Phil Lucht Math & Physics Archive
Home / Math and Physics Files / Physics / Transmission Lines / Notes By Chapter and Appendix / Appendix B MagJ

new Section B.6 REVIEWED

DOCX · 78.7 KB
Open DOCX file

Draft section of Appendix B dated 1.16.14, written by Phil. It explains why the Helmholtz integral for Az needs a homogeneous addition when μ1 ≠ μ2, and states the Jm Theorem: adding only the surface magnetization current to the conduction current satisfies the boundary conditions. The proof uses Stakgold's single-layer boundary results, including the extra ∓a/2 term in the normal derivative, and 2D propagators in the transmission line limit. The text shown ends partway through the proof.

AI-written summary; may contain errors.

Extracted text (machine-read; may contain errors)
New Section B.6 PhL 1.16.14 Section B.6 Modification of King's Helmholtz integral solution when μ1 ≠ μ2 1 (a) General Discussion 1 Comments regarding μ 1 (b) Statement and Proof of the Jm Theorem 2 Section B.6 Modification of King's Helmholtz integral solution when μ1 ≠ μ2 (a) General Discussion In Section 4.7 we wrote the vector potential for transmission line conductor C in this manner, Az(x,ω) = ∫ μ2 Jzc(x',y',z',ω)dx'dy'dz' . R = |x - x'| (4.7.2) where we have made a notational change to be consistent with previous sections of Appendix B. Here we shall use μ2 to refer to the permeability of the conductor, and μ1 to be that of the dielectric (these are called μ1 and μ in Section 4). The above "Helmholtz integral" is only the "particular solution" of the Helmholtz equation (2 + β12)Az= -μ2Jcz. When μ1 ≠ μ2, it turns out that one must add a homogeneous solution Az(homo) [ that is, (2 + β12) Az(homo) = 0] to the Helmholtz solution shown above in order to meet boundary conditions. Appendix M.4 provides a very detailed study of just how this works for a round conductor with a uniform current distribution. To avoid this massive complication, we limited the analysis of Chapter 4 to the case that μ1 = μ2. This means, for example, that Chapters 4,5,6 are only applicable for non-magnetic conductors in air. With the reader's permission, we replicate the following comments from below (4.7.6), making a few small changes: Comments regarding μ This is a subtle subject and is not discussed in King's transmission line theory book. If the dielectric and conductor have the same permeability so that μ1 = μ2, then there exists no "magnetic boundary" between the conductor and dielectric. The solution (4.7.2) is then smooth at this boundary, and so Az(x,y,z) "naturally" satisfies these two boundary conditions, Az(x+) = Az(x-) (1/μ1)∂nAz(x+) = (1/μ2) ∂nAz(x-) (4.7.7) (B.6.0) where x+ is just outside the conductor surface and x- is just inside. The second equation here is just (1.1.46) in the case that there is no free surface current Kfree flowing on the boundary, and indeed in our example at hand there is no such free surface current. Since we have assumed that μ1 = μ2, this second boundary condition just says ∂nAz(x+) = ∂nAz(x-). Since there is no magnetic boundary at the conductor/dielectric interface, the solution (4.7.2) is continuous and all its derivatives are also continuous at the boundary, since nothing special happens at that boundary. Thus, the Helmholtz integral solution provides the whole solution for Az since it automatically meets both "boundary conditions" at this pseudo boundary. If on the other hand we have μ1 ≠ μ2, then there is a magnetic boundary between conductor and dielectric which we have to worry about. In this case, (4.7.2) cannot possibly satisfy the second boundary condition of (B.6.0) since, as already noted, the Az of (4.7.2) satisfies ∂nAz(x+) = ∂nAz(x+). Thus, in this case (4.7.2) is not the full solution for Az. One must add a homogeneous Helmholtz equation solution to (4.7.2) in order to have a proper solution for Az that satisfies both equations in (B.6.0). It turns out that the correct total Az solution can be generated by adding a certain fictitious surface current to Jz in (4.7.6). Since such a surface current vanishes on both sides of the boundary between μ1 and μ2, the Helmholtz solution due just to this surface current is in fact a homogeneous solution to the Helmholtz equation in both the conductor and dielectric regions, away from that boundary. It turns out moreover that the correct fictitious surface current to add is in fact the magnetization surface current Jm which is created at the boundary between μ1 ≠ μ2. Adding this surface current is just a "trick" in order to generate the correct homogeneous adder solution so that the resulting total Az satisfies both boundary conditions in (B.6.0). Formally speaking, the J appearing in (1.5.3) and then Jz in (4.7.2) should not include such magnetization currents since this J is really the J in Maxwell's equation curl H = ∂tD + J, and this J does not include magnetization currents -- it includes only normal conduction currents. Here we wish to prove the claim that adding the surface magnetization current (only!) to the conduction current does in fact make the boundary conditions work. After doing this proof, we will show in Section B.7 just how this works out in the case of a round conductor. We stress that only the surface part of Jm gets added in. In general Jm will also have a "bulk" component in the dielectric and conductor. If we were to include this bulk component, we would not be adding a homogeneous solution to the particular solution, and we would in fact be creating a non-solution! In (M.3.4) we show the complete Jm for a round wire carrying a uniform current, and it does have both bulk and surface components. (b) Statement and Proof of the Jm Theorem The Jm Theorem. If Jmz represents the surface component of magnetization current density for a transmission line conductor of μ2 with conduction current density Jcz , embedded in a dielectric medium of μ1, then if we write Az(x) = ∫ [μ2 Jcz(x') + μ0 Jmz(x')] dV' . R = |x - x'| (B.6.1) we obtain the full solution which meets boundary conditions (B.6.0) shown above. Comment: Our proof below really applies in the "transmission line limit" of Sections 4.3 and 4.9 which is essentially a long wavelength and small β limit. In this limit, we can replace our various Helmholtz propagators below with Laplace propagators. Nevertheless, we maintain the Helmholtz forms in the hope that the above theorem is valid for reasonably moderate (but not huge) β values. At very large β values the whole transmission line framework collapses anyway, transverse Ax and Ay components are no longer small, and the line picks up transverse waveguide activity. (1) Preliminaries. We first quote a key result from Stakgold concerning boundary layer a: u(x) = ∫σ dSξ a(ξ) E(x|ξ) u(s) = ∫σ dSξ a(ξ) E(s|ξ) (B.6.2) ∂νu(x) = ∫σ dSξ a(ξ) ∂νE(x|ξ) ∂νu(s) = [∂nu(x)]x→s± = ∫σ dSξ a(ξ) ∂νE(x|ξ) ∓ a(s)/2 // extra term ! (B.6.3) This is a tricky subject and some words are certainly in order. In the Stakgold world, σ is a surface of n-1 dimensions existing in an n dimensional space. E(x|ξ) is the free-space propagator in that n dimensional space (the "fundamental solution"). The integrals shown above are over the surface σ, and ξ represents the n-1 dimensional coordinate of a point on the surface σ, while dSξ is a piece of "area" on the surface. (Stakgold does not write vectors in bold font as we do in this document.) Function a(ξ) is defined on the surface and is called a simple or monopole layer. Stakgold also deals with dipole layers (as in a cell membrane), but we don't care about them right now. The question at hand is this: What happens as a point x away from the surface approaches the surface where it becomes point s? We are interested in the limit x → s. As shown in the first pair of equations, nothing unusual happens for the function u(x) defined as shown by the integral. One then says that u(x) is "continuous" at x = s. But something very unusual happens for the function ∂νu(x) where ∂ν denotes a derivative locally normal to the surface at s. As x → s an "extra term" appears as shown above having value ∓a(s)/2. If normal ν points "out" from the surface then as one approaches from the outside (call it the + side), the extra term is -a(s)/2, but if the approach is from the inside (- side), the extra term changes sign. Here is a picture illustrating the geometry of the above equations: ( n is normal at ξ , ν is normal at s) Fig B.5 The reason the extra term appears has to do with the nature of the dξ integration when ξ is very close to s which is somewhat of a singular situation since R ≡ |s-ξ| → 0. Stakgold treats surface layers in Section 6.4 of his Volume II, pages 110-120, and his treatment involves a lot of detail. The claims shown above appear on pages 118 and 119, though the conclusions are a bit obscured in the detail. Stakgold works in 3D with E(x|ξ) = (1/4π|x-ξ|) = 1/4πR and often uses these quantities, k(s,ξ) = cos(s ξ, )/ [4π|s-ξ|2] // cos(upper marked angle) k(ξ,s) = cos(ξ s, )/[4π|s-ξ|2] = ∂νE(s|ξ) . // cos(lower marked angle) Later in his Problem 6.18 through 6.20 Stakgold has the reader verify that the results are also valid in 2D where surface σ is then just a curve. These are the results we shall use. Although he does not state it outright, we think his results are probably valid for σ being a surface of any number of dimensions, but our only interest will be the 2D case. (2) Outline of Proof We break up (B.6.1) into these two terms: Az(c)(x) = ∫ [μ2 Jcz(x')] dV' . R = |x - x'| (B.6.4) Az(m)(x) = ∫ [μ0 Jmz(x')] dV' . R = |x - x'| (B.6.5) Az(x) = Az(c)(x) + Az(m)(x) two terms (B.6.6) As noted earlier, the first term is smooth at a point s on a conductor surface and satisfies the two boundary conditions, Az(c)(s+) = Az(c)(s-) ∂nAz(c)(s+) = ∂nAz(c)(s-) . (B.6.7) For this term, which is the Helmholtz "particular" integral, we may then calculate, ∂nAz(c)(s+) – ∂nAz(c)(s-) = + [- ] ∂nAz(c)(s) . (B.6.8) Since this is non-zero, the term Az(c) on its own does not meet the required slope boundary condition at an interface between μ1 and μ2, and that is precisely why we need the Az(m) term. Our goal is to show that ∂nAz(m)(s+) – ∂nAz(m)(s-) = – [ - ] ∂nAz(m)(s) . (B.6.9) so that when we add the two terms we will get ∂nAz(s+) – ∂nAz(s-) = 0 (B.6.10) as required by (1.1.46). The concludes our proof outline, and it remains then to demonstrate (B.6.9). (3) Verification of (B.6.9) We start with (B.6.5) where ∫dV' is over the entire transmission line conductor C, Az(m)(x) = ∫ dV' [μ0 Jmz(x')] = ∫ dV' [μ0 Jmz(x') E3(x|x') (B.6.11) where E3(x|x') = → as β→0 . (B.6.12) We know from Appendix C and elsewhere in this document that in the transmission line limit we can do the dz' integration in dV' and arrive at a 2D-propagator expression for the above potential, where the integral is now over the cross section area of the conductor C, Az(m)(x) =∫ dA' [μ0 Jmz(x')] E2(x|x') (B.6.13) where E2(x|x') = (j/4) H0(1)(kR) → - ln(R2) β→0 . (B.6.14) We are only using that portion of Jmz which is a surface current on the perimeter of C, so we rewrite the above as Az(m)(x) = C ds' [μ0 Kz(x')] E2(x|x') (B.6.15) where Kz(x') is the magnetization surface current (amps/m) discussed in Section B.1. Stakgold's surface integral over σ is now just a line integral around the perimeter of the conductor C cross section. Recall from (B.1.10) that the magnetization surface current is given by, Kz = - ( - ) Hθ (B.1.10) where Hθ is the H field tangent to the cross section surface. Inserting this Kz into (B.6.15) gives Az(m)(x) = C ds' [(μ1-μ2) Hθ(x')] E2(x|x') . (B.6.16) We now identify this with the first of Stakgold's equations (B.6.2) and we know we can take x→s with no surprises. If we now replace Stakgold's normal direction ν with our usual normal symbol n, we can write (B.6.3) as ∂nAz(m)(x) = C ds' [(μ1-μ2) Hθ(x')] ∂nE2(x|x') (B.6.17) ∂nAz(m)(s±) = C ds' [(μ1-μ2) Hθ(x')] ∂nE2(s|x') ∓ [(μ1-μ2) Hθ(s)]/2 (B.6.18) Now since we want to prove (B.6.9), we first evaluate its left hand side using (B.6.18) twice, ∂nAz(m)(s+) – ∂nAz(m)(s-) = { C ds' [(μ1-μ2) Hθ(x')] ∂nE2(s|x') - [(μ1-μ2) Hθ(s)]/2 } – { C ds' [(μ1-μ2) Hθ(x')] ∂nE2(s|x') + [(μ1-μ2) Hθ(s)]/2 } = (μ1-μ2) [- ] C ds' Hθ(x') ∂nE2(s|x') – [+ ] (μ1-μ2) Hθ(s)/2 . Our task of showing that (B.6.9) is true then boils down to showing that the following equation is true: (μ1-μ2) [- ] C ds' Hθ(x') ∂nE2(s|x') – [+ ] (μ1-μ2) Hθ(s)/2 = – [- ] ∂nAz(c)(s) ? A question mark indicates an equation that we want to show is true, but have not yet done so. Cancelling (μ1-μ2) factors the equation in question becomes [- ] C ds' Hθ(x') ∂nE2(s|x') – [+ ] Hθ(s)/2 = + ∂nAz(c)(s) ? or (μ2-μ1) C ds' Hθ(x') ∂nE2(s|x') – (1/2)(μ2+ μ1) Hθ(s) = ∂nAz(c)(s ) ? (B.6.19) The integral can be replaced using (B.6.18) with the s+ choice, ∂nAz(m)(s+) = C ds' [(μ1-μ2) Hθ(x')] ∂nE2(s|x') - (1/2)[(μ1-μ2) Hθ(s) so (μ1-μ2) C ds' Hθ(x') ∂nE2(s|x') = ∂nAz(m)(s+) + (1/2) (μ1-μ2) Hθ(s) . (B.6.20) Our equation of interest (B.6.19) is then – ∂nAz(m)(s+) – (1/2)(μ1-μ2) Hθ(s) – (1/2)(μ2+ μ1) Hθ(s) = ∂nAz(c)(s) ? or – ∂nAz(m)(s+) – μ1 Hθ(s) = ∂nAz(c)(s) ? or – μ1 Hθ(s) = ∂nAz(c)(s) + ∂nAz(m)(s+) ? or – μ1 Hθ(s+) = ∂nAz(s+) ? // using (B.6.6) (B.6.21) We now introduce a local cylindrical coordinate system in this manner relative to point s Fig B.6 Notice that is the normal vector at point s, so ∂r = ∂n. Then first we determine Bθ, B = curl A = [ r-1∂θAz - ∂zAθ] + [∂zAr - ∂rAz] + [ r-1∂r(rAθ) - r-1∂θAr ] = [ r-1∂θAz] + [- ∂rAz] = [- ∂rAz] . Here we have set ∂θAz = 0 according to Fact 7 of (3.8.11) which says Az is constant on the cross section surface. The result is then, Bθ(s+) = - ∂nAz(s+) . (B.6.22) Since s+ is in the dielectric with μ1 we then have Hθ(s+) = (1/μ1) Bθ(s+) = - (1/μ1) ∂rAz(s+) so -μ1 Hθ(s+) = ∂rAz(s+) (B.6.23) But this last equation matches our equation in question (B.6.21), so we can then go back and erase all the question marks and we have then verified equation (B.6.9) and our proof is complete. Comment: We noted that Stakgold's analysis is quite complicated. He uses the Laplace free-space propagators such as E2(x|x') = -(1/2π) ln(R2), but we think his analysis also applies for the Helmholtz propagators. The reason is that the Helmholtz complication does not really change the singular nature of things near R = 0. This is most obvious when comparing e-jβR/4πR to 1/4πR. If we are wrong about this conjecture, we can regard the above theorem as proven only for small β which in fact is the transmission line limit.