Ferencz, Cs.

English

Periodica Polytechnica (Budapest University of Technology and Economics)

WAVE PROPAGATION IN INHOMOGENEOUS~ ANISOTROPIC, TIME-VARYING MEDIUM By CS. FERENCZ Department of Theoretical Electricity, Poly technical "Gniversity Budapest (Received ?lIay 31, 196B) Presented by Prof. Dr. K. SnlOXYI The necessity to investigate wave propagation III media characterized by general parameters arose as a consequence of space research, and the devel-opment of special, particularly microwave devices. As the original aim of thp research work 'was with respect to a possibility to treat the Doppler-effect more exactly - to investigate propagation in ionized, in time and space vary-ing, anisotropic media encountered in space research, the re5trictions used must be adjusted thereto. It is assumed that the space charge of the medium: ~. = 0, that is, it is electrically neutral. A solution for the Nlaxwell-equations of the following form: is sought for while the abrupt discontinuities must be excluded. that IS, 1 8Elli d --- ~ gra ;f!, 8x; 1 ~_l_ SEoi ...;;;:;. E --~l ;=1 0; 8t OJ -8t Discussing the assumption (2) reveals that if the solutions have the form of (1), these restrictions are not very severe. The effect of the energy exchange between the medium and the electro-magnetic wave was not taken into account, that is, the energy of the "gener-ator" governing the parameters of the medium, was considered as infinitely large. This is admissible so far the energy emitted or absorbed by the electro-magnetic wave is negligible, as compared to the energy content of the media, or if the energy exchange can be steadily compensated (e.g. by a pump-source). 348 CS. FERK"'iCZ 1. Solution hy using standard formalism Assume that the medium is characterized by the relative permittivity, '£(1', t) and the relative permeability ,ft(1', t), where E contains the conductivity in the well-known manner. The desired form of the solution is E = E 0(1', t) . • ej[wt-'P(r,t)] where the restrictions (2) are evaluable. Only such solutions are searched for. Maxwell's equations are: - a -rot H = -' (cv '8 E) at rotE = a _-a; (!-lo fi H) o (3) where Co and !-lo are the permittivity and permeability of the vacuum, respec-tively, r is the position vector, t is time, E and f1 are the rclative pcrmittivity and permeability of the medium, E is the electrical field, ii the magnetic field, w the radian frequency of the signal, cp the total phase, and ( 4) using D as electric flux density and jj as magnetic flux density. Introducing here the K = grad rp and at (5j (0* == (V symbols, the foIlo'wing equation system equivalent to (3) 111 e,-crv respect can he ohtained instead of Eqs (3): K X ii = - w* Co E E K >< E = (1)* .uoMH (6) where WAVE PROPAGATIO,'-. 1 a8 1=' =", 8-]----= ,eo w* at = = . 1 afl =, * ,'1 =,u-]-- --= 1 ,nL (1)* at 349 (7) The form of Eqs (6) is analogous with the wave equations for plane 'waves which propagate in homogeneous, stationary media, so let the common method be used: after multiplying repeatedly with K, one of the equations can be substitutcd into the other, and, therefore, it is possible to keep either if or fi only. The symbols used are: A=K>«Kx ... ) K? (=* ) ... = X e' ..• (8) ( /[ -L W*2 8 U 111) fi -L w* 8 P* if 0 -, 0, 0 , 0 (A -L (1)*2 8 11 c) it - 0 , 01""0'-- (9) The non-trivial solution of the homogeneous linear equation system (9) exists only if the determinant is equal to zero whereby dispersion equation well known in homogeneous case is obtained. This can be written in two advantageous equivalent forms. Let us use x 2 = w*2801.(0 for cancellation: XM )-1 o (10) or if' '=1 :-,X}l,\ x (A _)-1 _ [ - + x E lYI* I = 0 . x . ! (ll) These two equations give cp(r, t) resulting under propagation and, at the same time, the propagation path f and the connected time t, whereby E and fi satisfying the given boundary conditions and no'w existing necessarily can be obtained from Eqs (9). Eqs (10) or (11) contain the known cases of wave propagation - under the restrictions mentioned in the introduction (l) - and open the way for further general investigations. 350 cs. FERE.vCZ 2. Verification of the general applicability of the solution, the way of calculation 2.1. Propagation in wcuum Now € = ,11 t and Srp/8t = 0, as no parameters yary in time. The (10) or (ll) form of the dispersion equation is co~ cn,ill" I = 0 (12 ) where n is an arbitrary unit yector. The re:mlt is well known. 2.2. Homogeneous ferrite or plasma If the characteristic parameters are Ji = constant and I L in station-ary magnetic field the medium is ferrite, if E = constant and;fi = 1, the me-dium is plasma. In case of ferrite it is adyisahle to use (ll), in case of plasma rather (10). The resulting dispersion equations: III case of ferrite and III case of plasma (13) are also well known. 2.3. Stationary, isotropic, inhomogeneous medium Assume E = c(r) t ,Il = t and let the yariation in time he omitted. The new form of (10) is and after manipulation can he written. This is the hasic equation of the geometrical optics, the so-called Eikonal-equation, again well known: [~r -;- 1~!'2 8x . 1.8)" (14) The following method of calculation is well adaptahle in other inhomo-geneous cases as well, so let it he examined in detail. Let the common method of characteristics excluding the discontinuities be used. WA VE PROPAGATIO.Y Eq. (14) is of the following form: dF (8C! , 8x 8y 8; x, )', z) = 0 It is advisable to introduce here the parameter a instead of the length of arc, defined by the equation ds = /: (8(l) 2 + ( 8cp '1 2 -+-da 8x , . 8y. 8g: )2 8;:; . In this case the propagation path r = x(a)i -'- 'y(a)] z(a)k can be obtained and, among all the possibilities, the actual one can he selected by the houndary conditions. The total phase shift between t,,-o given point~ is G. g-12 = k~ r -s[7=( a)] da (15 ) and, with the upper limit of the integral made variable, the desired cp[r(a)] can be obtained. If, for instance, the Doppler-shift of an electromagnetic wave is to be determined, the transmitter and rcceiyer approach one another, that is, a1 = aI(t) and az = ait), and the Doppler-shift is dChz dt In solving an actual task, the integrals can be evaluated by computers. 2.4. Isotropic, inhomogeneous, quasi-stationary medium Assume that E = 1'(1', t) I, ,u I AS I and -- ~ E. In that case the (I) at actual form of (10) is: KZ (1)*2 So Po s(7=, t) (16) Using the method of characteristics, we get and t = tea), 352 CS. FERENCZ where the a parameter differs from the previous one, and 1 r sda + 112~[~-- k6 S ( PI (a) -1)]dada ,8t2 (J) (17) where pI(a) = 8rr/8t, and its value will be obtained as a result of the process. If it is assumed that the phenomena do not depend on time, (17) gives (15). 2.5. Stationary, anisotropic, inhomogeneous medium Let us have, for instance, s = s(T), /i = I and a stationary medium. So, if '8 is symmetric, we have the crystal optics, and if it is antisymmetric, the plasma. (If E = 1, fl = /l(T) it is possible to discuss inhomogeneous ferrites. etc. The results are formally equivalent to those represented here.) Eq. (10) can be written in the following form: (18) "\V-here A, B, C, D, F, G, J, L, 1\1 and R are given functions consisting only of the components of E. Suppose now that E is homogeneous and antisymmetric; this results in the well kno'wn dispersion equation of the homogeneous plasma, and (18) can be solved hy the method of characteristics. The discussion of the disper-sion equation gives information on the mode of propagation. Take lY = Kjk o, and let us introduce as ne'\\" variables the spherical coordinatcs, {j (the angle to the z-axis) and ep (that to the x-axis). Now (18) can he written in the following ne"w form: N4 + aN~ + b = 0, where a and b are functions of fj and cp in every point of the space. There is no propagation if N~ < 0 and real, hut if N~ > 0 and real, the propagation is ideal. In other cases there is an attenuated propagation. So the range (surface or surface-system) can be outlined in every point, along which an ideal propagation exists: the Fi(D, cp) as the solution of a 2 WA VE PROPAGATION and Fn(D, rp), along which there is no propagation, as the solution of 1 I a 1-i 2 (a 1.'ia)2 ) - 2 !, 12 - bJ 2.6. In-time fast varymg, isotropic medium Let us suppose that f = s(?, t)!, f1 = 1, then according to (10) [ ::r r ~)2 + (~)2 _ (~)2 S (~r 8y 8z , W , 8t 1 -- £oS - ] - - - - 0 S + ] - - = kg (n . 1 8S) 8q: k2 • kg as 0 w w at. at co at 353 (19) which determines cp. Since cp is complex, the ideal isotropic medium attenuates or amplifies (1) the signal. As the result is very interesting, let us briefly discuss the special results of (19) concerning in-space homogeneous media. The new form of Eq (19) is: I arp 12 = (arp 12 Sn/loS(t) ~ j ds(t) SuPo I, ax . at , dt at (20) In case of an ideal propagation Im = 0, and ax IS a modulated signal, or a static electrical field: a = const., b = const., may aTise. (J(Re rp) There is no propagation in the medium, if ---' r-, -- = O. A special case ox of this can be obtained if Re rp O. Then it is necessary, to have F= -1 4 const. 354 cs. FERESCZ Under the given restrictions (Re q = 0) only rJ= _.- 1 can occur. So Im q- = In 1 x -, ;-' = const. / ~ 1 1 - cos 2w \f ..l- t,,) and 2 (21 ) -- -~~--E 2E[)· ( \ 2 ). ej,nt --, cos 2(,) (t t,)) ; describes the phenomena in degenerated, ideal parametric amplifiers with distributed parameters. The magnetic parametric amplifiers can he in vesti-gated in a similar manner etc. It can he seen that (10) or (11) contains the hitherto well known re~ults of which several were represented here. Solving the prohlem under other suitahle conditions may result in completely ncw phenomena. 3. Relativistic formalism The introduction of T = jet does not involve any theoretical noyelty; as its only consequence, our equations are considerahly simplified by using the natural coordinates of Maxwell's equations. under the assumptions macle at the beginning, E Eo' ej<P [n applying the symbols K--aq: :. I - ---- ] ax ay J aW,aT ==E 8z 1 aE ] :x aT = . ail/aT = . 1 all .\t = ,U - ] aw/aT = ,u --- ] :x aT :x= aT (2.3) and keeping the other symhols in accordance ·wit h tlH~ir meaning, Eqs (10) and (11) will remain im:ariahly valid. IrATE PROPAGATIO.\ 355 Then, for instance, the dispersion equatiun of tIlt' ta;,;k III 2.4. can bp written as grad~ cp = eraCP)~ , aT c = 1 i. e which is better arranged and more advantageous for calculation, etc. A further task of generalization is to find a treatment 'whereby the abrupt discontinuities may be reckoned 'within the same general manner. Acknowledgement is due to Prof. Dr. K. Simouyi and Dr. A. Csurgay for their valuable assistance in this 'work. . ~ . Summary The paper wants to find a general way for the discussion of waye propagation in inhomo-geneous. anisotropic. time varying media. The abrupt discontinuities will be excluded from the discu;;sion. that is, "plane-wave" solution is sought for. After the general solntion of the probll'l11. the paper suggests a calculation method. and the different well-known wave propa-gation equations (e.g. the Eikonal-equation) are "hown to result from the general solution as special cases. Finally, the method of the relatiyistic rewriting is presented. References 1. SDI02"YI. K.: Foundations of Electrical Engineering. Pergamon Press, 1963 . . ) B"CDDE2". K. G.: Radio "'ayes in the Ionosl;here. C;mbridge l'niyersity Press,1966. 3. BOR2", ::\I. '\\'OLF, E.: Principles of Optics. Pergamon Press. 1959, .J.. SDIO::wr. K.: Elektronfizika. Tankonyykiad6. 1965. Dr. Csaba FERE::\CZ, Budapest XI., Egri J6zsef u. 18, Hungary 

WAVE PROPAGATION IN INHOMOGENEOUS, ANISOTROPIC, TIME-VARYING MEDIUM

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WAVE PROPAGATION IN INHOMOGENEOUS, ANISOTROPIC, TIME-VARYING MEDIUM

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