Area Differential in Cartesian and Polar Coordinates

Click For Summary

Discussion Overview

The discussion centers on the area differential in Cartesian and polar coordinates, specifically how to derive the relationship between the two forms: ##dA = dx \, dy## and ##dA = r \, dr \, d\theta##. Participants explore the mathematical transformations involved and express confusion regarding the derivation process and the use of partial derivatives.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • One participant states that the area differential in Cartesian coordinates is ##dx \, dy## and in polar coordinates is ##r \, dr \, d\theta##, questioning how to prove their equivalence.
  • Another participant suggests that partial differentiation of one coordinate with respect to the other is necessary for the conversion, expressing frustration with the methods presented in Griffiths' text.
  • Some participants express confusion about the determinant of the Jacobian matrix and its role in the transformation of differentials.
  • There are discussions about the validity of certain mathematical manipulations involving differentials, with some participants questioning whether specific operations are allowed or useful.
  • One participant mentions the need to consider the properties of multilinear maps in relation to the determinant and its effect on volume scaling.
  • Several participants express uncertainty about the clarity of the original post and the mathematical expressions used, indicating that some content may have been lost or misformatted.

Areas of Agreement / Disagreement

Participants do not reach a consensus on the best method for deriving the relationship between the area differentials. There are multiple competing views on the approach to take, and confusion remains regarding the mathematical details involved.

Contextual Notes

Limitations include unresolved assumptions about the mathematical steps required for the transformation and the clarity of the expressions used in the discussion. Some participants indicate that the methods referenced may not be adequately covered in the texts they are using.

Zap
Messages
406
Reaction score
120
TL;DR
How do we get rdrdt from dxdy?
The area differential ##dA## in Cartesian coordinates is ##dxdy##.
The area differential ##dA## in polar coordinates is ##r dr d\theta##.
How do we get from one to the other and prove that ##dxdy## is indeed equal to ##r dr d\theta##?

##dxdy=r dr d\theta##
The trigonometric functions are used to obtain the conversions ##x=r \cos \theta ## and ##y=r \sin \theta ## . If we differentiate both with respect to the polar angle ##\theta##,
$$
dx d\theta = \cos \theta dr d\theta -r \sin \theta\; , \;dy d\theta = \sin \theta dr d\theta +r \cos \theta
$$
The differentials then become
$$
dx= \cos \theta dr -r \sin \theta d\theta \; , \;dy = \sin \theta dr + r \cos \theta dr \theta
$$
which to me does not make any sense.
It seems as though finding ##dr d\theta ## is what we must do, but how? What am I missing?
How do we prove that indeed ...
$$
dx dy = r dr d\theta
$$
Is it in Griffiths? On what page?
 
Last edited by a moderator:
Physics news on Phys.org
O yea, you have to partially differentiate one coordinate with respect to the other.
That's not in Griffiths!
I totally forgot.
Thanks.
That was driving me crazy.
That method was always a great mystery to me, because the professor just kind of told us to think about how it is correct 🤔.
What if we thought too much about it and it no longer makes any sense 🤔?
I was thinking about taking a partial derivative, but it didn't "click."
Griffths has a God awful method for converting coordinate differentials.
I suggest everyone not use that method.
He actually brings out the old ##\Delta x## thing and takes the limit.
Hideous.
 
Last edited:
Zap said:
That's not in Griffiths!
It's in most calculus textbooks ...
 
Zap said:
O yea, you have to partially differentiate one coordinate with respect to the other.
That's not in Griffiths!
I totally forgot.
Thanks.
That was driving me crazy.
That method was always a great mystery to me, because the professor just kind of told us to think about how it is correct 🤔.
What if we thought too much about it and it no longer makes any sense 🤔?
I was thinking about taking a partial derivative, but it didn't "click."
Griffths has a God awful method for converting coordinate differentials.
I suggest everyone not use that method.
He actually brings out the old ##\Delta x## thing and takes the limit.
Hideous.
You use the total derivatives dx,dy, etc. aka exterior derivative and then sub-in.
 
Actually, I'm still not getting it. The wiki page shows this:
{\displaystyle dV=dx\;dy\;dz=\det {\frac {\partial (x,y,z)}{\partial (r,\theta ,z)}}dr\;d\theta \;dz=r\;dr\;d\theta \;dz}
,
but it leaves a lot to the imagination.
I was thinking of changing coordinates, not differentials. When changing coordinates you can do the $$\hat x = \frac{ \frac{\partial y(x)}{\partial x} }{ |\frac{ \partial y(x)}{ \partial x } |}$$ thingy to find the unit vectors. I guess we are still changing coordinates, but to find the differentials, so maybe the method is similar.

I think someone messed with the OP, because it's not really legible anymore. I was just asking how to get from ##dxdy## to ##rdrd\theta##.
 
Zap said:
Actually, I'm still not getting it. The wiki page shows this:
{\displaystyle dV=dx\;dy\;dz=\det {\frac {\partial (x,y,z)}{\partial (r,\theta ,z)}}dr\;d\theta \;dz=r\;dr\;d\theta \;dz}
,
but it leaves a lot to the imagination.
I was thinking of changing coordinates, not differentials. When changing coordinates you can do the $$\hat x = \frac{ \frac{\partial y(x)}{\partial x} }{ |\frac{ \partial y(x)}{ \partial x } |}$$ thingy to find the unit vectors. I guess we are still changing coordinates, but to find the differentials, so maybe the method is similar.

I think someone messed with the OP, because it's not really legible anymore. I was just asking how to get from ##dxdy## to ##rdrd\theta##.
I guess that someone was you together with a software bug. The MathJax code sometimes gets lost if you mix it with BB-code like "center" in the edit mode. Anyway, the calculation goes:
\begin{align*}
x&=r \cos \varphi \; , \; y= r\sin \varphi \\ &\Longrightarrow \\
\det J &= \left| \dfrac{\partial (x,y)}{\partial (r,\varphi)} \right| = \left| \begin{bmatrix} \dfrac{\partial x}{\partial r} & \dfrac{\partial x}{\partial \varphi} \\ \dfrac{\partial y}{\partial r} & \dfrac{\partial y}{\partial \varphi} \end{bmatrix} \right| = \left| \begin{bmatrix} \cos \varphi & -r \sin \varphi \\ \sin \varphi & r \cos \varphi \end{bmatrix} \right| =r\cos^2 \varphi +r \sin^2 \varphi = r \\
&\Longrightarrow \\
dA&= dx \,dy = \left(\det J \right) \,dr \, d\varphi = r \,dr \,d\varphi
\end{align*}
 
Weird. One might think it is better just to memorize it.
I guess I'm confused on this part ##dxdy=(detJ)drdφ##.
I'm not really sure where the det J is coming from. This question has been asked a few times on google, so I will continue reading up on it, but I'm still not entirely getting it.
 
Zap said:
Weird. One might think it is better just to memorize it.
I guess I'm confused on this part ##dxdy=(detJ)drdφ##.
I'm not really sure where the det J is coming from. This question has been asked a few times on google, so I will continue reading up on it, but I'm still not entirely getting it.
Sort of properties of multilinear maps come down to, or simplify into, the DetJ statement.
 
  • Like
Likes   Reactions: Zap
  • #10
Why is ## dxdy = (cos\theta dr - rsin\theta d\theta)(rcos \theta d\theta + sin\theta dr) ## not allowed? Is it because ##dx## and ##dy## are actually vectors and we have to do some kind of vector product? Or is it allowed, but not very useful, since it produces weird stuff like ##(dr)^2##.
 
  • #11
Zap said:
I guess I'm confused on this part ##dxdy=(\det J)drd\varphi##.
Try to convert a basis ##\{\,(1,0),(1,4)\,\}## into ##\{\,(2,5),(-1,7)\,\}##. The functional determinant is the factor which adjusts the volumes. If you measure in inch instead of centimeters, you apply a scaling factor, too, don't you? Now what about square inch and square centimeters?
 
  • #12
Zap said:
Why is dxdy=(cosθdr−rsinθdθ)(rcosθdθ+sinθdr)dxdy=(cosθdr−rsinθdθ)(rcosθdθ+sinθdr) not allowed? Is it because dxdx and dydy are actually vectors and we have to do some kind of vector product? Or is it allowed, but not very useful, since it produces weird stuff like (dr)2(dr)2.
It is allowed. You just used the wrong multiplication. If you insist on differential forms, then we have
\begin{align*}
dx \wedge dy &= (\cos \varphi \,dr -r\sin \varphi \, d\varphi) \wedge (\sin \varphi \, dr + r \cos \varphi \, d\varphi)\\
&= (\cos \varphi )\,dr \wedge (r\cos \varphi \, d\varphi) - (r \sin \varphi \, d \varphi) \wedge (\sin \varphi \, dr)\\
&= r\cos^2 \varphi \,dr \wedge d \varphi - r\sin^2 \varphi \,d\varphi \wedge dr \\
&= (r\cos^2 \varphi + r\sin^2\varphi )\, dr \wedge d\varphi \\
&=r \,dr \wedge d\varphi
\end{align*}
 
  • #13
Zap said:
Why is ## dxdy = (cos\theta dr - rsin\theta d\theta)(rcos \theta d\theta + sin\theta dr) ## not allowed? Is it because ##dx## and ##dy## are actually vectors and we have to do some kind of vector product? Or is it allowed, but not very useful, since it produces weird stuff like ##(dr)^2##.
You can do it that way. There is an antisymmetric product so
drdr=0 dθdθ=0 drdθ=-dθdr

dxdy=rdrdθ

The determinant give the ratio of the differentials
 
  • #14
Wow. I always wished that physics could be taught by mathematicians.
There's a lot for me to digest here, but I am learning.
 
  • Like
Likes   Reactions: weirdoguy

Similar threads

  • · Replies 8 ·
Replies
8
Views
3K
  • · Replies 11 ·
Replies
11
Views
3K
  • · Replies 29 ·
Replies
29
Views
5K
  • · Replies 4 ·
Replies
4
Views
3K
  • · Replies 5 ·
Replies
5
Views
2K
  • · Replies 2 ·
Replies
2
Views
3K
  • · Replies 3 ·
Replies
3
Views
4K
  • · Replies 5 ·
Replies
5
Views
4K
  • · Replies 4 ·
Replies
4
Views
4K
  • · Replies 3 ·
Replies
3
Views
3K