Lecture 23 Oblique Incidence and Reflection

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    EECS 117

    Lecture 23: Oblique Incidence and Reflection

    Prof. Niknejad

    University of California, Berkeley

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    Review of TEM Waves

    We found that E(z) = xEi0ejz is a solution to

    Maxwells eq. But clearly this wave should propagate inany direction and the physics should not change. We

    need a more general formulation.

    Consdier the following plane wave

    E(x,y,z) = E0e

    jxx

    jyy

    jzz

    This function also satisfies Maxwells wave eq. In thetime-harmonic case, this is the Helmholtz eq.

    2E + k2E = 0where k =

    =

    c

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    Conditions Imposed by Helmholtz

    Each component of the vector must satisfy the scalarHelmholtz eq.

    2Ex + k

    2Ex = 02

    x2+

    2

    y2+

    2

    z2

    Ex + k

    2Ex = 0

    Carrying out the simple derivatives

    2x 2y 2z + k2 = 0

    2x + 2y + 2z = k2

    Define k = xx + yy + zz as the propagation vector

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    Propagation Vector

    The propagation vector can be written as a scalar timesa unit vector

    k = kan

    The magnitude k is given by k = As well show, the vector direction an defines thedirection of propagation for the plane wave

    Using the defined relations, we now have

    E(r) = E0ejkr

    x = k x = kan xy = k

    y = kan

    y

    z = k z = kan zUniversit of California Berkele EECS 117 Lecture 23 . 4/

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    Wavefront

    wav

    efront

    plane

    r

    k

    Recall that a wavefront is a surface of constant phasefor the wave

    Then an R = constant defines the surface of constantphase. But this surface does indeed define a planesurface. Thus we have a plane wave. Is it TEM?

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    E is a Normal Wave

    Since our wave propagations in a source free region, E = 0. Or

    E0 e

    jkanr = 0ejkanr

    =

    x

    x+ y

    y+ z

    z

    ej(xx+yy+zz)

    = j(xx + yy + zz)ej(xx+yy+zz)

    So we have

    jk(E0 an)ejkanr

    = 0This implies that an E0 = 0, or that the wave ispolarized transverse to the direction of propagation

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    H is also a Normal Wave

    Since H(r) = 1j

    E, we can calculate the directionof the H field

    Recall that (fF) = f F +f FH(r) =

    1

    jejkr

    E0

    H(r) =1

    jE0

    jkejkr

    H(r) = k

    an E(r) = 1an E(r)

    = k

    =

    = /Universit of California Berkele EECS 117 Lecture 23 . 7/

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    TEM Waves

    So we have done it. We proved that the equations

    E(r) = E0ejkr

    H(r) =1

    an E(r)

    describe plane waves where E is perpendicular to thedirection of propagation and the vector H isperpendicular to both the direction of propagation andthe vector E

    These are the simplest general wave solutions toMaxwells equations.

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    Wave Polarization

    Now we can be more explicit when we say that a waveis linearly polarized. We simply mean that the vector Elies along a line. But what if we take the superposition

    of two linearly polarized waves with a 90

    time lag

    E(z) = xE1(z) + yE2(z)

    The first wave is x-polarized and the second wave isy-polarized. The wave propagates in the z direction

    In the time-harmonic domain, a phase lag corresponds

    to multiplication by jE(z) = xE10e

    jz jyE20ejz

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    Elliptical Polarization

    In time domain, the waveform is described by thefollowing equation

    E(z, t) = E(z)ejtE(z, t) = xE10 cos(t z) + yE20 sin(t z)

    At a paricular point in space, say z = 0, we have

    E(0, t) = xE10 cos(t) + yE20 sin(t)

    Thus the wave rotates along an elliptical path in thephase front!

    We can thus create waves that rotate in one direction or

    the other by simply adding two linearly polarized waveswith the right phase

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    Perpendicular Polarization

    Let the angle of incidence and relfection we given by iand r. Let the boundary consists of a perfect conductor

    Ei = yEi0ejk1r

    where k1 = k1ani and ani = x sin i + z cos i

    Ei = yEi0e

    jk1(x sin i+z cos i)

    Hi =1

    ian Ei

    For the reflected wave, similarly, we haveanr = x sin r z cos r so that

    Er = yEr0ejk1(x sin rz cos r)

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    Conductive Boundary Condition

    The conductor enforces the zero tangential fieldboundary condition. Since all of E is tangential in thiscase, at z = 0 we have

    E1(x, 0) = Ei(x, 0) + Er(x, 0) = 0

    Substituting the relations we have

    yEi0e

    jk1x sin i + Er0ejk1x sin r

    = 0

    For this equation to hold for any value of x and , thefollowing conditions must hold

    Er0 = Ei0 i = rUniversit of California Berkele EECS 117 Lecture 23 . 13/

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    Snells Law

    We have found that the angle of incidence is equal tothe angle of reflection (Snells law)

    The total field, therefore, takes on an interesting form.The reflected wave is simply

    Er = yEi0ejk1(x sin iz cos i)

    Hr =1

    1anr Er

    Hr = Ei01(x cos i z sin i)ejk1(x sin iz cos i)

    The total field is thus

    E1 = Ei + Er = yEi0ejk1z cos i ejk1z cos i ejk1x sin i

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    The Total Field

    Simplifying the expression for the total field

    E1 = y2jEi0 sin(k1z cos i) standing waveejk1x sin i

    prop. wave

    H1 = 2Ei0

    1 ( x cos i cos(k1z cos i)ejk1x sin i

    +

    z j sin i sin(k1z cos i)ejk1x sin i )

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    I Ob i

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    Important Observations

    In the z-direction, E1y and H1x maintain standing wave

    patterns (no average power propagates since Eand Hare 90 out of phase. This matches our previous

    calculation for normal incidenceWaves propagate in the x-direction with velocityvx = /(k1 sin i)

    Wave propagation in the x-direction is a non-uniformplane wave since its amplitude varies with z

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    TE Waves

    Notice that on plane surfaces where E = 0, we are freeto place a conducting plane at that location withoutchanging the fields outside of the region

    In particular, notice that E = 0 when

    sin(k1z cos i) = 0

    k1z cos i =2

    1z cos i = m

    This holds for m = 1, 2, . . .

    So if we place a plane conductor at z = m12cos i , therewill be a guided wave traveling between the twoplanes in the x direction

    Since E1x = 0, this wave is a TE wave as H1x = 0Universit of California Berkele EECS 117 Lecture 23 . 17/

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    P ll l P l i ti (II)

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    Parallel Polarization (II)

    Now consider an incident electric field that is in theplane of polarization

    Ei = Ei0(x cos i z sin i)ejkr

    Hi = yEi01

    ejkr

    Likewise, the reflected wave is expressed as

    Er = Er0(x cos i + z sin i)ejkr

    Hr = yEr01

    ejkr

    Note that ki,r r = x sin i,r z cos i,r

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    T ti l B d C diti

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    Tangential Boundary Conditions

    Since the sum of the reflected and incident wave musthave zero tangential component at the interface

    Ei0 cos iejk1x sin i

    + Er0 cos rejk1x sin r

    = 0

    These equations must hold for all . Thus Er0 = Ei0 asbefore

    Thus we see that these equations can hold for allvalues of x if and only if i = r

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    The Total Field (Again)

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    The Total Field (Again)

    Using similar arguments as before, when we sum thefields to obtain the total field, we can observe astanding wave in the z direction and wave propagation

    in the x direction.Note that the magnetic field H = Hy is alwaysperpendicular to the direction of propagation but the

    electric field has a component in the x direction.This type of wave is known as a TM wave, ortransverse magnetic wave

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