said:
In order to do what?
In order not to have a inconsistent equation when ##r = 0##.
 
Well, the relation ##(0,0) \longleftrightarrow \{0\} \times (0,2\pi]## is obviously not one-to-one which causes problems. To remove a point is problematic, as it directly affects the functions defined on ##\mathbb{D}^1##. I'd rather change the coordinate system depending on the task.
 
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fresh_42 said:
Well, the relation ##(0,0) \longleftrightarrow \{0\} \times (0,2\pi]## is obviously not one-to-one which causes problems. To remove a point is problematic, as it directly affects the functions defined on ##\mathbb{D}^1##. I'd rather change the coordinate system depending on the task.
Any examples of such coordinate systems?
This is not a specific problem, I was just thinking about what I mentioned in post #1.
 
I assume in most cases it doesn't make a difference. If so, I'd simply use the Cartesian version, but that's only because I'm no big fan of polar coordinates. It would be interesting to have an example, where it makes a difference to see, what exactly shouldn't work.
 
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Basically, your coordinate change map is not defined for r=0:

We have:
##x=rcos\theta ##
## y=rsin\theta ##
But this holds for ## r \neq 0 ## only , as you said . Then the same is true for ## dx \wedge dy = (\frac {\partial}{\partial \theta}d\theta+ \frac{\partial}{\partial r}dr )( rcos\theta+ ysin\theta)##. The wedge is not defined at 0 because the coordinate expression for r=0 is not defined.
EDIT: the one way I can see ##dx \wedge dy ## turned into 0 is if the determinant of the Jacobian of a change of coordinate is 0. This is what ##f(x)dx\wedge dy ## measures; how much f(x) stretches/shrinks the area element under a trasnformation.
 
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  • #10
WWGD said:
EDIT: the one way I can see ##dx \wedge dy ## turned into 0 is if the determinant of the Jacobain of a change of coordinate is 0
Which is not the case we are considering, because for this case we as you said, ##r=0## is not on the domain, isn't?
 
  • #11
davidge said:
Which is not the case we are considering, because for this case we as you said, ##r=0## is not on the domain, isn't?
Right, we are not really transforming the space, we are expressing it in different terms, i.e., changing coordinate systems, so no squashing ( nor stretching) is happenning. EDIT: By ( many) definition(s) , actually , a change of variable is supposed to be a diffeomorphism, meaning the ais invertible,and therefore its determinant is non-zero. Which kind of makes sense, that you would want that for a coordinate change.
 
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  • #12
Am I the only one bothered by the fact that the set ##[0,1]\times [0,2\pi)## is not open and so the described mapping is not a chart? Polar coordinates can never give you a chart at ##r=0## and so it makes no sense to try to interpret coordinate expressions for tensors in polar coordinates at the origin.
 
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  • #13
Orodruin said:
Am I the only one bothered by the fact that the set ##[0,1]\times [0,2\pi)## is not open and so the described mapping is not a chart? Polar coordinates can never give you a chart at ##r=0## and so it makes no sense to try to interpret coordinate expressions for tensors in polar coordinates at the origin.
But I think the map is just intended to be a (local) change of coordinates. Is this equivalent to ##[0,1] \times [0,2\pi) ## being a chart?EDIT: I can see how a manifold is a way of assigning coordinates, but I had never seen things that way. Still, I agree, the coordinate change is a local diffeomorphism so it should preserve the topology of ##\mathbb D^1 ##.
 
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  • #14
WWGD said:
But I think the map is just intended to be a (local) change of coordinates. Is this equivalent to ##[0,1] \times [0,2\pi) ## being a chart?
A chart is a homeomorphism from an open subset of the manifold to an open subset of ##\mathbb R^n##. It does not need to cover the entire manifold. Remove ##r=0##, ##r=1## and ##\theta = 0## and you have a chart that covers almost the entire disc.
 
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  • #15
@Orodruin I've been considering ##[0,1] \times [0,2 \pi)## throughout this thread because that set covers the entire disk and I think it's the most familiar way of mapping points on the disk, although it's not homeomorphic to ##\mathbb{R}^2##.
Orodruin said:
it makes no sense to try to interpret coordinate expressions for tensors in polar coordinates at the origin.
Is the area element and all other quantities defined only when we have charts? Is it what you mean here?
 
  • #16
davidge said:
@Orodruin I've been considering ##[0,1] \times [0,2 \pi)## throughout this thread because that set covers the entire disk and I think it's the most familiar way of mapping points on the disk, although it's not homeomorphic to ##\mathbb{R}^2##.

Is the area element and all other quantities defined only when we have charts? Is it what you mean here?

If you want to use the coordinate expressions at a point, you must use a chart that is valid at that point. Writing ##r\, dr\wedge d\theta## makes no sense at ##r = 0## because your coordinate system does not define a chart there. There are some charts that cover all of the disc, your coordinate system with the given set is not one of them because it is not a chart. If you use any chart that covers the origin (such as Cartesian coordinates), you will find that the area element is non-zero there.
 
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  • #17
Orodruin said:
If you want to use the coordinate expressions at a point, you must use a chart that is valid at that point. Writing ##r\, dr\wedge d\theta## makes no sense at ##r = 0## because your coordinate system does not define a chart there. There are some charts that cover all of the disc, your coordinate system with the given set is not one of them because it is not a chart. If you use any chart that covers the origin (such as Cartesian coordinates), you will find that the area element is non-zero there.
I got it. Thanks.
 
  • #18
davidge said:
Consider the mapping ##f: \mathbb{D}^1 \longrightarrow [0,1] \times (0,2 \pi]## where ##\mathbb{D}^1## is the unit disk. This is the familiar polar coordinate system.
This mapping cannot be continuous.

In the other direction the map is continuous but singular.
 
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  • #19
lavinia said:
In the other direction the map is continuous but singular.
Where it is singular?
 
  • #20
davidge said:
Where it is singular?
The map in the other direction maps the entire half open interval ##{0}×(0,2π]## onto the center of the unit disk.
 
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  • #21
lavinia said:
The map in the other direction maps the entire half open interval ##{0}×(0,2π]## onto the center of the unit disk.
Oh, yea. Thanks.
 
  • #22
lavinia said:
This mapping cannot be continuous.

In the other direction the map is continuous but singular.
Are you referring to the coordinate change map ##x=rcos\theta, y=rsin\theta ##?
 
  • #23
WWGD said:
Are you referring to the coordinate change map ##x=rcos\theta, y=rsin\theta ##?

The map from the disk to ##[0,1]×(0,2π]## cannot be continuous. The reverse is singular.
 
  • #24
lavinia said:
The map from the disk to ##[0,1]×(0,2π]## cannot be continuous. The reverse is singular.
I meant, by "The map" , are you referring to the change of variable map ## x=rcos\theta, y =rsin\theta ##?
 
  • #25
WWGD said:
I meant, by "The map" , are you referring to the change of variable map ## x=rcos\theta, y =rsin\theta ##?

The OP described the inverse of polar coordinates as a surjective map ##D^1→[0,1]×(0,2π]##. If this map were continuous - as you also pointed out - then ##[0,1]×(0,2π]## would be compact - which it isn't. So no surjective map can be continuous.

The reverse map from ##[0,1]×(0,2π]→D^1## can be defined as ##(α,β) →(α##cos ##(β),α## sin##(β))## but this map is singular.
 
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