Vector Analysis - University of Mississippiperera/EM/EM_lec01.pdfVector Analysis Vector analysis is...

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Vector Analysis Electromagnetic Theory PHYS 401 Fall 2017 1

Transcript of Vector Analysis - University of Mississippiperera/EM/EM_lec01.pdfVector Analysis Vector analysis is...

  • Vector Analysis

    Electromagnetic Theory

    PHYS 401

    Fall 2017

    1

  • Vector AnalysisVector analysis is a mathematical formalism with which EM concepts are most conveniently expressed and best comprehended.

    • Many physical quantities are completely describes by their value

    – e.g. temperature, pressure, mass, frequency…

    • Such quantities are called scalars, and their values can be given in numbers.

    • But many physical quantities have a direction in addition to magnitude– e.g.: velocity, force, displacement…

    – To describe such quantities their direction as well as their magnitudes have to be specified. So just a regular number is not inadequate.

    Vector: a mathematical object that has a magnitude and a direction.

    – Physical quantities which possess a direction as well as a

    magnitude are represented by vectors

    Vector Notation: A vector is usually written as a bold face letter (like A) or with an little arrow or line above it �� , �̅

    The magnitude of a vector A is written as |A| or A2

  • • Often a vector is graphically represented by a directed line segment (an arrow):

    – Whose length represents the magnitude and its orientation in the direction of the vector.

    NB.: This is just a geometrical representation, vectors are not arrows, they are abstract mathematical objects.

    In representing a vector graphically, it is defined only by its magnitude and direction, not its position.

    length = |A|, A

    magnitude of vector

    direction:

    direction of vector

    All these represent the same vector

    A

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  • • When a vector is multiplied by a positive number, it multiplies its magnitude, its direction stays the same.

    • Multiplying by a negative number flips the direction of a vector

    A 2A2.5A

    -2A

    • Sum of two vectors is the single equivalent vector which has same effect as application of the two vectors.

    • e.g. consider adding two displacements.

    A

    BA+BGraphically, vectors are added using the

    triangular rule

    (also called “head-to-tail” rule; Move B so that the head of A touches the tail of B)

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  • • This can be repeated to add any number of vectors

    AB

    A+BCA+B+C

    given any three vectors A, B, and C vector addition obey following properties:

    Addition Multiplication by a scaler

    Commutative

    Associative

    Distributive

    where k and l are scalars

    5

  • • Just like vectors can be added to form a single vector, any given vector can be written as a combination of other vectors.

    • This is called vector decomposition.

    • One particularly useful decomposition is, decomposing a vector as a sum of vectors parallel to coordinate axes.

    A

    X

    Y

    X

    Y

    A

    X

    Y

    Y

    X

    Z

    Z

    A=X+YA=X+Y+Z

    • Those are called components of the vector along coordinate axes

    Vector Decomposition

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  • • Unit vectors: A vector whose magnitude is 1.

    – Usually unit vectors are written with a hat (like �� , �� =1 )

    – Any vector can be written as a product of its magnitude times the unit vector in that direction.

    ��

    aa= � ��

    �� : the unit vector in the direction of the vector a

    X

    A

    X

    Y

    Y

    Z

    Z

    A=X+Y+Z

    ��

    ��

    Suppose �� , �� , are unit vectors along X,Y,Z coordinate directions,

    Then X=|X| �� , let |X| = x then X= x��

    Similarly Y= y�� , Z= z

    So A=X+Y+Z = x��+ y�� + z

    Often it is just written as a coordinate triplet

    A= (x,y,z) leaving the sum over unit vectors to

    be understood.

    Magnitude of the vector A= � � � � �

    ⇒ �� = �

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  • Position Vector (Radius Vector)

    The position vector r of point P is defined as the directed distance from the origin O to P; that is,

    r = x��+ y�� + z

    • The unit vector in the direction of r is

    � =�

    �=

    ��� � ��� � �

    � � � � �

    • If there are two points with position vectors r1 and r2 , thedistance vector between them r12 = r2 – r1

    X

    r

    xy

    Y

    Z

    z

    P

    ��

    ��

    O

    8

    O

    r1

    r2

    P1

    P2

    r12

  • • Components of sum of vectors is sum of components

    e.g. Let A = ����+ ���� + �� and B = ����+ ���� + ��

    Then A+B = �����+ ���� + �� �� ) +(����+ ���� + �� )

    = ����+���� +���� +����+ �� + ��

    = ���������+���������+���+���

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  • Vector Products• Vector quantities are often combined to form a new quantities.

    the result could be a scale or a vector.

    – e.g. Work done by a force is the product of displacement times the force in the direction of displacement.

    • Both force and displacement are vector quantities, and work is a scalar.

    – Angular momentum is the product of momentum and distance perpendicular to momentum to origin (axis of rotation).

    • Momentum is a vector, since distance is taken in a specified direction it also becomes a vector. Resulting angular momentum is also a vector.

    • So two types of vector products are defined, scalar and vector.

    � = �� cos "

    p

    rO

    "

    ��

    # = ��$% sin "

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  • The Scalar Product (Dot Product)

    The scalar product (also called of the two vectors A and B is defined as the product of the magnitude of A and the projection of B onto A (or vice versa):

    ( · * = AB cos "-.

    where "-. is the angle between A and B.

    dot product is commutative : ( · * = * · (

    and distributive : ( · * + / = ( · * + ( · /

    • If two vectors are perpendicular to each other their scaler product is zero (cos90∘ = 0) .

    • Therefore for unit vectors �� , ��, along coordinate axes

    �� · �� = 4; �� · = 4; �� · = 4

    and �� · �� = 5; �� · �� = 5; · = 5

    "-.A

    B

    ��

    ��11

  • if A = ����+ ���� + �� and B = ����+ ���� + ��

    ( · * = �����+ ���� + �� � · ����� � ���� � �� �

    using above properties = ����+ ����+ ����

    ( · ( = ����+ ����+ ���� = ��

    � ��

    ���

    = (

    Since ( · * = AB cos "-.

    cos "-. =(·*

    ( *useful in finding angle

    between two vectors.

    In general the component of a vector ( in the direction of vector C is given by ( · /7

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  • The Vector Product(Cross Product)

    • The vector product of two vectors, A and B is a vector,

    –its magnitude is equal to the product of the magnitudes of A and B and the sine of the angle between them

    –its direction is perpendicular to the plane containing A and B, in the direction of advance of a right handed screw when it is turned from A to B.

    ( 8 * = 9�AB sin "-.

    ( 8 * = area of the parallelogram determined by A and B

    A

    B

    "-.

    :�

    ( 8 * = 9�AB sin "-.

    ( 8 *

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  • • The vector product has following properties:

    – It is not commutative: ( 8 *= ;* 8 (

    – It is not associative: ( 8 * 8 / < ( 8 * 8 /

    – It is distributive: ( 8 * � / = ( 8 * � ( 8 /

    – ( 8 ( = 4�sin θ = 0�

    • For unit vectors �� , ��, along coordinate axes

    �� 8 �� = 4; �� 8 �� = 4; 8 = 4

    �� 8 �� = ; �� 8 = ��; 8 �� = ��

    �� 8 �� = ; ... and so on

    In tems of components

    A = ����+ ���� + �� and B = ����+ ���� + ��

    ( 8 * = �����+ ���� + �� � 8 ���� � ���� � ��

    = ����� ; ������� � ����� ; ������� � ����� ; �����

    ��

    ��

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  • Triple vector products

    • Since result of the vector product between two vectors gives a vector it can it can be multipied with another vector.

    • The scalar triple product between A ,B and C :

    – It is equal to the volume of the parallelepiped spanned by A, B, and C

    In terms of components

    • The vector triple product between A ,B and C :

    ( 8 * 8 / = * ( · / ; /�( · *� (“bac-cab” rule)

    It is not associative: ( 8 * 8 / < ( 8 * 8 /

    A

    B

    C

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  • Vector Calculus

    A field can be defined as a function that specifies a value for a particular quantity everywhere in a region. It could be a scalar, vector or other type of field.

    – Air temperature in a room: every location has a specific temperature so temperature can be considered as scalar field.

    – Wind speed: Speed of air in the atmosphere is another example, since wind speed has a direction (velocity), it is a vector field.

    16Wind speed at sea level during hurricane Katrina

    Fields:

  • Gradient of a scalar Field

    • Suppose a certain scalar field (i.e. temperature) given by T(x,y,z)

    temperature at the point P1 is T(r) = T(x,y,z)

    temperature at the point P2 is T(r+dr)=T(x+dx,y+dy,z+dz)

    The displacement from P1 to P2 is the displacement vector dr with

    components (dx,dy,dz). �� = dx�� + dy�� + dz

    Temperature difference between P1,P2: dT = T(r+dr)-T(r)

    dT=T(x+dx,y+dy,z+dz) - T(x,y,z)

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    X Y

    Z

    P1(r)

    P2(r+dr)

    dx

    dy

    dz

  • So the change in temperature dT is given as the projection of a ‘change of temperature vector’ (inside square brackets) corresponds to the displacement dr .

    This vector is called the Gradient of the scalar T,

    written as Grad T or >?.

    It is a generalization of one the dimensional differential operator

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    to 3 (or higher) dimensions:

  • Gradient operator

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    • Gradient is the ‘slope’ of a scalar field at a point. It gives the direction and magnitude of the greatest rate of change of the field.

    • Rate of change in any other direction is given by the projection of gradient in that direction

    • Rate of change in a given direction = �� · >?,

    �� unit vector in that direction

    >@

    A surface of constant @ (a level surface), >@is normal to it.

    >?, maximum rate of change in this direction

    T(x,y)

    T lowT high

    rate of change in this

    direction = �� · >?

    ��

    9�

    T constant curves

    P

  • Example:

    • Find the directional derivative of f(x,y,z)= x2 +y2 +z2 along the direction 3x � 2y ; zand evaluate it at the point (2,1, 2).

    Lets denote the given direction as a

    The unit vector in the direction of a= F =F

    F=

    GHIJ�KL

    GMIMI�KN�M=

    GH�IJ�KL�

    NO

    directional derivative in the direction 3x � 2y ; z = P · >Q

    =GHIJ�KL

    NO· 2xx � 2yy � 2zz =

    RHIO�KL

    NO

    at the point (2,1,2) = R⋅IO⋅NK⋅

    NO=

    N

    NO

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  • ‘Del’ Operator

    can be considered as the operator

    acting on the scalar field T.

    It is called the ‘del’ operator when grad T is written as >? it represent this process.

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  • Divergence of a Vector Field• The divergence of a vector field at a given point is the net

    outward flux per unit volume. It is a scalar quantity.

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    flow of A integrated over the surface

    Net outward flow,positive divergence

    No net outward flowzero divergence

    Net inward flow,positive divergence

    It represents the amount of field sources at each point.

  • • Suppose a vector filed A =(Ax,Ay,Az) at the the point (x,y,z).

    Lets calculate the net outward flus of this field over a small rectangular box of size (2∆x,2∆y,∆z) centered at (x,y,z)

    On the left face of the box outward flux is

    Divergence

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    X

    Z

    areafield normal to face at the center of face

    P(x,y,z)

    2∆x

    2∆y

    2∆z(x+∆x,y+∆y,z+∆z)

    A

    (x-∆x,y-∆y,z-∆z)

    Az

    AyAx 2∆x

    2∆z�x,yx-∆y,z)

    On the right face of the box outward flux

    Y

  • Total outward flux from left and right faces

    Similarly

    Total outward flux from front and back faces

    Total outward flux from top and bottom faces

    Total outward flux

    Divergence

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    P(x,y,z)

    2∆x

    2∆y

    2∆z

    A

    X

    Z

    Y

  • Divergence of the vector field A

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    Divergence Theorem:

    The total outward flux of a vector field A at the closed surface S is

    the same as volume integral of divergence of A.

    Here is the surface integral of A over the surface

    flux through the surface element of area ∆S

    ∆W: directed area element (direction of area is the normal direction)

    A

    :�∆S

    "

  • The Curl of a Vector Field

    Since the del operator > = X

    Y

    Y�+Z

    Y

    Y�+

    Y

    Y�is a vector, it is possible to

    take the vector product of it with a vector field.

    The vector field produced by this operation is called the curl of the vector field.

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  • The Curl of a Vector Field

    • The curl of a vector field describes the infinitesimal rotation (circulation) of the vector field.

    • A good measure of the circulation is the line integral of the field around a closed curve at a given point. If the vector field is ‘rotational’ it contributes to the integral.

    27

    "A

    is the line integral of the field A along the closed

    curve C, ∮ ( · ∆\ ]

    is the integral of component

    (projection) of the vector field along the curve.

    For a small segment of the curve ∆l :

    ∆\ ( cos " = ( · ∆\

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    no rotationrotation exits away from the center

    bulk rotation around center, no local rotation elsewhere

    local rotation everywhere

    Watch the video: www.youtube.com/watch?v=vvzTEbp9lrc

  • To see this lets calculate the circulation of field A around a closed rectangular contour abcd of size 2∆Y82∆Z around point P(x,y,z), perpendicular to X axis.

    29

    X

    Z

    Y

    P(x0,y0,z0)

    b

    (x0,y0+∆Y,z0-∆Z)

    c (x0,y0+∆Z,z0+∆Z)d

    (x0,y0-∆Z,z0+∆Z)

    a

    (x0,y0-∆Y,z0-∆Z)

    2∆Y

    2∆Z

    evaluated at (x0,y0,z0)

  • The Curl of a Vector Field

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    curl of the vector field A can be defined as:

    C

    ∆l ∆S is the area enclosed by an enclosed curve C oriented such that the integral has maximum value.

    :� : unit vector normal to area ∆S, in the direction of motion of a right handed screw when it is turned in the direction of integral is taken.

    "A

    ∆S

    :�

    area of loop

  • Stokes’ Theorem• Stokes’ theorem converts the surface integral of the curl of a

    vector field over an open surface into a line integral of the vector field along the curve bounding the surface.

    31

    dS

    C

    dlValidity of this can be intuitively seen directly from the definition of curl

    Divide the surface in to a large number of small areas and apply above to each and take the sum

    • the line integrals along the common sides

    of adjacent areas mutually cancel.

    • only those sides in the periphery of the

    surface contribute to the sum.

    ∴ In the limit areas are infinitesimal this becomes the Stokes’ theorem

  • Laplacian Operator

    The Laplacian operator is the scalar product of the del operator with itself.

    32

    The result is a scalar operator. It can be applied to a scalar or vector field.

  • Coordinate Systems

    Infinitesimal volume element = dxdydz

    Infinitesimal volume element dr=dx��+ dy�� + dz

    33

    X

    xy

    Y

    Z

    z

    P

    ��

    ��

    O

    Cartesian coordinates :

    • Three mutually orthogonal axes X,Y,Z,

    unit vectors �� , ��, arein the direction of

    increasing coordinate value.

    A point P in space is given by the

    projections x , y , z on coordinate axes.

    P(x , y , z) = x��+ y�� + z

    −∞ < � < ∞, −∞ < � < ∞, −∞ < � < ∞

    P(x,y,z)

    dx

    dy

    dz dr

  • Cylindrical Coordinates

    • Unit vectors e, f�, are in the direction of increasing coordinate values.

    • Unlike in Cartesian system not all unit vectors are fixed. Directions of eand f� are depend on the position (azimuthal angle g).

    Relation between Cartesian and cylindrical coordinates.

    � = h cosg , y = s sing, � = �

    e = ��cosf � ��sinf , f� = ;��sinf � ��cosf

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    X

    x

    y Y

    Z

    z

    P

    O

    s

    s

    e

    f�

    • In cylindrical coordinates position of a point P is given by:

    – S : the radial distance from Y axis

    – ∅ ∶the azimuthal angle, measured from the X-axis in the XY plane

    – z : the distance from the XY plane

    (same as in the Cartesian system)

    0 d h d ∞, 0 d g d 2k, ;∞ d � d ∞

  • • Sides of the infinitesimal volume element: ��; �h; h�g

    • infinitesimal volume element= h�h���g

    • Del operator:

    35

    s+ds

    sdφ

    ds

    s

  • Spherical Coordinates

    • Unit vectors �, f�, m� are in the direction of increasing coordinate values. Their directions depend on the position.

    Relation between Cartesian and spherical coordinates.

    � = $ sin " cosg , y = $sin " sing , � = $ cos "

    �� = ��sin" cosg � �� sin " sing � cos " �� = �sin" cosg � m� cos " cosg ; f� sing

    m� = ��cos" cosg � �� cos " sing ; sin " �� = �sin" sing � m� cos " sing �f� cosg

    f� = ;��sing � ��cosg = �cos " ; m�sing36

    X

    x

    y

    Y

    Z

    z

    P

    O

    ∅s

    m�

    f�

    In cylindrical coordinates position of a point P is given by:

    – r: radial distance the origin

    – ∅ ∶azimuthal angle, measured from the X-axis in the XY plane

    – " : angle between the Z axis and the line from origin to point P

    0 d $ d ∞, 0 d g d 2k, 0 d " d k

    " r

    X

    x

    y

    Y

    Z

    z

    P

    O

    ∅s

    m�

    f�

    " r

  • Line element: =dr��rdθm�+rsinθdφf�

    Volume element: dr rdθ rsinθdφ = r2sinθdθdφ

    Del operator :

    Example: A sphere of radius 2 cm contains a volume charge density ρgiven by

    Find the total charge Q contained in the sphere 37

    X

    x

    y

    Y

    Z

    z

    P

    O

    ∅s

    m�

    f�

    " r

    dr

    rsinθdφ

    rdθ

  • Summary

    38

  • Show that: curl of gradient of a scalar field is zero > 8 >@ = 0

    Show that : divergence of curl of a vector field is zero > · > 8 n = 0

    Calculate grad of 5

    o

    Calculate the divergence of : �

    oM

    39

  • the Fundamental Theorems

    (1)Gradient :

    combine (1) and (3)

    combine (3) and (2)

    (2)Divergence :

    (3)Curl :

    curl of grad zero

    div of curl zero

    when the boundary

    shrinks to a point

  • Few basic identities for grad, div, curl

    41

  • 42

    > · ( 8 p =n. > 8 p − p · > 8 n :

  • but it leads to contradiction with the divergence theorem , say applied over a sphere:

    Naive calculation gives:

    Problem is the field is ∞atr=0andnotcorrectlyexpressed

    x > y z�v =|}~o

    0

    Delta function:

  • Delta Function

    To work with such situations the Dirac delta function is � used:

    In 1dimention it is defined as:

    It is an even fiction with unit area

    44

    1

    1

    x �

    K�� = 1

    Q � = lim⇢1

    k K���M

  • Other properties of delta function

    45

  • 3D Delta function

    Which can be generalized to 3 D as

    and

    Now consider

    Since according to divergence theorem and

    > · = 0for$ < 0

    46

  • • Since for any sphere arbitrary small, it shows

    that the entire contribution comes from the point at the origin r=0

    Which implies:

    So that

    As required by the divergence theorem

    47

  • Helmholtz Theorem(The fundamental theorem of vector analysis)

    The Helmholtz theorem states that any continuous vector field can be written as a sum of a gradient of a scalar field and a curl of a vector field.

    �� = >�$� � > ×(r)U is called the scalar potential and W is called the vector potential of the field Proof:

    48

    rr’

    0

    dv’

    P

    (Both U(r), W(r) have to go to zero faster than 1/r2 as r →∞)

  • • So any vector can be written as a sum of a Divergence less field and a Curl less field.

    49

    The divergence and curl of a vector field uniquely define a vector field.