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  • 7/23/2019 notes 15 3317

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    Prof. David R. Jackson

    Notes 15Notes 15Plane WavesPlane Waves

    ECE 3317

    [Chapter 3]

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    Introduction to Plane Waves

    A plane wave is the siplest sol!tion to "a#well$s e%!ations for a wave that

    travels thro!&h free space.

    'he wave does not re%!ires an( cond!ctors ) it e#ists in free space.

    A plane wave is a &ood odel for radiation fro an antenna* if we are far

    eno!&h awa( fro the antenna.

    x

    z

    E

    H

    S

    S E H=

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    http+,,www.ipression-.or&,solarener&(,isc,espectr!.htl

    The Electromagnetic Spectrum

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    Source Frequency Wavelength

    US !" Po#er $% &' 5%%% (m

    E)F Su*marine"ommunications 5%% &' $%% (m

    !+ radio ,-T.&/ 0% (&' %5 m

    T2 ch 3 ,2&F/ $% +&' 5 m

    F+ radio ,Sunny 441/ 441 +&' m

    T2 ch 6 ,2&F/ 16% +&' 10 m

    T2 ch 4 ,U&F/ $3% +&' 6 cm

    "ell phone ,P"S/ 65% +&' 5 cm

    "ell Phone ,P"S 14%%/ 145 7&' 15 cm

    -#ave oven 35 7&' 13 cm

    Police radar ,89*and/ 1%5 7&' 365 cm

    mm #ave 1%% 7&' mm

    )ight 51%1

    :&'; %$% m89ray 1%16 :&'; otational chan&e+

    >ote+ for a lossless transission line* we have+ LC = =

    A transission line filled with a dielectric aterial has the sae waven!?er asdoes a plane wave travelin& thro!&h the sae aterial.

    Plane Wave Field ,cont/

    A wave travels with the sae velocit( on a transission line

    as it does in space* provided the aterial is the sae.

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    'he Hfield is fo!nd fro+

    so

    E Hj =

    $ ( )( )

    $

    $

    1H E

    E1

    1( ) E

    x

    x

    x

    x zj

    d

    yj dz

    jk yj

    =

    =

    =

    E =

    E E Ex y z

    x y z

    x y z

    0E ( ) jkz

    x z E e=

    Plane Wave Field ,cont/

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    Intrinsic Impedance

    or

    /ence

    $H Exk

    y

    =

    E

    H

    x

    y k

    = = =

    where

    = 8ntrinsic ipedance of the edi!

    H Ey xk

    =

    00

    0

    376.730313 [ ]

    = = B0reespace+

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    Poynting 2ector

    'he cople# Po(ntin& vector is &iven ?(+

    0

    0

    E

    1H

    jkz

    jkz

    x E e

    y E e

    =

    =

    ( )*1

    S E H2

    =

    /ence we have

    ( )

    ( ) ( )

    *

    00

    *

    0 0

    2

    0

    1S

    2

    1

    2

    1

    2

    jkz jkz

    jkz jkz

    Ez E e e

    z E e E e

    z E

    =

    =

    =

    2

    0 2S [VA/m ]

    2

    Ez

    =

    ( ) ( )2

    0 2= Re S [W/m ]2

    ES t z

    =

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    Phase 2elocity

    ( )

    0

    0 0

    E

    cos

    jkz

    x

    x

    E e

    E E t kz

    =

    = +

    pv

    k

    = =

    1p d

    v c

    = =

    0ro o!r previo!s disc!ssion on phase velocit( for transission lines* we know that

    /ence we have

    5speed of li&ht in the dielectric aterial6

    pv

    =

    so

    0

    0 0

    jE E e

    =

    >ote+ all plane wave travel at the sae speed in a lossless edi!*

    re&ardless of the fre%!enc(. 'his iplies that there is no dispersion* which

    in t!rn iplies that there is no distortion of the si&nal.

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    Wavelength

    2 2

    k

    = =

    2 2 2 1

    2

    dc

    k ff f

    = = = = =

    dc

    f=

    0ro o!r previo!s disc!ssion on wavelen&th for transission lines* we know that

    /ence

    Also* we can write

    0

    0

    2

    k

    =0ree space+

    0ree space+ 0c

    f =

    ( )

    0

    0 0

    E

    cos

    jkz

    x

    x

    E e

    E E t kz

    =

    = +

    0

    0 0

    jE E e

    =

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    Summary ,)ossless "ase/

    0

    0

    2

    0

    E

    1H

    S2

    jkz

    x

    jkz

    y

    z

    E e

    E e

    E

    =

    =

    =

    y

    z

    x E

    H

    S

    ( )0 0cosxE E t kz = +

    00 0

    jE E e =

    ( )Re E j tx xE e

    =

    'ie doain+

    Denote

    1pvk

    = =

    2

    k

    =

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    )ossy +edium

    E HH J E

    jj

    = = +

    J E=

    Ret!rn to "a#well$s e%!ations+

    Ass!e Bh$s law+

    ( )

    H E E

    E

    j

    j

    = +

    = +

    Apere$s law

    e define an effective 5cople#6 perittivit( cthat acco!nts for cond!ctivit(+

    cj j = + c j

    =

    z

    xE

    ocean

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    )ossy +edium

    E HH Ec

    jj

    = =

    "a#well$s e%!ations+ then ?ecoe+

    'he for is e#actl( the sae as we had for the lossless case* with

    c

    /ence we have

    0

    0

    E

    1H

    jkz

    x

    jkz

    y

    E e

    E e

    =

    =

    !ck k jk = =

    j

    c

    e

    = =

    5cople#6

    5cople#6

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    )ossy +edium ,cont/

    E#aine the waven!?er+

    !k k jk =

    !

    0 0

    jkz jk z k z

    xE E e E e e

    = =

    c k

    ck = c j

    =

    0

    0

    k

    k

    Denote+

    8n order to ens!re deca(* the waven!?er k!st ?e in the fo!rth %!adrant.

    /ence+ k

    k

    Copare with loss( '+

    ) + di , /

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    )ossy +edium ,cont/

    !

    0

    jk z k z

    xE E e e =

    z

    0

    k z

    E e

    2

    k

    =

    ) + di , t /

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    )ossy +edium ,cont/

    !

    0

    jk z k z

    xE E e e =

    1 / !pd k=

    'he depth of penetration dpis defined.

    !

    k ze

    z

    xE 1

    1 0.37e B

    pd

    ) + di , t /

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    )ossy +edium ,cont/

    2 2

    0 0* 2 ! 2 !

    *1S E H2 2 2

    k z j k z

    x yE Ez z e z e e

    = = =$ $ $

    !

    0

    !

    01

    jk z k z

    x

    jk z k z

    y

    E E e e

    H E e e

    =

    =

    'he cople# Po(ntin& vector is+

    j

    c

    e

    = =

    ( )

    2

    0 2 !ReS cos2k zz z

    ES t e

    = = 2 !k ze

    z

    Sz1

    1 / !p

    d k=

    2 0.1"e =

    E l

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    E=ample

    Bcean water+

    0

    #1

    " [S/m]

    r

    =

    ==

    Ass!efF 2.: G/4

    0

    0

    c rj j

    = =

    ( )( )0 #1 3$.%$ [&/m]c j =

    0 0 0c rck = = ( )3#6.022 #1.#16 [1/m]k j=

    1/pd k= 0.013 [m]pd =

    2 /k = 0.016 [m]=

    5'hese val!es are fairl( constant !p thro!&hicrowave fre%!encies.6

    E l , t /

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    E=ample ,cont/

    f dp [m]

    1 [/4] 2-1.

    1: [/4] 7=.

    1:: [/4] 2-.2

    1 [k/4] 7.=1: [k/4] 2.-2

    1:: [k/4] :.7=

    1 ["/4] :.22

    1: ["/4] :.:9:

    1:: ["/4] :.:22

    1.: [G/4] :.:131:.: [G/4] :.:12

    1:: [G/4] :.:12

    'he depth of penetration into the ocean water is shown for vario!s fre%!encies.

    ) T t

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    )oss Tangent

    c j

    =

    Denote+ c c cj =

    'he loss tan&ent is defined as+ 'a( c

    c

    =

    e then have+ 'a(

    =

    'he loss tan&ent characteri4es the nat!re of the aterial+

    'a HH 1+ lowloss edi! 5atten!ation is sall over a wavelen&th6'a II 1+ hi&hloss edi! 5atten!ation is lar&e over a wavelen&th6

    ( ) ( )2 / 2 /k k k k ke e e

    = =>ote+

    ) ) )i it

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    ( )

    0 0

    0

    0

    1

    1 'a

    ck j

    j

    j

    = =

    =

    =

    )o#9)oss )imit

    ( )( )0 1 'a / 2k j owloss liit+ 1 1 / 2 1( )z z z+ +

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    Polari'ation )oss

    'he perittivit( can also ?e cople#* d!e to olec!lar and atoic polari4ationloss5friction at the olec!lar and atoic levels6 .

    c j

    =

    j =

    ( )c j j

    =

    c j

    = +

    E#aple+ distilled water+ 0 5?!t heats !p well in a icrowave oven6.

    'a

    = + or

    >ote+ 8n practice* it is !s!all( diffic!lt to deterine how !ch of the loss

    tan&ent coes fro cond!ctivit( and how !ch coes fro polari4ation loss.

    P l i ti ) , t /

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    Polari'ation )oss ,cont/

    c j

    = +

    ( )1 'ac j =

    0 r =

    Re&ardless of where the loss coes fro* 5cond!ctivit( or polari4ation loss6* we

    can write

    where

    1c

    j

    = +

    or

    >ote+ 8f there is no polari4ation loss* then r r =

    Polari'ation )oss ,cont /

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    Polari'ation )oss ,cont/

    0or odelin& p!rposes* we can l!p all of the losses into an

    effective cond!ctivit(ter+

    eff

    c j

    =

    c j

    = +

    0 r =where