Can't find potential of vector field

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The discussion revolves around the challenges of finding the potential of a vector field in curvilinear coordinates. Participants express frustration over the apparent contradiction between their calculations and the assertion that no potential exists due to a non-zero curl. They emphasize the importance of correctly applying the gradient in curvilinear coordinates and suggest that coordinate transformations may be necessary for clarity. The conversation highlights the need for a deeper understanding of derivative operators in different coordinate systems, as well as the potential limitations of the textbook being used. Ultimately, the consensus is that a proper approach requires careful integration and consideration of the coordinate system's properties.
Addez123
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Homework Statement
There's two exercises where I'm suppose to find if there's a potential and if so determine it.
$$1. A = 3r^2sin v e_r + r^3cosv e_v$$
$$2. A = 3r^2 sin v e_r + r^2 cos v e_v$$
Relevant Equations
None
1. To find the solution simply integrate the e_r section by dr.
$$\nabla g = A$$
$$g = \int 3r^2sin v dr = r^3sinv + f(v)$$
Then integrate the e_v section similarly:
$$g = \int r^3cosv dv = r^3sinv + f(r)$$

From these we can see that ##g = r^3sinv + C##
But the answer is apparently that there is no solution since ∇ × A does not equal zero.
Wtf? Take the derivative of ##r^3sinv## with respect to r and v and you'll literally get A!
So how does it "not exist"?

Same problem with number 2.
$$g = \int 3r^2 sin v dr = r^3 sin v + f(v)$$
$$g = \int r^2 cos v dv = r^2 sin v + f(r)$$
From this you can CLEARLY see there is NO solution available.
Yet this exercise has the audacity to claim that
$$g = r^3 cos v$$
would be a solution!
Have they even tried taking the derivative of that with respect to literally ANYTHING?!
##d/dr (r^3 cos v) = 3r^2 COS v##, which is not ##A_r##.

Are they trying to make me go mad??
 
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Orodruin said:
That's not how the gradient works in curvilinear coordinates.
My textbook does not cover potentials except in cartesian coordinates.

What's wrong with my approach?
I need to add a jacobian somewhere or something?
 
In plane polars, <br /> \nabla g = \frac{\partial g}{\partial r} e_r + \frac 1r \frac{\partial g}{\partial v} e_v.
 
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Addez123 said:
My textbook does not cover potentials except in cartesian coordinates.

What's wrong with my approach?
I need to add a jacobian somewhere or something?
You would need to convert r, ##e_r##, v, and ##e_v## to Cartesian coordinates. It's technically possible but it's going to be a real mess.

The concepts are identical if you use polar coordinates and it will give you some good experience to work it that way. Coordinate transformations are a good technique to learn when solving these types of problems, and many others.

-Dan
 
Ahh ok I get it!
So when solving for ##e_v## in 1.
I should have done
$$g = \int r^3cosv * 1/r dv = r^2sinv + f(r)$$
which then has no solution.
Is that correct?
 
Addez123 said:
My textbook does not cover potentials except in cartesian coordinates.
But does it cover the derivative operators in curvilinear coordinates? That should be enough since the potential concept in itself is not coordinate dependent.

Edit: … and if it doesn’t, then consider another textbook that does (nudge, nudge, wink, wink) 😁
 
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Addez123 said:
Ahh ok I get it!
So when solving for ##e_v## in 1.
I should have done
$$g = \int r^3cosv * 1/r dv = r^2sinv + f(r)$$
which then has no solution.
Is that correct?

No, you have <br /> \begin{split}<br /> \frac{\partial g}{\partial r} &amp;= A_r \\<br /> \frac 1r \frac{\partial g}{\partial v} &amp;= A_v \end{split} so if g exists then <br /> \int A_r\,dr + B(v) = \int rA_v\,dv + C(r).
 
pasmith said:
No, you have <br /> \begin{split}<br /> \frac{\partial g}{\partial r} &amp;= A_r \\<br /> \frac 1r \frac{\partial g}{\partial v} &amp;= A_v \end{split} so if g exists then <br /> \int A_r\,dr + B(v) = \int rA_v\,dv + C(r).
I would write it slightly differently. If a potential ##\phi## exists, then
$$
\phi = \int^{\vec x} \vec A\cdot d\vec x.
$$
This is coordinate independent. In polar coordinates however
$$
d\vec x = \vec e_r dr + \vec e_v r \, dv
$$
and so
$$
\phi = \int^{\vec x} (A_r dr + rA_v dv).
$$
Integrate along any curve to find the result.

The result is of course the same.
 
  • #10
Don't we need the condition ## U_x=V_y## , in Cartesian , as a necessary condition?
 
  • #11
First calculate the curl (I'd extend it to 3D to use the standard formulae for cylinder coordinates ;-)). If the curl doesn't vanish there's no scalar potential. Otherwise, I'd use the hint in #8.
 

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