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5 Wave Propagation

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    STANLEY L. AQUINOInstructor, ECE

    ELECTRONIC W VE PROP G TIO

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    In Earths atmosphere, ray wavefron

    propagation may be altered from freespace behavior by optical effects such

    Refraction (Bending)

    Reflection (Bouncing)Diffraction (Scattering)

    Interference (Colliding)

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    Optical properties can be analyzed

    completely by application of Maxwellequation, this is necessarily complex.

    For most applications, geometric raytracing can be substituted for analysis

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    Refraction is sometimes referred to a

    bending of the radio-wave path. How

    the ray does not actually bend.

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    Electromagnetic refraction is actuallychanging of direction of an electroma

    ray as it passes obliquely from one me

    into another with different velocities

    propagation.

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    Refraction of electromagnetic waves c

    expressed in terms of the refractive in

    of the atmosphere. Refractive index is

    square root of the dielectric constant

    =

    =

    = refractive index

    = equivalent dielectric constant relative

    = number of electrons per cubic centim

    = frequency (kHz)

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    Whenever a ray passesfrom a less de

    a more dense medium, it is effectively

    toward the normal.

    The normal is simply an imaginary line d

    perpendicular to the interface at the poincidence.

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    Conversely, whenever a ray passesfro

    more dense to a less dense medium, i

    effectively bent away from the norma

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    The angle of incidence is the angle fo

    between the incident wave and the n

    The angle of refraction is the angle fo

    between the refracted wave and thenormal.

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    The refractive index (index of refracti

    the two materials is simply the ratio ovelocity of propagation of a light ray i

    space to the velocity of propagation o

    light ray in a given material. =

    = refractive ind = speed of ligh

    = speed of ligh

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    How an electromagnetic wave reacts w

    it meets the interface of two transmis

    materials that have different indexes o

    refraction can be explained with Snell

    =

    =

    1 = refractiv

    2 = refractiv

    1 = angle of

    2 = angle of

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    and because the refractive index of a

    material is equal to the square root o

    dielectric constant,

    =

    1 = dielectric co

    2 = dielectric co

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    Refraction also occurs when a wavefrpropagates in a medium that has a de

    gradient that is perpendicular to the

    direction of propagation (i.e., parallel

    wavefront).

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    Reflect means to cast or turn back, an

    reflection is the act of reflecting.

    Electromagnetic reflection occurs wh

    incident wave strikes a boundary of tw

    media and some or all of the incidentpower does not enter the second mat

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    The angle of reflection is equal to the

    of incidence = .

    However, the reflected voltage field

    intensity is less than the incident voltintensity.

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    The ratio of the reflected to the incidevoltage intensities is called the reflect

    coefficient, (sometimes called the

    coefficient of reflection).

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    For a perfect conductor, = . is u

    indicate both the relative amplitude oincident and reflected fields and the p

    shift that occurs at the point of reflec

    =

    =

    () = reflect = incide

    = reflec

    = incide

    = reflec

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    The portion of the total incident power t

    not reflected is called the power transm

    coefficient (or simply the transmissicoefficient)

    For a perfect conductor, = . The law

    conservation of energy states that for aperfect reflective surface, the total reflec

    power must equal the total incident pow

    + =

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    If medium 2 is not a perfect conducto

    some of the incident waves penetrateand are absorbed.

    The fraction of power that penetratesmedium 2 is called the absorption

    coefficient.

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    Reflection also occurs when the reflecsurface is irregular or rough; howeve

    a surface may destroy the shape of th

    wavefront.

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    When an incident wavefront strikes a

    irregular surface, it is randomly scattemany directions. Such condition is cal

    diffuse reflection, whereas reflection

    a perfectly smooth surface is calledspecular (mirrorlike) reflection.

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    Surfaces that fall between smooth anirregular are called semirough surface Semirough surfaces cause a combination of diffus

    specular reflection. A semirough surface will not t

    destroy the shape of the reflected wavefront. Howthere is a reduction in the total power.

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    The Rayleigh criterion states that a

    semirough surface will reflect as if it w

    smooth surface whenever the cosine angle of incidence is greater than /8

    where d is the depth of the surface

    irregularity and is the wavelength ofincident wave.

    >

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    Diffraction is defined as the modulatiredistribution of energy within a wave

    when it passes near the edge of an op

    object.

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    When a wavefront passes near an obs

    or discontinuity with dimensionscomparable in size to a wavelength, s

    geometric analysis cannot be used to

    explain the results, and Huygens prin

    (which is deduced from Maxwells

    equation) is necessary.

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    Huygens principle states that every p

    on a given spherical wavefront can beconsidered as a secondary point sour

    electromagnetic waves from which ot

    secondary waves (wavelets) are radiaoutward.

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    Diffraction occurs around the edge ofobstacle, which allows secondary wav

    sneak around the corner of the obs

    into what is called the shadow zone.

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    Refraction, reflection and diffraction a

    categorized as a geometric optics.

    Interference, on the other hand, is su

    to the principle of linear superpositioelectromagnetic waves.

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    If the difference in distance travelled

    odd integral multiple of one-half

    wavelength, reinforcement takes plac

    If the difference is an even integral m

    of one-half wavelength, total cancella

    occurs.

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