Verify about the solution of wave equation of potential.

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Discussion Overview

The discussion revolves around the wave equation related to a point charge at the origin, specifically examining the conditions under which the potential V satisfies a homogeneous equation, and exploring solutions for time-harmonic waves. The scope includes theoretical aspects of wave equations, mathematical reasoning, and potential solutions in the context of electromagnetic theory.

Discussion Character

  • Technical explanation
  • Mathematical reasoning
  • Debate/contested

Main Points Raised

  • Alan questions why the wave equation excludes the origin, suggesting it may be due to the singularity at R=0.
  • Some participants agree with Alan's reasoning regarding the exclusion of the origin.
  • Alan presents a follow-up question about finding solutions for a time-harmonic wave, proposing a transformation of variables to simplify the wave equation.
  • Alan derives a solution for U(R,t) as a function of R and t, indicating that for potential reaching infinity, the second term in the solution disappears.
  • Other participants suggest that the periodic solution can be derived directly from the wave equation without substituting δ initially.
  • Discussion includes the necessity of a plus sign before ω² in the equation for periodic solutions, with some participants emphasizing the importance of defining parameters correctly for lossy and lossless media.
  • Alan reflects on the distinction between using δ for lossy media and k for lossless media, indicating a deeper understanding of the topic.

Areas of Agreement / Disagreement

Participants generally agree on the mathematical transformations and the implications of the wave equation, but there are differing views on the handling of parameters and the nature of solutions in lossy versus lossless media. The discussion remains unresolved regarding the optimal approach to defining solutions.

Contextual Notes

Limitations include potential assumptions about the nature of the medium (lossy vs. lossless) and the implications of singularities at the origin. The discussion does not resolve the mathematical steps or definitions used in the context of the wave equation.

yungman
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I read in the book regarding a point charge at the origin where [itex]Q(t)= \rho_{(t)}Δv'\;[/itex]. The wave eq is.

[tex]\nabla^2V-\mu\epsilon\frac{\partial^2 V}{\partial t^2}= -\frac {\rho_v}{\epsilon}[/tex]

For point charge at origin, spherical coordinates are used where:

[tex]\nabla^2V=\frac 1 {R^2}\frac {\partial}{\partial R}\left( R^2 \frac {\partial V}{\partial R}\right)[/tex]

This is because point charge at origin, [itex]\frac {\partial}{\partial \theta} \hbox{ and }\; \frac {\partial}{\partial \phi}[/itex] are all zero.

My question is this:

The book then said EXCEPT AT THE ORIGIN, V satisfies the following homogeneous equation:

[tex]\frac 1 {R^2}\frac {\partial}{\partial R}\left( R^2 \frac {\partial V}{\partial R}\right)-\mu\epsilon \frac {\partial^2 V}{\partial t^2}=0[/tex]

The only reason I can think of why this equation has to exclude origin is because R=0 and origin and this won't work. Am I correct or there's another reason?

Thanks

Alan
 
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Yep, you're right. Nothing complicated here.
 
Thanks

Alan
 
I have another question follow up with the original wave equation:

[tex]\frac 1 {R^2}\frac {\partial}{\partial R}\left( R^2 \frac {\partial V}{\partial R}\right)-\mu\epsilon \frac {\partial^2 V}{\partial t^2}=0[/tex]

According to the book, to simplify this equation, Let:

[tex]V_{(R,t)}=\frac 1 R U_{(R,t)}[/tex]

This will reduce the wave equation to:

[tex]\frac {\partial^2U_{(R,t)}}{\partial R^2}-\mu\epsilon\frac {\partial^2U_{(R,t)}}{\partial t^2}=0[/tex]

One of the solution is [itex]U_{(R,t)}=f\left(t-\frac R {\mu\epsilon}\right)[/itex]

My question is I want to find the solution if U(R,t) is time harmonic which is a continuous sine wave. The book does not show the anything. So I am using the regular solution of time harmonic wave equation and using direction to be [itex]\hat R[/itex]. So the formula become:

[tex]\frac {\partial^2U_{(R,t)}}{\partial R^2}-\mu\epsilon\frac {\partial^2U_{(R,t)}}{\partial t^2}= \frac {\partial^2U_{(R,t)}}{\partial R^2}+\omega^2\mu\epsilon U= 0.[/tex]
[tex]δ^2=-\omega^2\mu\epsilon\;\Rightarrow\; \frac {\partial^2U_{(R,t)}}{\partial R^2}-δ^2 U= 0.[/tex]

This is a 2nd order ODE with constant coef and the solution is:

[tex]U_{(R,t)}= V_0^+ e^{-δ R}+V_0^- e^{δ R}[/tex]

For potential that reach to infinity space, there will be no reflection so the second term disappeared, whereby:

[tex]U_{(R,t)}= V_0^+ e^{-δ R}[/tex]

Do I get this right? This might look very obvious, but I am working on retarded potential and I am interpreting what the book don't say, I have to be careful to make sure I get everything right.

Thanks

Alan
 
Last edited:
[itex]\frac {\partial^2U_{(R,t)}}{\partial R^2}-\mu\epsilon\frac {\partial^2U_{(R,t)}}{\partial t^2}= \frac {\partial^2U_{(R,t)}}{\partial R^2}+\omega^2\mu\epsilon U= 0.[/itex]
just from the last in it you can write the periodic solution.Don't substitute any δ after.
 
andrien said:
[itex]\frac {\partial^2U_{(R,t)}}{\partial R^2}-\mu\epsilon\frac {\partial^2U_{(R,t)}}{\partial t^2}= \frac {\partial^2U_{(R,t)}}{\partial R^2}+\omega^2\mu\epsilon U= 0.[/itex]
just from the last in it you can write the periodic solution.Don't substitute any δ after.

Thanks for the reply, I just finished updating the last post, please take a look again. The reason I use δ is because this will be used in phasor form which is going to be in form of:

[tex]U_{(R,t)}= V_0^+ e^{\alpha R} e^{j\beta R}\; \hbox { where } δ=\alpha + j\beta[/tex]
 
a plus sign before ω2 in eqn is necessary for periodic solution.First write solution in terms of ω and then introduce other definitions.
 
andrien said:
a plus sign before ω2 in eqn is necessary for periodic solution.First write solution in terms of ω and then introduce other definitions.

This is because for lossy dielectric medium ε=ε'+jε'' therefore [itex]δ=j\omega \sqrt{\mu(ε'+jε'')}[/itex] is a complex number where [itex]δ=\alpha + j \beta[/itex]. Solution of:

[tex]\frac {\partial ^2 U}{\partial R^2} -δ^2U=0 \hbox { is }\; U_{(R,t)}= U_0^+ e^{-δR}\;=\; U_0^+ e^{-\alpha R} e^{-j\beta R}[/tex]

This is a decay periodic function.

For lossless, we use [itex]k=\omega\sqrt{\mu\epsilon}\hbox { where ε is real.}[/itex]

Then

[tex]\frac {\partial ^2 U}{\partial R^2} +k^2U=0 \hbox { is }\; U_{(R,t)}= U_0^+ e^{-jkR}[/tex]

Actually because you brought this up, I dig deep into this and answer the question why the books use δ for lossy media and k for lossless media. I never quite get this all these years until now.
 
Last edited:
that is why it is better to go with + sign.but it is ok,now.In case,ε is complex it is still possible to define things after.But you already got it.
 
  • #10
Thanks.
 

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