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    Review ofReview ofVector AnalysisVector Analysis

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    Review of Vector Analysis

    Vector analysis is a mathematical tool with whichelectromagnetic (EM) concepts are most conveniently

    expressed and best comprehended.

    A quantity is called a scalar if it has only magnitude (e.g.,

    mass, temperature, electric potential, population).

    A quantity is called a vector if it has both magnitude and

    direction (e.g., velocity, force, electric field intensity).

    The magnitude of a vector is a scalar written as A or

    AA

    A

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    A unit vector along is defined as a vector whose

    magnitude is unity (that is,1) and its direction is along

    A

    A

    A

    AeA !!

    )(A

    1!

    Thus

    Ae

    which completely specifies in terms ofA and itsdirection Ae

    A

    AeAA !

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    A vector in Cartesian (or rectangular) coordinates may

    be represented as

    or

    where AX, Ay, and AZ are called the components of in the

    x, y, and z directions, respectively; , , and are unitvectors in the x, y and z directions, respectively.

    zzyyxx eAeAeA )A,A,A( zyx

    A

    A

    Review of Vector AnalysisReview of Vector Analysis

    xe

    ze

    ye

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    Suppose a certain

    vector is given by

    The magnitude orabsolute value ofthe vector is

    (from the Pythagorean theorem)

    zyx e4e3e2V !V

    385.5432V 222 !!

    V

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    The Radius Vector

    A point P in Cartesian coordinates may be represented by

    specifying (x, y, z). The radius vector (or position vector) of

    point P is defined as the directed distance from the origin O

    to P; that is,

    The unit vector in the direction ofr is

    zyx ezeyexr !

    r

    r

    zyx

    ezeyexe zyxr !

    !

    222

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    Vector Algebra

    Two vectors and can be added together to give

    another vector ; that is ,

    Vectors are added by adding their individual components.

    Thus, if and

    A B

    C

    BAC !

    zzyyxx eAeAeA zzyyxx eBeBeBB !

    zzzyyyxxx e)BA(e)BA(e)BA(C !

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    Parallelogram Head torule tail rule

    Vector subtraction is similarly carried out as

    zzzyyyxxx e)BA(e)BA(e)BA(D

    )B(ABAD

    !

    !!

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    The three basic laws of algebra obeyed by any given vector

    A, B, and C, are summarized as follows:

    Law Addition Multiplication

    Commutative

    Associative

    istributive

    where k and l are scalars

    ABBA !

    C)BA()CB(A !

    AA !

    A)l()Al(!

    BkAk)BA(k !

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    When two vectors and are multiplied, the result is

    either a scalar or a vector depending on how they are

    multiplied. There are two types of vector multiplication:

    1. Scalar (or dot) product:

    2.Vector (or cross) product:

    The dot product of the two vectors and is defined

    geometrically as the product of the magnitude of and the

    projection of onto (or vice versa):

    where is the smaller angle between and

    A

    ABcosABBA

    U!

    BA

    B

    ABU

    A

    BA v

    A B

    B

    B

    A B

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    If and then

    which is obtained by multiplying and component by

    component

    ),A,A,A(A ZYX! )B,B,B(B ZYX!

    ZZYYXX BABABABA !

    A B

    ABBA !

    CABACBA ! )(

    A A ! A2

    !A2

    eX ex ! ey ey ! eZ ez !1

    e ey ! ey ez ! e ex ! 0

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    The cross product of two vectors and is defined as

    where is a unit vector normal to the plane containing

    and . The direction of is determined using the right-

    hand rule or the right-handed screw rule.

    A

    A

    nABesinABBA U!

    B

    B

    e

    ne

    BA

    irection ofand using(a) right-hand rule,(b) right-handed

    screw rule

    ne

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    If and then

    zyx

    zyx

    zyx

    BBBAAA

    eee

    BA !

    ),A,A,A(AZYX

    ! )B,B,B(BZYX

    !

    zxyyxyzxxzxyzzy e)BABA(e)BABA(e)BABA( !

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    Note that the cross product has the following basic

    properties:

    (i) It is not commutative:

    It is anticommutative:

    (ii) It is not associative:

    (iii) It is distributive:

    (iv)

    ABB

    A v{v

    ABBA v!v

    )BA()B(A vv{vv

    CABACBA vv!v )(

    0AA ! )0(sin !U

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    Also note that

    which are obtained in cyclic permutation and illustrated

    below.

    yxz

    xzy

    zyx

    eeeeee

    eee

    !!

    !

    Cross product using cyclic permutation: (a) moving clockwise leads to positive results;

    (b) moving counterclockwise leads to negative results

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    Line Integrals

    A line integral of a vector field can be calculated whenever a

    path has been specified through the field.

    The line integral of the field along the path P is defined asV

    U!2

    1

    P

    PPdlcosVdlV

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    For segment P3,

    dl!dxex (the differentiallengthdl pointsto the left)

    oo

    xx

    x

    xxo

    P

    xV-)edx()eV(dlVo

    !! !

    !03

    0

    4

    ! dlVP

    field)ive(conservat00xV0xVI ooooP P PP 2 3 41

    !!!

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    Example. Let the vector field be given by .

    Find the line integral of over the semicircular path shown

    below

    xoeVV !

    V

    V

    Consider the contribution ofthe path segment located atthe angle 5

    dl ! dl cos Jex

    dl sin Jey

    Since J ! U - 90 r

    cos J ! cos( U - 90 r) ! sin U

    sin J ! sin( U - 90 r) ! cos U

    dl ! dl sin Uex

    dl cos Uey

    ! adUdl

    { (sin Uex cos Uey )

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    ]

    o

    oo

    yxxxo

    yxxo

    aV

    aVdaV

    deeeeaV

    adeeeVI

    2

    )0cos180cos(sin

    ])(cos)([sin

    )cos(sin)(

    11

    180

    0

    0

    180

    0 1

    180

    0

    !

    r!!

    !

    !

    r

    r

    r!

    !

    UU

    UUU

    UUUU

    U

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    Surface Integrals

    Surface integration amounts to adding up normal

    components of a vector field over a given surface S.

    We break the surface S into small surface elements and

    assign to each element a vector

    is equal to the area of the surface element

    is the unit vector normal (perpendicular) to the surface

    element

    nedsds !

    ne

    ds

    The flux ofa vectorfieldAthrough

    surface S

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    (IfS is a closed surface, is by convention directed

    outward)

    Then we take the dot product of the vector field at theposition of the surface element with vector . The result is

    a differential scalar. The sum of these scalars over all the

    surface elements is the surface integral.

    is the component of in the direction of (normal

    to the surface). Therefore, the surface integral can be

    viewed as the flow (or flux) of the vector field through the

    surface S

    (the net outward flux in the case of a closed surface).

    ds

    ds

    ds

    V

    UcosV

    U! cosdsVdsV

    V

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    Example. Let be the radius vector

    The surface S is defined by

    The normal to the surface is directed in the +z direction

    Find

    V

    dyddxd

    cz

    !

    S

    dsV

    zyx

    ezeyexV !

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    V is not perpendicular to S, except at one point on the Z axis

    Surface S

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    5! SS cosdsVdsV

    c4d(-d)]-2dc[d

    dx)]d(d[cdydxcyx

    ccyxdsV

    cyx

    ccosdxdydscyxV

    2

    dx

    dx

    dscos

    222

    dx

    dx

    dy

    dy

    V

    222

    S

    222

    222

    !!

    !

    !

    !U!!

    !

    !

    U

    !

    !

    !

    !

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    Introduction to ifferential Operators

    An operator acts on a vector field at a point to produce

    some function of the vector field. It is like a function of a

    function.

    If O is an operator acting on a function f(x) of the single

    variable X , the result is written O[f(x)]; and means thatfirst f acts on X and then O acts on f.

    Example. f(x) = x2 and the operator O is (d/dx+2)

    O[f(x)]=d/dx(x2 ) + 2(x2 ) = 2x +2(x2 ) = 2x(1+x)

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    An operator acting on a vector field can produce

    either a scalar or a vector.

    Example. (the length operator),Evaluate at the point x=1, y=2, z=-2

    Thus, O is a scalar operator acting on a vector field.

    Example. , ,

    x=1, y=2, z=-2

    Thus, O is a vector operator acting on a vector field.

    )]z,y,x(V[O

    O(A) ! A A yx ezey3V !)V(O

    scalar32.640zy9VV)V(O 22 n!!!!

    A2AAA)A(O ! yx ezey3V !

    vectore65.16e49.95e4e1240)e2e(6

    ez2ey6zy9)ezey3()V(O

    yx

    yxyx

    yx22

    yx

    n!!

    !

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    Vector fields are often specified in terms of their rectangular

    components:

    where , , and are three scalar features functions of

    position. Operators can then be specified in terms of ,

    , and .

    The divergence operator is defined as

    zzyyxx e)z,y,x(Ve)x,y,x(Ve)z,y,x(V)z,y,x(V !

    xV yV zV

    zyx Vz

    Vy

    Vx

    Vx

    x

    x

    x

    x

    x!

    xV

    yV zV

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    Example . Evaluate at the

    point x=1, y=-1, z=2.zyx

    2 e)x2(eyexV ! V

    0Vz

    1Vy

    x2Vx

    x2VyVxV

    zyx

    zy

    2

    x

    !x

    x!

    x

    x!

    x

    x

    !!!

    31x2V !!

    Clearly the divergence operator is a scalar operator.

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    1. - gradient, acts on a scalar to produce a vector

    2. - divergence, acts on a vector to produce a scalar

    3. - curl, acts on a vector to produce a vector

    4. -Laplacian, acts on a scalar to produce a scalar

    Each of these will be defined in detail in the subsequent

    sections.

    V

    V

    Vv

    V2

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    Cartesian coordinates (x,y,z)

    The ranges of the coordinate variables are

    A vector in Cartesian coordinates can be written as

    The intersection of threeorthogonal infinite places

    (x=const, y= const, and z =const)

    defines point P.

    gg

    gg

    gg

    z

    y

    x

    zzyyxxzyx eAeAeAor)A,A,A(

    A

    Constant x, y and z surfaces

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    zyx edzedyedxdl !

    Differential elements in the right handed Cartesian coordinate system

    dxdydzd !R

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    z

    y

    x

    adxdy

    adxdz

    adydzdS !

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    Cylindrical Coordinates .

    - the radial distance from the z axis- the azimuthal angle, measured from the x-axis in the xy plane

    - the same as in the Cartesian system.

    A vector in cylindrical coordinates can be written as

    Cylindrical coordinates amount to a combination of

    rectangular coordinates and polar coordinates.

    )z,,( JV

    gg

    TJe gVe

    z

    200

    2/12

    z

    22

    zzz

    )AAA(A

    eAeAeAor)AA,A(

    !

    JV

    JJVVJV

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    Positions in the x-y plane are determined by the values of

    Relationship between (x,y,z) and )z,,( JV

    JV and

    zzx

    ytanyx 122 !!J!V

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    R i f V A l iR i f V A l i

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    JV

    VJ

    JV

    !v

    !v

    !v

    eee

    eee

    eee

    z

    z

    z

    0eeeeee

    1eeeeee

    z

    zz

    !!!

    !!!

    VJJJV

    JJVV

    Point Pand unit vectorsin the cylindricalcoordinate system

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    R i f V t A l iR i f V t A l i

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    zand,JV

    semi-infiniteplane with itsedge alongthe z - axis

    Constant surfaces

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    R i f V t A l iR i f V t A l i

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    Differential elements in cylindrical coordinates

    Metric coefficient

    zp adzadaddl JVV! J

    dzdddv JVV!

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    Planar surface( = const)

    Cylindricalsurface

    ( =const)

    dS! VdJdzaV dVdzaJ

    VdJdVaz

    Planar surface( z =const)J

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    Spherical coordinates .

    - the distance from the origin to the point P

    - the angle between the z-axis and the radius

    vector of P

    - the same as the azimuthal angle incylindrical coordinates

    ),,r( JU

    Review of Vector AnalysisReview of Vector Analysis

    0 e r0 e5 T

    Colatitude(polarangle)

    1 24 34

    0 e * 2T

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    2/1222

    r

    rrr

    )AAA(A

    eAeAeAor)AA,A(

    JU

    JJUUJU

    !

    UJ

    JU

    JU

    !v

    !v

    !v

    eee

    eee

    eee

    r

    r

    r

    0eeeeee

    1eeeeee

    rr

    rr

    !!!

    !!!

    JJUU

    JJUU

    A vector A in spherical coordinates may bewritten as

    Point Pand unit vectors in sphericalcoordinates

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    U!

    JU!

    JU!

    cosrz

    sinsinry

    cossinrx

    22

    11-22

    1222

    yx

    xcos

    x

    yt n

    z

    yxt nzyxr

    !!J

    !U!

    rzcos

    zt n 11 !V!U

    Rel tionships between sp ce v ri bles )z,,(

    nd),,,r(),z,y,x( JVJU

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    JU nd,,rConst nt surf ces

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    Differential elements in the spherical coordinate system

    JU JUU! adsinrardadrdl r

    JUU! ddrdsinrdv 2

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    J

    U

    J

    JU

    JUU!

    adrdr

    adrdsinr

    addsinrdS r2

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    e e o ecto a ys se e o ecto a ys s

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    yy