ELECTROMAGNETICS AND APPLICATIONS

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    ELECTROMAGNETICS AND APPLICATIONS

    Lecture 2

    Electromagnetic Waves

    in Homogenous Media

    Luca Daniel

    L2-2

    Course Overview and Motivations

    Maxwell Equations (review from 8.02)

    in integral form

    in differential form

    EM waves in homogenous lossless media

    EM Wave Equation

    Solution of the EM Wave equation

    Uniform Plane Waves (UPW)

    Complex Notation (phasors)

    Wave polarizations

    EM Waves in homogeneous lossy media

    Todays Outline

    TodayToday

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    L2-3

    Second derivative in space second derivative in time,therefore solution is any function with identical dependencies

    on space and time (up to a constant)

    Maxwells Equationsin l inear isotropic homogeneous lossless media

    0

    0Faradays Law: = BE t

    Amperes Law:

    = D = D E

    GausssLaw

    = +D

    H Jt

    =B 0 = B H

    =

    22

    2EM Wave Equation : E E 0

    t

    ConstitutiveRelations

    ( )E(z, t) E t a z= + z

    E(z, t ) E t

    =

    or

    L2-4

    What are Electromagnetic Waves

    A wave is a fixed disturbance propagating through a medium

    Medium A B A energy B energy

    String stretch velocity potential kineticAcoustic pressure velocity potential kineticOcean height velocity potential kineticElectromagnetic E H electric magnetic

    0

    A,B energy density

    z

    z

    null

    A

    B

    0

    A,B

    wave motion

    zA(z, t ) A t

    =

    zB(z, t ) B t

    =

    zvelocity c

    t

    = =

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    L2-5

    Solutions of the Wave Equation

    Possible solutions are many Try Uniform Plane Wave (UPW),e.g. assume:

    0

    2 2 22

    2 2 2E E

    x y z

    = + +

    0

    propagationt = t

    t = 0

    z

    E+(t z/)

    z=vt0

    ( , )yy E z t=

    =

    2 2y y

    2 2

    E E

    z t

    = y

    zy E t

    1 =

    In air/vacuum waves moves at velocity

    81 3 10 [ / ]

    = = = = o o

    zc m s

    t

    ( , , , ) ( , )=E x y z t E z t1)

    2)

    3)

    2

    2Ez=

    =

    22

    2E E 0

    t

    =

    2 2y y

    2 2 2

    E E1

    z t

    L2-6

    Sinusoidal Uniform Plane Wave (UPW) in +z direction

    Ey(z,t) = E+(t - z/v) [V/m]

    One special solution:

    = =

    k

    To find the magnetic field:

    Faradays Law: = HEt

    General solution:

    0 0= = E cos[ (t z / )] E cos( t kz)

    where

    0

    0

    0

    0

    x y z

    x y z

    E det x y z

    E E E

    = 0xkE sin( t kz)=

    0

    =

    kH x E cos( t kz)

    H E

    E H in +z direction

    = E / HNote:

    = = = o

    oo

    377

    ( )0x E cos t kz z

    =

    0=

    Ex cos( t kz)

    In air/vacuum

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    L2-7

    Uniform Plane Wave: EM fields

    EM Wave in z direction:

    ( ) ( ) ( ) ( ) ( )0 0 oE z,t y E cos t kz , H z,t x E cos t kz = =

    y

    z

    x

    ( )E z,0

    ( )H z,0

    = = =

    2 2k f

    Wavelength

    L2-8

    Complex Notation (Phasors)

    { }= tE(r,t) Re E(r ) eComplex notation for a single frequency (f = /2)

    oE(z,t) yE cos( t kz )= + =

    Phasor : contains all amplitude, vector,

    spatial and phase information

    UPW case

    { }= tRe E(z) e

    oE(y,t) zE sin( t ky)=

    Phasor E Time domain EExample:

    { } = jky j to( Re zjE e e )

    jkyoE(r ) zjE e =

    { }jkz j toRe yE e e e

    = jkzoE(z) yE e e

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    L2-9

    Uniform Plane Wave (UPW) in Complex Notation

    = oE xE cos( t kz)

    = =

    8

    o o

    1c 3x10 m/ s

    Example : x-polarized UPW traveling in +z direction

    ==

    jkz

    o

    jkzo

    E(z) xE eE

    H(z) y e

    E H : z direction of propagation

    y

    z

    ( )H z,0

    ( )E z,0

    x

    =

    2

    kwavelength

    direction of propagation

    =c

    f

    = = = =

    o

    o0

    2(rads / s) 2 f k(rads /m)

    c

    =

    oEH y cos( t kz)

    L2-10

    Uniform Plane Wave (UPW)

    Linear vs. Circular vs. Elliptical Polarization

    y

    z

    ( )E z,0

    x

    Image source: http://en.wikipedia.org

    Linear Polarization

    Linear Polarization Circular Polarization