Electric Field and Dielectric: Displacement Field

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    Displacement Field
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Discussion Overview

The discussion revolves around the relationship between the electric field (E), displacement field (D), and polarization (P) in dielectric materials, particularly focusing on the physical meaning of the permittivity of free space (ε₀) and the applicability of the displacement field equation in different contexts, including dynamic electric fields and specific materials like water.

Discussion Character

  • Technical explanation
  • Conceptual clarification
  • Debate/contested
  • Experimental/applied

Main Points Raised

  • One participant questions the physical meaning of the term ε₀E in the displacement field equation and its scaling effect on the applied electric field E.
  • Another participant explains that ε₀ is necessary for unit consistency and mentions that alternative definitions of the displacement field could be used without changing the underlying physics.
  • A third participant notes that the original equation is a restricted form applicable to linear, non-moving materials and presents various equivalent forms of the constitutive relation.
  • A participant expresses concern about applying the equation to dynamic electric fields in water and seeks guidance on extending the equation to more general cases.
  • Another participant responds that sinusoidal fields are fundamental and states that the original constitutive relation is valid for water under certain conditions, but suggests a more general nonlinear relation may be needed for high frequencies or large amplitudes.

Areas of Agreement / Disagreement

Participants generally agree on the basic formulation of the displacement field but express differing views on its applicability under various conditions, particularly regarding dynamic fields and specific materials. The discussion remains unresolved regarding the best approach for non-linear or dynamic cases.

Contextual Notes

Limitations include the assumption of linearity and isotropy in the original equation, as well as the potential need for a nonlinear constitutive relation in dynamic scenarios. The discussion does not resolve the complexities introduced by high-frequency fields or material movement.

Apteronotus
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Hi,

Suppose we apply an electric field E to a dielectric material. It is my understanding that the actual field that is formed as a result of our applied field is given by the displacement field D.

D=[tex]\epsilon_{0}[/tex]E+P

I know that the field P is due to the polarization of the atoms withing the dielectric.

1. what is the physical meaning behind [tex]\epsilon_{0}[/tex]E?
2. Specifically, why is the contribution of our applied field E being scaled by the permittivity of free space [tex]\epsilon_{0}[/tex]?

Thanks in advance.
 
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The [itex]\epsilon_0[/itex] is there to make the units work out correctly. The polarization field is measured in coulombs per meter squared (perpendicular to the vector, just as current density is measured). The D field uses the same units as P.

This is just a convention; one could just as easily define

[tex]\vec D_{new} = \vec E + \frac 1{\epsilon_0} \vec P[/tex]

and you could work out the same equations, only with different constants. In fact, in some systems of units, [itex]\epsilon_0 \equiv 1[/itex], so this question becomes moot.
 
What you wrote is a highly restricted form of a constitutive relation- you wrote it for a linear material which is not moving.

There's lots of equivalent ways to write what you wrote (D = [itex]\epsilon[/itex]E = [itex]\epsilon_{r}\epsilon_{0}[/itex]E = (1+4[itex]\pi\chi[/itex])[itex]\epsilon_{0}[/itex]E =...)

The idea is that the displacement field in regions of matter is composed of the "matter-free" field and an additional contribution from the matter.
 
Fantastic! Thank you both very much.

On a related item...

I now that the equation is valid only for Linear, Homogenous Isotropic materials.
The material that I'm concerned with is water (which I believe to be isotropic --Encyclopedia Britannica).
And my applied electric field is dynamic (sinusoidal).

Off the top of your heads... is there a great leap between the equation
[tex] \vec D = \epsilon_0 \vec E + \vec P[/tex]
and one which would apply in my case?

Could you direct me to any resources where the above equation is given for a more general case (ie. not so restrictive)?
 
Sinusoidal fields are about as basic as they come, and application of the field to a material is independent of the material response to the field.

For water, your constitutive relation is fine, as long as the frequency of oscillation doesn't go to high and the field amplitude isn't too large. In those cases, you need a more general, nonlinear, constitutive relation:

D ~ aE +bE^2 +cE^3+...

If it's moving, there's components from the magnetization that also figure in.
 

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