Uniform Plane Waves in Lossless Media UCF Phasor Form Representation u ( z, t ) u ( z, t ) u ( z, t ) A cos( t kz A ) B cos( t kz B ) Re (Ae j A e jkz e j t ) Re( Be j B e jkz e j t ) U Ae j A e jkz U 0 e jkz (propagating in +z direction) U Be j B e jkz U 0 e jkz (propagating in -z direction) 0, 0 x y z Uniform Plane Wave (UPW) UCF Definition: For all the points in the plane which is perpendicular to the direction of propagation, the electric and magnetic fields are the same (or uniform). For an electromagnetic UPW propagating in +z direction, we have E E 0 e jkz H H 0 e jkz If the wave is propagating in +direction, we replace z by . E E 0 e jk H H 0 e jk a or a k k k r a ( k a ) r k r r 0 r a Define k ka ka k as wave vector. In the following write a as a k . Del Operator in UPW Solution UCF For UPW solution: E E 0 e j k r H H 0 e j k r k r ( k x a x k y a y k z a z ) ( xa x ya y z a z ) kx x k y y kz z jk r j(kx xk y ykz z) (e ) [e ] jk x e jk r x x This means that we can replace / x by jk x . Likewise, we can replace / y by jk y and / z by jk z . Since ax ay az z x y jk x a x jk y a y jk z a z jk Lossless UPW Equations UCF In lossless, isotropic, source free media E jωH H j ω E jk jk E jωH jk H jωE E 0 jk E 0 H 0 jk H 0 k E ωH k H ω E k E 0 k H 0 UCF (1) Properties of UPW in Lossless Isotropic Media (1) k E 0 k E k H 0 k H This means that there is no electromagnetic field components in the direction of propagation. We can define the direction of propagation as longitudinal direction and the directions that are perpendicular to the direction of propagation as transverse directions. For a wave, when there is no longitudinal electric and magnetic field components or all the field components are in the transverse directions, it is called “transverse electromagnetic” (TEM) wave. The UPW in lossless, isotropic media is a TEM wave. Properties of UPW in Lossless Isotropic Media (2) UCF E k E ωH k H ω E (2) EH H k E, H and k form a right handed system. (3) k k E ω k H ω ( ω )E ω 2 E k k E k ( k E ) E (k k ) k 2 E k E ω E 2 2 ω or k ω vp k ω dispersion relationship 2 2 UCF (4) Properties of UPW in Lossless Isotropic Media (3) ω k E ωH a k E H k Since k is real in lossless media, E and H have the same phase. (5) E ω ω H k ω 0 Define 0 as wave impedance. 1 H a k E, r r 377 r r E ak H UCF Average Power Density of UPW 1 S av Re( E H * ) 2 For UPW in lossless, isotropic media k E k E ωH H ω 1 k E * S av Re[ E ( ) ] 2 1 Re[ 2 E 2 2 2 k E E* (k E) or ak H 2 2 ak ] Example 1 UCF An electric field of UPW in free space is given as z E 800 cos(108 t ky)a z V/m Find : (a) k , (b) , (c)H at point (0.1,1.5,0.4) m and t 8 ns. Solution : E 800e jky a z V/m x propagation direction : a y , electric field direction : a z , magnetic field direction : a x , 108 rad/s. 108 (a) k 0.333 rad/m 8 c 3 10 2 2 (b) 18.84 m 0.333 k 800 jky 800 jky e ax e a x 2.12 e jky a x V/m (c) H 0 377 H ( x, y, z , t ) 2.12 cos(108 t ky)a x H (0.1, 1.5, 0.4, 8ns) 2.12 cos(108 8 10 9 0.333 1.5)a x 2.03a x V/m y Example 2 UCF The EM fields of UPW in lossless,isotropic and uniform dielectricare given as E 500 cos(107 t kz)a x V/m, H 1.1cos(107 t kz)a y A/m, v p 0.5c Find : (a) r , (b) r , (c)k , (d) , and (e). z Solution : propagation direction : a z , electricfield direction : a x , magneticfield direction : a y , 107 rad/s. 500 454.54 , 0 r / r 377 r / r 1.1 r / r 454.54 / 377 r / r 1.455 (1) v p c / r r 0.5c x r r 2 r r 4 (2) From (1) and (2), we have r 2.41 and r 1.66. 107 2 2 0.0667 rad/m, 94.2 m k 8 v p 0.5c 0.5 3 10 k 0.0667 y Example 3 (1) UCF The electric fields of UPW in lossless,isotropic and uniform dielectricis given as z E (5a y j10a z )e j 2 x V/m, f 50 MHz, r 1 Find : (a) k , (b) , (c)v p , (d) r , (e) , and (f) H at origin (0,0,0) and t / 2. Solution : x (a) k 2 rad/m, propagation direction is a x , k 2a x rad/m (b) 2f 2 50 106 3.14 108 rad/s (c) k vp 3.14 108 rad/s vp 1.57 108 m/s k 2 rad/m 2 2 c 1 c 1 3 108 m/s 3.65 (d) v p r 8 r v p 1 1.57 10 m/s r r (e) 0 r 1 377 197 r 3.65 y Example 3 (2) UCF z (f) E (5a y )e j 2 x ( j10a z )e j 2 x V/m H 5 (a z )e j 2 x j10 a y e j 2 x A/m 5 10 H Re[He jt ] cos(t 2 x)a z at origin (0,0,0) and t sin(t 2 x)a y 2 5 10 cos( 2 0 ) sin( a 2 0)a y z t 2 2 2 H (0,0,0) | 10 a y 0.051a y . x y